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Samstag, 17. Dezember 2016

GEOFON GLOBAL EARTHQUAKE MONITORING 2016

 

Our Mission

GEOFON seeks to facilitate cooperation in seismological research and earthquake and tsunami hazard mitigation by providing rapid transnational access to seismological data and source parameters of large earthquakes, and keeping these data accessible in the long term.
It pursues these aims by operating and maintaining a global network of permanent broadband stations in cooperation with local partners, facilitating real time access to data from this network and those of many partner networks and plate boundary observatories, providing a permanent and secure archive for seismological data. It also archives and makes accessible data from temporary experiments carried out by scientists at German universities and institutions, thereby fostering cooperation and encouraging the full exploitation of all acquired data and serving as the permanent archive for the Geophysical Instrument Pool at Potsdam (GIPP). It also organises the data exchange of real-time and archived data with partner institutions and international centres.
Using real-time data streams, GEOFON determines rapid automatic location estimates for all globally recorded earthquakes and most regional ones, and provides manually revised solutions for the largest earthquakes with minimal delay. This service provides basic rapid earthquake information to earthquake and tsunami warning centres worldwide, governmental agencies, disaster management teams, news media and scientists at the GFZ and elsewhere. The GEOFON earthquake monitoring system acts as key node for rapid global earthquake information for the European-Mediterranean Seismological Centre (EMSC) and as background centre of many tsunami warning centres in the Indian Ocean and in the Mediterranean.
It develops and improves methods of rapid analysis of real-time data, works at the forefront of software development to incorporate methodological developments elsewhere into its analysis streams, and cooperates with other national and international data centres in the setting of standards of seismological data exchange.
The access to data and earthquake parameters contributes to basic research into Earth structure and dynamics, primarily of the solid Earth, but also the hydrosphere and atmosphere, applied research related to the hazard from large earthquakes and tsunamis, seismic monitoring for hazard mitigation purposes by national and transnational agencies, and rapid information of the general public.
GEOFON is part of the Modular Earth Science Infrastructure (MESI) housed at the GeoForschungsZentrum providing services within the “Permanent networks”, “Data Distribution and Archiving” and “Communications” groups of MESI. GEOFON's activities are supervised by an external steering committee, the GEOFON Advisory Committee. It directly supports the Helmholtz mission by providing the scientific infrastructure, in the form of the global seismic network, data archival and monitoring facilities, to research the complex system Earth and thus contributes to solving the grand challenge of mitigating the hazard from earthquakes and tsunamis.
Ernst von Rebeur-Paschwitz
Wir wollen in erster Linie die Gründung eines internationalen Netzes von Erdbebenstationen in Anregung bringen, dessen Aufgabe es sein soll, die Ausbreitung der von großen Erdbebencentren ausgehenden Bewegungen auf der Erdoberfläche und durch den Erdkörper in systematischer Weise zu beobachten.
Primarily we would seek the establishment of an international network of earthquake stations, whose purpose would be to systematically observe the propagation of movements generated at earthquake centers, along the Earth's surface and through its interior.
– Ernst von Rebeur-Paschwitz 1895 –

GEOFON Earthquake Information Service

Rapid global earthquake information is a major task of the GEOFON Program of GFZ Potsdam. As a key node of the European Mediterranean Seismological Centre (EMSC), GFZ has the responsibility for rapid global earthquake notifications. GFZ has also become a driving force in earthquake monitoring for tsunami warning in the Mediterranean and the north-east Atlantic as well as for the Indian Ocean.
The GEOFON Earthquake Information Service is
  • one of the fastest sources for earthquake information worldwide,
  • at first fully automatic (type A solutions), therefore errors may occur,
  • only later verified by GEOFON seismologists on an ad hoc (non 24/7) basis (type M solutions, or type C confirmed automatic solutions)
  • based on a virtual seismic network (GEVN: GEOFON Extended Virtual Network, > 700 stations) composed of GEOFON real-time stations as well as from compatible stations from partner networks (in Europe mostly from the VEBSN: Virtual European Broadband Seismic Network).
  • issuing notification e-mail and RSS feeds.

Global Seismic Monitor

The GEOFON Global Seismic Monitor is a world map of global seismicity located automatically using the global virtual seismic network. Detailed information including hypocenter coordinates and a location map are displayed for the last major earthquake. There is also a large version suitable for display on a 1280x1024 screen, e.g. by using a web browser in full-screen mode.

Earthquake Bulletin

Event classification criteria

  • Normal
    • All events which are located automatically by a sufficient number of stations (>=25) or manually revised events.
  • BIG
    • all events with M >= 4.5 in Central Europe, or
    • >= 5.0 in the wider Europe/Mediterranean area, or
    • >= 5.5 in the rest of the world.
  • XXL
    • All events with M >= 5.0 in Central Europe, or
    • >= 5.5 in the wider Europe/Mediterranean area, or
    • >= 6.5 in the rest of the world.
Subscribe (or unsubscribe) for automatic earthquake notification e-mail, using our form.
Recent earthquakes of the GEOFON bulletin are also accessible through an RSS feed.

 

GEOFON real-time earthquake monitoring - how does it work?

Every day there are tens of earthquakes causing small to severe ground shaking. Only a few of these can be felt immediately by people in the vicinity of the epicenter. Many more earthquakes can be located only using a sensitive, global, network of instruments.
Here we describe how earthquakes are located by our instruments and quantified here at GEOFON.

Global earthquake monitoring

When an earthquake ruptures it radiates seismic energy in the form of seismic waves. These waves propagate away from the earthquake source at wave speeds that depend on the mechanical properties of the rocks that the seismic waves travel through. If the earthquake and hence the energy of the seismic waves is large enough, the waves may be registered as a signal at a distant seismic sensor.
Since earthquake waves travel at a finite speed the signals are recorded at seismic stations with a delay, which depends on the wave type and the path the wave has travelled. Compressional waves, so-called P waves, are the fastest and travel with speeds ranging from about 6 km/s in the Earth's crust to up to about 14 km/s in the mantle. P waves are the signals most commonly used in earthquake location.
The distribution of the seismic wave speeds is relatively well known for most parts of the Earth. Allowing a prediction of the arrival time for any point on Earth for any earthquake hypocenter and time. By measuring the arrival times at many stations and comparing these with the times predicted for certain hypocenter locations and times, the latter can be estimated quite accurately. This is the principle of earthquake location.
Using sensitive modern digital broadband seismometers deployed at seismic stations, recording the ground motion continuously, seismic waves radiated from earthquakes can be detect anywhere on Earth, provided the earthquake signal amplitude is sufficiently above the background noise. As a rule of thumb, earthquakes above a magnitude of about 5, sometimes a bit less, can be recorded at quiet world-wide. Smaller earthquakes are normally recorded at shorter distances only. For instance a magnitude 3 earthquake in Central Europe is usually well recorded up to distances of about 100-200 km.

Data acquisition

Before the arrival times of seismic phases can be measured, the waveform data must reach the GEOFON data center at Potsdam. Nowadays, real-time data telemetry is standard for permanent seismic stations. Often stations are installed in very remote areas, where there is no other means than satellite connection. In other places, permanent internet connections, or even dial-up lines, can be used. To keep operating costs to a minimum, GEOFON stations are connected to the GEOFON data center by the technology that provides the best reliablility at the lowest possible cost. At stations within Europe where the infrastucture is excellent, costly satellite telemetry can mostly be avoided. In contrast, in the Indian Ocean region, VSAT is often the only option, not only because of the lack of land-based alternatives, but also because data must remain available immediately after major earthquakes, when Internet connections or mobile phone lines may have failed. Often a combination of VSAT and terrestrial Internet connections are used: VSAT connects the remote station site to a regional satellite hub, from where the data are streamed through terrestrial Internet connections to Potsdam. A protocol called SeedLink, developed by our group in 2001, is used to cope with the diversity of possible data transport links. Advanced: This protocol has become a de facto standard for reliable data transmission from the stations to the data centers but also amongst data centers. Data transmission is very fast, with delays typically in the range of 5-30 seconds.

Virtual network

In addition to the approximately 80 stations currently active in its own network, GEOFON acquires data from partner networks, which are included in our processing. This increases the number of stations available in real time to form a virtual network of well over 500 stations [Now 600-700? UPDATE!] and ensures good global coverage with stations. Even at times when some networks are unavailable due to technical problems, there are always enough stations providing data to allow a reliable earthquake monitoring.

Automated analysis in real time

Once the data arrive at the GEOFON data center they are analyzed in real time. At the same time, they are archived permanently and made available to the scientific community. At the first stage, phase [Link: IASPEI (2001)? MSOP (1979)?] arrivals must be detected and timed. Advanced: Usually phase arrivals are characterized by a rather sudden increase in amplitude within a relatively narrow frequency band at around 1 Hz, where the signal-to-noise ratio is usually favorable to observe signals from earthquakes thousands of kilometers away. By comparing the short-term average amplitude to the long-term average amplitude, sudden amplitude increases can be detected quite reliably. The time of the onset of the amplitude increase is then taken as the arrival time of the seismic phase. This procedure is normally referred to as "phase picking". P waves are the fastest seismic waves and usually provide the best defined onset times, so normally the vertical component of ground motion is used for phase picking, where the P wave can be observed best. The continuously flowing waveform data produces frequent phase picks with sometimes hundreds of picks per hour [per stream?]. The vast majority of these picks do not correspond to seismic phase onsets i.e. actual earthquakes, but represent noise generated by human activities ( e.g., mining, traffic) or weather phenomena (e.g., thunderstorms). It is important to prevent these from being misinterpreted as seismic phase onsets. The software that analyses the phase picks in real time has to recognize picks corresponding to the same event while at the same time it has to keep the wrong picks out of the solution. The more picks are available for a given seismic event, the better this distinction will work, because questionable or inconsistent picks can be identified more easily.
Internally an earthquake is often located within a few minutes of its occurrence. Much of the delay is due to the time for seismic waves to reach enough stations to form a rough initial location. As more picks are received from stations further away from the epicenter, the initial location gets refined. In parallel to locating the earthquake, amplitudes are measured, which are then used to compute the magnitude of the event. Once a certain publication threshold is reached, usually defined by the number of picks contributing to the location, the information on the earthquake is published. As the automatic analysis continues, updated solutions - both in terms of location and magnitude - are provided immediately on the GEOFON earthquake bulletin web site and the RSS feed. E-mail is normally sent only once for an event, immediately after the publication threshold is reached. (You can sign up for e-mail alerts.) The GEOFON publication criteria are chosen to ensure a reasonable quality of the solution, but it is recommended to check the GEOFON earthquake bulletin website for the latest updates.

Manual revision

Up to this point in the processing chain, the analysis and publication is fully automatic. This ensures that within a short time after an important earthquake, the main parameters epicenter location, depth and magnitude are made available on the GEOFON website day and night, 7 days a week. Automatic solutions, however, are subject to uncertainties. One parameter which is often difficult to determine with good accuracy is the focal depth. Especially for shallow earthquakes where a difference of 10 km in depth might make a big difference in terms of expected damage. Advanced: The depth uncertainty is related to the geometry of the waves leaving the source. To allow a good depth estimate, it is important to have data from stations close to the epicenter. This is often not the case, especially in remote regions, or due to restrictive data policies. As an alternative to using data from nearby stations, it is possible to constrain the source depth using so-called depth phases. These are waves initially travelling upwards from the hypocenter and then being reflected at the Earth's surface, resulting in a seismogram in which both the direct and the reflected phase are visible. From the time difference between the two phases, the depth can be estimated quite accurately. Unfortunately these depth phases require observations from at least 3000 km away from the epicentre, and even there depth phases cannot always be identified. Furthermore, depth phases of shallow events follow the direct waves very closely and it requires an experienced analyst to distinguish them reliably. This unfortunately prevents the use of depth phases in automatic processing. At GEOFON depth phases are hand picked if present, improving the depth accuracy during a manual revision of an event. Manually revised events are marked with a green M in the event list.
[Mention: we do not run a 24-hour operation.] Left: Schematic view of the data flow at the GEOFON data center. Blue arrows represent the flow of seismic waveform data, whereas red arrows represent derived parametric data. Human interaction with the mainly automatic system is represented by orange arrows.

Further reading

  • Bormann, P. (Ed.) (2012). New Manual of Seismological Observatory Practice (NMSOP-2), IASPEI, GFZ German Research Centre for Geosciences, Potsdam; http://nmsop.gfz-potsdam.de; DOI: 10.2312/GFZ.NMSOP-2 urn:nbn:de:kobv:b103-NMSOP-2

GEVN network

To fullfill its global earthquake monitoring task, data from the permanent GEOFON network and from many of its partner networks as well as from other public networks in Europe and worldwide are collected over Internet, forming the so-called GEOFON Virtual Network (GEVN). Broad-scale real-time data exchange within Europe (Virtual European Seismic Network (VEBSN)) is mainly an achievement of the EC projects MEREDIAN and NERIES, coordinated by ORFEUS and based mainly on GFZ developments and initatives, globally by the FDSN (Federation of Digital Seismograph Networks) . The GFZ earthquake information service must therefore be regarded as a joint effort of all involved institutions and credit has to be given to all of them. SeedLink real-time data feeds are mostly provided directly by the individual network data centers. However, data feeds for BE, BS, NO, NS, SS networks are obtained from the ORFEUS Data Centre (De Bilt, Netherlands), and data feeds from CU, GT, IC, JP, MS, MY, US are retrieved from the IRIS Data Management Center (Seattle, USA), which acts also as the data center for the FDSN backbone network.
For more information about the GEOFON Global Seismic Network (network code GE) please visit our archived network information page.




 

GEVN virtual network list

Network Description Start Date # Station(s)
AF  South Africa National Seismograph Network (SANSN-Net) 2007 7
AU  Australian National Seismograph Network 1998 38
AW  AWI Network Antarctica (AWI-Net) 2006 18
C  Servicio Sismologico de Chile Network 2001 18
CK  CAREMON, Central Asian Cross-border Network (CAREMON) 2009 7
CM  Red Sismologica Nacional de Colombia - RSNC 2008 5
CN  Canadian National Seismograph Network 1989 14
CR  CR - Croatian Seismograph Network 1999 3
CU  (GSN affil) Carib/USGS (CU), Nat Res Env, UH, UWI 2006 9
CX  IPOC Seismic Network (Integrated Plate boundary Observatory Chile) 2006 20
CZ  Czech Regional Seismic Network 1995 19
DK  Danish National Seismic Network 1999 19
EE  Estonian Seismological Network 2005 2
EI  Irish National Seismic Network, DIAS, Dublin, Ireland 2011 3
ES  ES - SPANISH DIGITAL SEISMIC NETWORK 1980 10
EV  No Description 2014 1
FN  Northern Finland Seismological Network 2005 4
FR  RESIF - OMP - Toulouse, France 1994 17
G  GEOSCOPE 1982 26
GE  GEOFON Program, GFZ Potsdam, Germany 1993 79
HE  Finnish National Seismic Network 2006 6
HT  Aristotle University Thessaloniki (HT-Net) 2006 15
HU  Hungarian National Seismological Network, MTA CSFK GGI (GGI_Net) 2004 14
IA  BMG-Net, Indonesia (IA-Net) 2000 143
IG  IG network 2008 3
II  (GSN) Global Seismograph Network (IRIS/IDA) 1986 38
IN  Indian Seismic Network 2006 3
IO  EvK2-CNR Pyramid Laboratory - Mount Everest 2014 1
IQ  Plate Boundary Project Iquique, GFZ Potsdam, Germany 2009 1
IS  Israelian Broadband Seismological Network (GII-Net) 2002 37
IU  (GSN) IRIS/USGS (IU), Pacific 21, and GSRAS 1988 72
JP  Japan Meteorological Agency Seismic Network 1996 23
JS  Jordanian Seismological Network 1983 19
KC  CAIAG Network Kyrgyzstan (CAIAG-Net) 2010 4
KP  KOPRI glisn station 2013 1
KZ  KAZAKH NETWORK IGR NNC 2000 3
MK  MK-Net 2000 3
MS  Singapore Seismological Network 1996 4
MX  Mexico 2013 11
MY  Malaysian National Seismic Network 1970 7
NU  Nicaragua National Seismological Network (NU-Net) 2006 8
NZ  New Zealand National Seismograph Network 2001 9
PA  PA-Net 2010 1
PL  Polish Seismic Network 1995 8
PM  Portugese National Seismic Network (IM_Net) 2006 5
PS  Ocean Hemisphere Network, a part of Pacific21 1993 2
RM  RIMES 2008 4
SJ  Serbian Network of Seismic Stations (SJ-Net) 2000 6
SK  Slovak National Network of Seismic Stations (SK-Net) 2004 8
TM  THAI Seismic Network 2006 11
TT  Tunisia BB Network (TT_Net) 2010 3
TU  National Seismic Network of Turkey 2009 11
TW  Broadband Array in Taiwan for Seismology 2010 7
US  ANSS-NEIC 1992 19
WA  Trillium 120P, 120 s, 1201 V/m/s-Q330SR, gain 1, 1 2011 1
WM  Western Mediterranea Seismic Network (WM-Net) 1997 14
Z3  AlpArray backbone temporary stations 2015 10

Database last updated at 2016 Dec 17 07:22:54
 

Waveform Access

The GFZ Seismological Data Archive is the largest seismological data archive in Europe. It holds data from the permanent GEOFON VBB seismic network. For many GEOFON partner networks, GEOFON acts as backup archive and data distribution center. Additionally, data from many temporary station deployments are permanently archived at GEOFON, in particular passive seismological experiments of the GFZ Geophysical Instrument Pool Potsdam (GIPP) and the German Task Force Earthquake (data archival pending).
Real-time data streams from permanent networks are mostly acquired over the Internet and are immediately accessible as continuous data stream by SeedLink real-time feeds or on request from the archive. Most of the acquired European networks are members of the Virtual European Broadband Seismic Network (VEBSN). Although the archive consists mostly of data from broad band stations, a substantial amount of short period data is archived as well as some strong motion and OBS data.
The GEOFON Data Archive is linked by GFZ's ArcLink protocol to other partner data centers in Germany (German Integrated Data Archive - GIDA) and Europe (European Integrated Data Archive - EIDA). This integrated data archive infrastructure allows transparent access to the data of all participating archives through a single front-end data portal. All data are accessible in a unified way through ArcLink, SeedLink, web forms or by e-mail.

Archive Access Overview

MethodData:Open GFZ NetsRestricted GFZ DataOther EIDA Nets1
ArcLinkYesYesYes
WebDC3YesYesYes
fdsnws-stationYesYesNo
fdsnws-dataselectYesYes (trial version)No2
1 EIDA nets are third-party contributions to the EIDA collaboration, hosted at other nodes.
2 Except where the EIDA contributor lists GFZ as an alternative route.

Data availability

Archive access

Several methods are available to access waveform data from the GEOFON archive:
  • Using the FDSN web services, for data archived at GFZ.
  • Direct access through ArcLink, e.g. by using the arclink_fetch command line client.
  • Web-based requests through our web portal, especially for smaller requests.
Archive data shipments by HTTP (web portal or direct ArcLink requests) or FTP (BREQ_FAST requests) only!

Archive access to restricted data

Access is restricted for:
  • data from recent temporary deployments (limited-duration embargos)
  • some permanent third-party stations/networks for which GEOFON also acts as archive and distribution point
Access to these data may be granted only if the data user can produce written permission from the data producer to use the data, i.e. from the PI of the experiment or a representative of the institution that operates the network. Requests for data access must be sent to GEOFON including the permission statement. Requests using FDSN web services can now be made for restricted data; data requested by Arclink will be encrypted and needs to be decrypted before use.

Real-Time data feeds

GEOFON/GEVN data are available as real-time data feeds without special permission by the SeedLink protocol from the GEOFON SeedLink server at geofon.gfz-potsdam.de:18000. A visualization of the GEOFON real-time stations is provided in the form of "live" seismogram plots.
The telemetry status can be displayed by the following SeedLink monitors:

Data formats

  • SeedLink real-time data comes in 512 byte Mini-SEED format.
  • Archive data shipments in 512 or 4096 byte SEED format.
  • Instrument response information as Dataless SEED volumes or ArcLink XML response files are available through ArcLink and the WebDC3 data request interface (http://eida.gfz-potsdam.de/webdc3).
  • Restricted data is encrypted using OpenSSL.
 

Alert classification criteria (for automatically classified events)
  • Normal (valid location solution)
    • all events which are located by a sufficient number of stations (>=6),
  • Bold
    • all events with M >= 3.5 in Central Europe (mainly Germany),
    • >= 5.0 in Europe/Mediterranean area and
    • >= 5.5 outside of Europe/Mediterranean area,
  •  Bold Red
    • all events with M >= 4.5 in Central Europe (mainly Germany),
    • >= 5.5 in Europe/Mediterranean area and
    • >= 6.5 outside of Europe/Mediterranean area.
Manual vs. confirmed vs. automatic locations Earthquake locations are published automatically without review by a geophysicist if the event was observed at least at 25 stations. While this usually ensures both decent location and magnitude, automatically determined earthquake locations may be erroneous, unless revised by a geophysicist! Automatic locations are therefore marked with an A in the respective row. Manually revised locations are marked with an M instead. Also, small events with less than 25 observations are always manual, because these events are published only after review. If an automatic solution was checked and found to be acceptable without manual revision, it is marked as confirmed with a C.
 
This real-time bulletin is a product of the GEOFON Extended Virtual Network (GEVN) and credit belongs to all involved institutions!
Disclaimer: Unless revised by a geophysicist, automatically determined earthquake locations may be erroneous!
This bulletin is customizable and also available as RSS news feed.
New search    FAQ   
Earlier events No newer events
Origin Time
UTC 		Mag Latitude
degrees		 Longitude
degrees		 Depth
km		 A
M		 Flinn-Engdahl Region Name
2016-12-17 23:54:13 4.1 42.87°N 13.19°E 10 A
Central Italy
2016-12-17 22:21:32 5.3 26.83°S 177.22°W 156 A
South of Fiji Islands
2016-12-17 21:17:21 5.3 16.28°N 146.11°E 10 A
Mariana Islands
2016-12-17 18:54:25 5.2 6.21°S 154.25°E 10 A
Solomon Islands
2016-12-17 18:45:07 5.2 29.15°S 61.11°E 10 C
Southwest Indian Ridge
2016-12-17 17:54:07 4.4 21.61°S 67.15°W 214 A
Chile-Bolivia Border Region
2016-12-17 17:46:36 5.1 6.06°S 153.99°E 10 A
New Britain Region, P.N.G.
2016-12-17 16:12:13 4.9 15.32°N 93.07°W 69 C
Near Coast of Chiapas, Mexico
2016-12-17 15:29:45 5.2 5.80°S 153.93°E 10 A
New Ireland Region, P.N.G.
2016-12-17 13:55:01 5.2 6.25°S 154.12°E 95 A
Solomon Islands
2016-12-17 13:40:49 5.3 5.29°S 153.60°E 98 A
New Ireland Region, P.N.G.
2016-12-17 13:22:34 6.7 6.37°S 154.47°E 39 C MT Solomon Islands
2016-12-17 13:16:31 5.4 4.61°S 153.62°E 124 A
New Ireland Region, P.N.G.
2016-12-17 12:52:35 5.7 5.70°S 153.66°E 10 A
New Ireland Region, P.N.G.
2016-12-17 12:27:29 5.2 6.14°S 154.28°E 54 C
Solomon Islands
2016-12-17 12:01:01 5.2 6.28°S 154.52°E 28 C
Solomon Islands
2016-12-17 11:27:40 6.4 5.70°S 153.84°E 34 C MT New Ireland Region, P.N.G.
2016-12-17 11:22:38 5.7 4.47°S 153.46°E 83 C
New Ireland Region, P.N.G.
2016-12-17 10:51:10 7.8 4.52°S 153.46°E 93 C MT New Ireland Region, P.N.G.
2016-12-17 10:39:37 4.4 40.06°N 19.89°E 10 C
Albania
2016-12-17 09:30:38 5.1 51.59°N 177.24°E 43 C
Rat Islands, Aleutian Islands
2016-12-17 07:23:27 4.8 10.83°S 78.79°W 10 C MT Near Coast of Peru
2016-12-17 06:18:28 4.7 25.87°N 128.47°E 10 A
Ryukyu Islands, Japan
2016-12-17 03:50:06 4.6 36.54°N 70.94°E 183 A
Hindu Kush Region, Afghanistan
2016-12-17 03:02:09 4.6 5.38°N 125.60°E 194 A
Mindanao, Philippines
2016-12-16 23:11:42 5.2 30.44°S 71.67°W 32 C MT Near Coast of Central Chile
2016-12-16 22:39:33 4.8 3.09°S 139.23°E 70 A
Irian Jaya, Indonesia
2016-12-16 21:21:53 4.3 39.73°N 39.71°E 10 A
Turkey
2016-12-16 14:58:05 4.8 5.98°S 129.64°E 195 A
Banda Sea
2016-12-16 11:34:58 5.4 14.19°N 90.62°W 80 M MT Guatemala
2016-12-16 09:40:41 4.7 32.31°S 67.51°W 34 M
Mendoza Province, Argentina
2016-12-16 09:17:19 4.8 10.02°S 160.41°E 10 C
Solomon Islands
2016-12-16 06:46:51 4.6 51.57°N 16.10°E 1 M
Poland
2016-12-16 04:13:23 4.5 23.99°S 66.76°W 189 M
Jujuy Province, Argentina
2016-12-16 03:50:38 4.6 65.43°S 179.50°W 10 C
Pacific Antarctic Ridge
2016-12-16 01:35:52 4.9 2.78°S 128.14°E 47 C
Ceram Sea
2016-12-16 00:34:33 4.5 13.35°N 90.31°W 55 C
Near Coast of Guatemala
2016-12-15 23:32:19 4.5 9.67°S 161.05°E 23 C
Solomon Islands
2016-12-15 22:23:25 5.3 9.93°S 160.54°E 10 C MT Solomon Islands
2016-12-15 22:15:57 3.9 2.24°S 120.08°E 19 M
Sulawesi, Indonesia
Earlier events
GEOFON Program
Automatic GEOFON Global Seismic Monitor
big map
The events displayed occurred within the last 24 hours / 1-4 days / 4-14 days .
regional map
Most recent large event:
New Ireland Region, P.N.G.
Magnitude:7.8 (Mw)
Origin time:2016-12-17 10:51:10 UTC
Epicenter:153.46°E  4.52°S
Depth:93 km
Location status:confirmed
See also:
Last updated 2016-12-17 22:37:31 UTC
 
 F-E Region:

New Ireland Region, P.N.G.
Mw Beach Ball
Time: 2016-12-17 10:51:10.9 UTC
Magnitude: 7.8 (Mw)
Epicenter: 153.46°E  4.52°S
Depth: 93 km
Status: C - confirmed
Event Map
  • Additional information about this event
  • Moment tensor solution
  •  
    GFZ Event gfz2016ysdb
16/12/17 10:51:10.84
New Ireland Region, P.N.G.
Epicenter: -4.49 153.47
MW 7.8

GFZ MOMENT TENSOR SOLUTION
Depth  64        No. of sta: 159
Moment Tensor;   Scale 10**20 Nm
  Mrr= 6.71       Mtt=-2.88
  Mpp=-3.82       Mrt=-2.96
  Mrp= 0.90       Mtp= 2.80
Principal axes:
  T  Val=  7.55  Plg=74  Azm=182
  N       -0.83      11      314
  P       -6.72      11       47

Best Double Couple:Mo=7.2*10**20
 NP1:Strike=150 Dip=35 Slip= 109
 NP2:       307     57        77

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    ##----------------------     
  ----########-----------------  
  ---#############-------------  
 ----###############------------ 
-----#################-----------
-----###################---------
------###################--------
------#########   ########-------
-------######## T #########------
 -------#######   ##########---- 
  -------####################--  
  --------###################--  
    --------#################    
     ----------#############     
        -----------######        
           -----------


Analysis performed by J. Saul
Last updated 2016-12-17 11:58:21 UTC
  • Epicenter location in Google Maps
Method Origin Time
UTC		MagLatitude
degrees		Longitude
degrees		Depth
km		 StrikeDipRake
GEOFON standard1 2016-12-17 10:51:10 7.8 4.49°S 153.47°E 64 150
307		 35
57		 109
77		 beachball
W-Phase2 2016-12-17 10:51:10 7.8 4.49°S 153.47°E 96 140
301		 50
41		 102
76		 beachball
  1. GEOFON standard inversion using body and surface waves. [Details].
  2. GEOFON W-Phase solution.
This is a product of the GEOFON Extended Virtual Network (GEVN) and credit belongs to all involved institutions.

The 2016-12-17 M 7.46 earthquake and aftershocks in New Ireland Region, P.N.G.

GEOFON locations for main shock(s)

GEOFON waveform recording(s)

Seismogram recorded at GEOFON station Fakfak, Indonesia (FAKI).
Caption: Seismogram recorded on 2016-12-17 at GEOFON station Fakfak, Indonesia (FAKI). For other days and locations, use our Live Seismogram service.
Credit: Section 2.4, Deutsches GeoForschungsZentrum GFZ Potsdam.
Contact: GEOFON
>>
This real-time bulletin is a product of the GEOFON Extended Virtual Network (GEVN) and credit belongs to all involved institutions!
Origin Time
UTC 		Mag Latitude
degrees		 Longitude
degrees		 Depth
km		 A
M		 Flinn-Engdahl Region Name
2016-12-17 15:29:45 5.2 5.80°S 153.93°E 10 A
New Ireland Region, P.N.G.
2016-12-17 13:40:49 5.3 5.29°S 153.60°E 98 A
New Ireland Region, P.N.G.
2016-12-17 13:16:31 5.4 4.61°S 153.62°E 124 A
New Ireland Region, P.N.G.
2016-12-17 12:52:35 5.7 5.70°S 153.66°E 10 A
New Ireland Region, P.N.G.
2016-12-17 11:27:40 6.4 5.70°S 153.84°E 34 C MT New Ireland Region, P.N.G.
2016-12-17 11:22:38 5.7 4.47°S 153.46°E 83 C
New Ireland Region, P.N.G.
2016-12-17 10:51:10 7.8 4.52°S 153.46°E 93 C MT New Ireland Region, P.N.G.
2016-12-10 16:24:36 6.0 5.71°S 154.37°E 151 C MT Solomon Islands
2016-12-04 04:41:07 5.0 5.52°S 151.85°E 25 M
New Britain Region, P.N.G.
Earlier events No newer events

GEOFON moment tensor solutions

Geophysical Background

Peak ground acceleration, in New Ireland Region, P.N.G. Caption: Peak ground acceleration with 10% exceedance probability in 50 years. Excerpt from the GSHAP Global Seismic Hazard Map*. Provided by the Equator II system, GFZ Potsdam, 2016-12-17.
* Giardini, D., Grünthal, G., Shedlock, K. M. and Zhang, P.: The GSHAP Global Seismic Hazard Map. In: Lee, W., Kanamori, H., Jennings, P. and Kisslinger, C. (eds.): International Handbook of Earthquake and Engineering Seismology, International Geophysics Series 81 B, Academic Press, Amsterdam, 1233-1239, 2003.

Other data access

Data and metadata from the GE and other seismic networks are available. You may use:
If you make use of this data, please acknowledge it appropriately. This can best be done by citing data providers of individual networks (network name and/or network code). Some data sets distributed by GEOFON, including the GE network, have DOI associated with their seismic network, following a standard procedure approved by the FDSN. Where a DOI is available, this is shown on the network list page (or by an FDSN service), and you are requested to use this in your acknowledgments or citations as appropriate.

Related resources

  1. GFZ Pressemitteilungen, Kurzmeldungen, usw. (German)

About this page

This special event page provides a platform for GFZ scientists working on this event to quickly disseminate results from preliminary analysis in the immediate aftermath of the event. Some parts of this page are static, and updated manually with new results/information as soon as they are made available by the contributors.
Disclaimer: Some of the results on this page are preliminary and sometimes obtained with procedures still under development. The content here may rapidly change as additional information about the event becomes available.

M 7.9 - NEW IRELAND REGION, P.N.G. - 2016-12-17 10:51:09 UTC

http://www.emsc-csem.org/Earthquake/earthquake.php?id=553230#scientific

 



AuthorEMSC
Date/Time UTC2016/12/17 10:51:09.9
Distances to cities887 km NE of Port Moresby, Papua New Guinea / pop: 284,000 / local time: 20:51:09.9 2016-12-17
137 km E of Kokopo, Papua New Guinea / pop: 26,300 / local time: 20:51:09.9 2016-12-17
Latitude4.49 S
Longitude153.49 E
Depth83.2 Km
MagnitudeMw 7.9
RegionNEW IRELAND REGION, P.N.G.
rms1.45 s
Nphases, Nstation358, 348
Gap10 °
95% confidence Ellipse Semi major
Semi minor
Azimuth
4.3 Km
4.2 Km
176 °
Location Typemanual
Publication Time2016-12-17 12:30 UTC
Source parameters reviewed by a seismologist


More information at:

 Badan Meteorologi, Klimatologi, dan Geofisika Djakarta, Indonesia
 USGS/NEIC Denver, USA
 GeoForschungsZentrum (GEOFON) Potsdam, Germany

Tsunami information at:

 Japan Meteorological Agency  Tokyo, Japan
 Pacific Tsunami Warning Centre  Hawai, USA
Explanation of Parameters

Explanation of Parameters

AuthorReporting agency
Date/Time (UTC)The time in UTC the earthquake occurred
Distances to citiesDistances from epicenter to local cities + population and local time in these cities when the earthquake occurred
LatitudeEpicenter latitude in degrees
LongitudeEpicenter longitude in degrees
DepthHypocentral depth
MagnitudeMagnitude type and value


RegionFlinn-Engdahl region
rmsRoot-mean-square travel time residual, in seconds
Nb stationsNumber of seismic stations which reported arrival times for this earthquake.
Nb PhasesNumber of arrival-time observations used to compute the hypocenter location.
GapThe largest azimuthal gap between azimuthally adjacent stations (in degrees).
95% confidence Ellipse95% confidence ellipse on the epicentral coordinate
Semi-major axisLength of the semi-major axis of the 95% confidence ellipse
Semi-minor axisLength of the semi-minor axis of the 95% confidence ellipse
AzimuthAzimuth of the semi-major axis of the 95% confidence ellipse
Location typeA= Automatic; M=Manual


Publication timeThe time this information was published by EMSC.
StaInternational station code
DistDistance in degrees between the epicenter and the station
EvAzAzimuth of Epicenter-Station segment compared to the North direction
AMType of picking : A=Automatic; M=Manual
CDDirection of the first motion : C=Compression; D=Dilation
IEOnset quality (i=impulsive, e=emergent)
PhasePhase code
Pick timeThe UTC time the phase was picked
TresResidual in seconds
AzimObserved backazimuth (degrees)
SlowObserved slowness (seconds/degree)
Tif T, this phase has been used in the location. If empty, this phase has not been used in the location.
Aif A, this azimuth has been used in the location. If empty, this azimuth has not been used in the location.
Sif S, this slowness has been used in the location. If empty, this slowness has not been used in the location.
Amp0-peak amplitude measurment in nm
PerPeriod measurment in seconds
MagMagnitude type and value computed at this station
RNReporting network (EMSC code)
IRSSOperating network IRSS code
FDSNOperating network FDSN code
Sta
Dist
EvAz
AM
CD
IE
Phase
Pick Time
Tres
Azim
Slow
T
A
S
Amp
Per
Mag
RN
Operating Network
IRSS
FDSN
RABL1.36282.7m

Pn2016/12/17 10:51:36.02.5

T




NEIR
AUST
∅
RABL1.36282.7m

P2016/12/17 10:51:36.12.6

T




MAD
AUST
∅
RABL1.36282.7m

Sn2016/12/17 10:51:55.94.6

T




NEIR
AUST
∅
MANU6.59291.5m

Pn2016/12/17 10:52:46.22.2

T




NEIR
AUST
∅
MANU6.59291.5a

P2016/12/17 10:52:47.43.4

T

6015.11.20
GFZ
AUST
∅
PMG7.96231.8a

P2016/12/17 10:53:05.22.5

T

43188.80.80
GFZ
PMG
∅
PMG7.96231.8m

Pn2016/12/17 10:53:05.22.5

T




NEIR
PMG
∅
HNR8.08127.8m

Pn2016/12/17 10:53:04.0-0.3

T




NEIR
HNR
∅
HNR8.08127.8a

P2016/12/17 10:53:06.52.2

T

33459.11.00
GFZ
HNR
∅
PATS12.2523.2m

Pn2016/12/17 10:53:58.9-2.1

T




NEIR
ERIJ
∅
PATS12.2523.2a

P2016/12/17 10:53:59.3-1.7

T

42571.20.80
GFZ
ERIJ
∅
JAY12.92278.3a

P2016/12/17 10:54:12.11.8

T

1185.11.00
GFZ
DJA
∅
GENI13.44277.6a

P2016/12/17 10:54:20.0-0.7

T

4031.81.80
SC3
∅
∅
COEN13.87226.5a

P2016/12/17 10:54:24.8-3.2

T

2403.91.60
GFZ
AUST
∅
COEN13.87226.5m

Pn2016/12/17 10:54:24.82.3

T




NEIR
AUST
∅
MTSU16.27212.8a

P2016/12/17 10:54:56.82.1

T

2485.70.90
GFZ
AUST
∅
CTA17.04203.8a

P2016/12/17 10:55:04.91.7

T

3856.61.70
GFZ
BRS
∅
CTAO17.04203.8a

P2016/12/17 10:55:04.91.7

T

3481.61.70
GFZ
BRS
∅
KOUNC19.13147.6m

P2016/12/17 10:55:26.50.5

T




NEIR
∅
∅
KWAJ19.3346.8a

P2016/12/17 10:55:31.53.3

T

7250.01.60
GFZ
∅
∅
RKPI19.53278.1a

P2016/12/17 10:55:32.01.6

T

4207.61.50
GFZ
∅
∅
MWPI19.77279.8a

P2016/12/17 10:55:35.12.2

T

1660.31.30
GFZ
∅
∅
GUMO19.92334.6a

P2016/12/17 10:55:37.93.3

T

1690.60.90
SC3
NEIC
∅
TARA20.2973.8a

P2016/12/17 10:55:40.72.1

T

7558.01.70
GFZ
∅
∅
EIDS20.91186.1a

P2016/12/17 10:55:45.80.5

T

2225.81.40
GFZ
AUST
∅
QIS20.93219.0a

P2016/12/17 10:55:46.00.4

T

2665.91.10
GFZ
AUST
∅
LIFNC21.02141.6a

P2016/12/17 10:55:51.04.6

T




NEIR
∅
∅
FAKI21.28273.5a

P2016/12/17 10:55:49.30.1

T

1018.51.80mb 5.9SC3
DJA
∅
DZM21.54145.5a

P2016/12/17 10:55:51.3-0.9

T

4600.51.30mb 6.7
GFZ
NOU
∅
ONTNC21.73145.8a

P2016/12/17 10:55:55.41.3

T

5375.11.40mb 6.7SC3
∅
∅
OUENC22.04145.3a

P2016/12/17 10:56:00.02.7

T

3375.62.40mb 6.3SC3
∅
∅
KDU22.33247.3m

P2016/12/17 10:56:00.0-0.3

T




MAD
AUST
∅
SAUI22.35260.0a

P2016/12/17 10:56:03.22.6

T

11633.61.30mb 7.1
GFZ
DJA
∅
SIJI22.47278.5a

P2016/12/17 10:56:02.10.2

T

1081.01.10mb 6.1
GFZ
∅
∅
BNDI23.54269.0m

P2016/12/17 10:56:11.1-1.2

T




MAD
DJA
∅
MTN23.61248.0a

P2016/12/17 10:56:12.5-0.5

T

2476.21.20mb 6.5
GFZ
AUST
∅
QLP23.70201.0a

P2016/12/17 10:56:13.6-0.3

T

4372.51.60mb 6.6
GFZ
AUST
∅
WRAB24.17228.9a

P2016/12/17 10:56:18.0-0.1

T

2022.70.90mb 6.6
GFZ
CAN
∅
WRA24.18228.9m
iP2016/12/17 10:56:16.9-1.4

T




GSRC
CAN
∅
MSAI24.56271.8a

P2016/12/17 10:56:23.92.3

T

72.80.60
GFZ
DJA
∅
KRAI25.09271.8a

P2016/12/17 10:56:26.80.4

T

461.21.30mb 5.8
GFZ
∅
∅
AAI25.27270.9a

P2016/12/17 10:56:29.01.0

T

673.60.90mb 6.1
GFZ
DJA
∅
ARMA25.87183.7a

P2016/12/17 10:56:33.6-0.1

T

1156.71.20mb 6.3
GFZ
AUST
∅
FUNA25.88100.2a

P2016/12/17 10:56:34.30.8

T

1311.30.80mb 6.5
GFZ
∅
∅
NLAI26.39271.8a

P2016/12/17 10:56:39.11.0

T

392.61.50mb 5.7
GFZ
DJA
∅
TNTI26.65280.7a

P2016/12/17 10:56:41.10.6

T

680.31.50mb 6.0
GFZ
DJA
∅
KNRA26.75243.6a

P2016/12/17 10:56:42.00.6

T

1556.31.10mb 6.5
GFZ
AUST
∅
ASAR26.86222.9a

P2016/12/17 10:56:41.7-0.8

T




NEIR
AUST
∅
WAKE26.9828.3m

P2016/12/17 10:56:43.40.0

T




MAD
∅
∅
LHI27.41169.6a

P2016/12/17 10:56:46.5-0.9

T

1124.70.80mb 6.5
GFZ
AUST
∅
MSVF27.44120.6a

P2016/12/17 10:56:47.80.1

T

296.21.40mb 5.7
GFZ
SVA
∅
SANI27.59274.2a

P2016/12/17 10:56:48.90.0

T

472.31.10mb 6.0
GFZ
∅
∅
CMSA27.91194.3a

P2016/12/17 10:56:51.1-0.7

T

1628.81.00mb 6.6
GFZ
AUST
∅
NFK28.03152.3m

P2016/12/17 10:56:51.0-1.9

T




MAD
AUST
∅
OOD28.74214.3a

P2016/12/17 10:56:58.3-0.9

T




KAN
∅
∅
SGSI29.13285.8a

P2016/12/17 10:57:04.92.4

T

896.10.80mb 6.5
GFZ
DJA
∅
STKA29.46200.9a

P2016/12/17 10:57:04.8-0.8

T

144.10.80mb 5.7
GFZ
AUST
∅
SOEI29.48258.1a

P2016/12/17 10:57:06.50.6

T

800.41.40mb 6.2
GFZ
DJA
∅
LCRK29.59207.4a

P2016/12/17 10:57:05.9-0.8

T




KAN
∅
∅
BATI30.14257.4a

P2016/12/17 10:57:12.71.2

T

1615.81.00mb 6.7
GFZ
DJA
∅
FITZ30.44241.4a

P2016/12/17 10:57:13.4-0.8

T

144.41.00mb 5.7
GFZ
AUST
∅
LUWI30.90275.5a

P2016/12/17 10:57:18.20.0

T

1540.51.20mb 6.6
GFZ
DJA
∅
CNB30.93186.6a

P2016/12/17 10:57:19.81.1

T

528.21.10mb 6.2
GFZ
AUST
∅
CAN30.98187.1a

P2016/12/17 10:57:20.21.1

T

642.41.30mb 6.2SC3
CAN
∅
MMRI31.34260.8a

P2016/12/17 10:57:22.50.4

T

1240.31.60mb 6.4
GFZ
DJA
∅
MULG31.56213.4a

P2016/12/17 10:57:22.9-1.2

T




KAN
∅
∅
WRKA31.70227.3m

P2016/12/17 10:57:24.5-0.9

T




MAD
AUST
∅
KKSI31.78269.3a

P2016/12/17 10:57:26.80.9

T

652.41.10mb 6.3
GFZ
∅
∅
HTT31.86203.5m

P2016/12/17 10:57:26.2-0.6

T




MAD
ADE
∅
BBOO32.57208.0a

P2016/12/17 10:57:32.4-0.6

T

1011.40.90mb 6.6
GFZ
AUST
∅
MILA32.67186.4a

P2016/12/17 10:57:35.91.9

T

564.62.70mb 5.9
GFZ
AUST
∅
BASI33.15258.2a

P2016/12/17 10:57:38.20.3

T

3396.81.20mb 7.1
GFZ
∅
∅
TOLI233.19278.9a

P2016/12/17 10:57:37.8-0.4

T

375.31.20mb 6.1
GFZ
∅
∅
JCJ33.28341.4a

P2016/12/17 10:57:38.8-0.3

T




NEIR
∅
∅
KAPI33.66267.7a

P2016/12/17 10:57:42.40.1

T

550.81.20mb 6.3
GFZ
DJA
∅
SPSI33.67269.6a

P2016/12/17 10:57:42.1-0.3

T

457.61.00mb 6.3
GFZ
DJA
∅
TOO33.75191.5a

P2016/12/17 10:57:44.81.5

T

410.01.40mb 6.1
GFZ
AUST
∅
ARPS33.88196.9a

P2016/12/17 10:57:44.50.1

T

1879.30.90mb 6.9
GFZ
AUST
∅
FORT35.49219.6a

P2016/12/17 10:57:57.4-0.8

T

1951.30.60mb 7.2
GFZ
AUST
∅
AFI35.53107.7a

P2016/12/17 10:57:59.20.6

T

367.11.10mb 6.2
GFZ
WEL
∅
PLAI35.76261.2m

P2016/12/17 10:57:57.3-3.1

T




MAD
∅
∅
OUZ35.81151.2a

P2016/12/17 10:58:01.40.4

T

723.90.90mb 6.6
GFZ
WEL
∅
MYLDM36.28285.0a

P2016/12/17 10:58:07.12.3

T

963.61.30mb 6.6
GFZ
KLM
∅
TWSI36.63261.4a

P2016/12/17 10:58:07.0-0.8

T

633.31.10mb 6.4
GFZ
∅
∅
BKB36.70273.9a

P2016/12/17 10:58:09.61.2

T

761.12.30mb 6.2
GFZ
DJA
∅
MBWA36.75240.2a

P2016/12/17 10:58:07.8-1.1

T

857.12.00mb 6.3
GFZ
AUST
∅
JMZ37.11325.5a

P2016/12/17 10:58:12.70.8

T

1392.81.10mb 6.8
GFZ
JMA
∅
SRBI38.24262.7a

P2016/12/17 10:58:21.50.1

T

460.50.90mb 6.4
GFZ
DJA
∅
MOO38.22187.5a

P2016/12/17 10:58:23.01.5

T

1044.01.70mb 6.5
GFZ
AUST
∅
DNP38.28261.7a

P2016/12/17 10:58:22.40.7

T

1074.81.10mb 6.7
GFZ
DJA
∅
IGBI38.35261.5a

P2016/12/17 10:58:21.5-0.8

T

528.70.60mb 6.6
GFZ
DJA
∅
NIUE38.56115.2a

P2016/12/17 10:58:25.61.5

T

927.21.00mb 6.6
GFZ
AUST
∅
BBKI38.61270.1a

P2016/12/17 10:58:25.71.2

T

1310.91.40mb 6.6
GFZ
DJA
∅
TAU38.67187.3a

P2016/12/17 10:58:26.31.1

T

867.01.20mb 6.5
GFZ
TAU
∅
KKM38.71285.4a

P2016/12/17 10:58:26.00.6

T

531.11.10mb 6.3
GFZ
KLM
∅
MTKI38.75274.1a

P2016/12/17 10:58:25.80.2

T

436.01.50mb 6.1
GFZ
∅
∅
BYJI39.10262.5a

P2016/12/17 10:58:28.80.2

T

2317.41.30mb 6.9
GFZ
DJA
∅
HIZ39.08153.0a

P2016/12/17 10:58:29.20.6

T

1278.71.00mb 6.8
GFZ
WEL
∅
ABJI39.20263.2a

P2016/12/17 10:58:28.6-0.8

T

562.51.20mb 6.3
GFZ
DJA
∅
JAGI39.31262.1a

P2016/12/17 10:58:29.3-1.1

T

1322.21.30mb 6.6SC3
DJA
∅
JOW39.59323.3a

P2016/12/17 10:58:33.60.9

T

791.21.30mb 6.4SC3
JMA
∅
BLJI39.83263.3a

P2016/12/17 10:58:34.4-0.2

T

432.71.00mb 6.2
GFZ
DJA
∅
URZ39.94150.6a

P2016/12/17 10:58:34.9-0.8

T

747.31.00mb 6.4
GFZ
WEL
∅
MEEK39.97232.8a

P2016/12/17 10:58:35.0-0.9

T

1104.90.70mb 6.8
GFZ
AUST
∅
KMBL39.98224.3a

P2016/12/17 10:58:35.1-1.0

T

1826.41.20mb 6.8
GFZ
AUST
∅
GMJI40.00262.5a

P2016/12/17 10:58:34.9-1.2

T

417.91.30mb 6.1
GFZ
DJA
∅
QRZ40.04157.4a

P2016/12/17 10:58:37.40.8

T

1013.00.80mb 6.7
GFZ
WEL
∅
BKZ40.36152.0a

P2016/12/17 10:58:38.3-1.0

T

717.80.60mb 6.7
GFZ
WEL
∅
BWJI40.73266.3a

P2016/12/17 10:58:42.10.1

T

1933.61.20mb 6.8
GFZ
DJA
∅
GRJI40.91264.6a

P2016/12/17 10:58:45.31.7

T

513.91.20mb 6.2
GFZ
DJA
∅
KRKI40.98262.8a

P2016/12/17 10:58:39.5-4.6

T

179.40.70mb 6.0
GFZ
DJA
∅
INZ41.30159.9a

P2016/12/17 10:58:45.0-2.0

T




NEIR
∅
∅
SNZO41.32155.6a

P2016/12/17 10:58:47.30.2

T

1921.51.40mb 6.7
GFZ
WEL
∅
YOJ41.37315.6a

P2016/12/17 10:58:47.80.5

T

1621.90.90mb 6.8
GFZ
JMA
∅
BFZ41.46153.6a

P2016/12/17 10:58:46.9-1.4

T

897.60.50mb 6.8
GFZ
WEL
∅
FOZ41.49162.2m

P2016/12/17 10:58:47.3-1.2

T




NEIR
WEL
∅
PWJI41.62263.0a

P2016/12/17 10:58:48.0-1.3

T

1291.01.00mb 6.7
GFZ
DJA
∅
KHZ41.80157.6a

P2016/12/17 10:58:50.8-0.2

T

1239.71.10mb 6.6
GFZ
WEL
∅
PBKI41.82271.0a

P2016/12/17 10:58:52.21.2

T

1822.71.10mb 6.8
GFZ
DJA
∅
SBUM41.86278.7a

P2016/12/17 10:58:51.90.6

T

768.02.10mb 6.1
GFZ
KLM
CH
YULB41.93312.9a

P2016/12/17 10:58:51.90.0

T

823.40.90mb 6.5
GFZ
TATO
∅
NGJI41.93264.0a

P2016/12/17 10:58:52.70.8

T

573.11.30mb 6.2
GFZ
DJA
∅
JSU42.03330.0a

P2016/12/17 10:58:52.1-0.7

T

252.31.00mb 6.0
GFZ
JMA
∅
GIRL42.05240.8a

P2016/12/17 10:58:54.51.5

T

1591.31.40mb 6.6
GFZ
AUST
∅
RPZ42.06160.9a

P2016/12/17 10:58:52.4-0.8

T

7491.70.80
GFZ
WEL
∅
NACB42.19314.0a

P2016/12/17 10:58:54.40.4

T

1158.10.80mb 6.7
GFZ
TATO
∅
JOHN42.2459.1a

P2016/12/17 10:58:53.2-1.2

T

1941.71.60mb 6.7
GFZ
HON
∅
JMN42.33335.5a

P2016/12/17 10:58:55.1-0.2

T

235.90.80mb 6.0
GFZ
JMA
∅
TPUB42.36312.2a

P2016/12/17 10:58:55.1-0.4

T

790.50.80mb 6.6
GFZ
TATO
∅
LBZ42.38162.2a

P2016/12/17 10:58:54.4-1.4

T




NEIR
WEL
∅
SSLB42.42313.0a

P2016/12/17 10:58:56.50.6

T

552.60.80mb 6.4
GFZ
TATO
∅
UWJI42.43265.4a

P2016/12/17 10:58:57.61.7

T

998.41.40mb 6.4
GFZ
DJA
∅
WKZ42.44163.6a

P2016/12/17 10:58:56.80.5

T




NEIR
WEL
∅
INU42.58340.0a

P2016/12/17 10:58:57.0-0.3

T

151.70.80mb 5.8SC3
NGY
∅
MQZ42.59159.4a

P2016/12/17 10:58:56.0-1.4

T




NEIR
WEL
∅
YHNB42.65314.4a

P2016/12/17 10:58:59.01.1

T

755.90.40mb 6.8
GFZ
TATO
∅
JGF42.69340.5a

P2016/12/17 10:58:58.30.0

T

132.12.50
GFZ
JMA
∅
TATO42.76314.9a

P2016/12/17 10:58:59.71.0

T

1110.11.10mb 6.5
GFZ
TATO
∅
UGM42.88263.2a

P2016/12/17 10:59:01.41.8

T

1276.01.80mb 6.4
GFZ
∅
∅
SMRI42.94264.5a

P2016/12/17 10:59:00.80.7

T

983.61.30mb 6.4
GFZ
DJA
∅
KLBR43.05226.9a

P2016/12/17 10:58:59.4-1.7

T

1101.21.20mb 6.5
GFZ
AUST
∅
YOGI43.10263.4a

P2016/12/17 10:59:02.30.9

T

1164.22.10mb 6.2
GFZ
DJA
∅
MORW43.11231.2a

P2016/12/17 10:59:00.3-1.3

T

905.41.90mb 6.2
GFZ
AUST
∅
ODZ43.12162.2a

P2016/12/17 10:59:01.3-0.5

T

521.01.20mb 6.1
GFZ
WEL
∅
JNU43.15331.8a

P2016/12/17 10:59:00.9-1.0

T

672.40.90mb 6.4SC3
JMA
∅
MAJO43.28342.0a

P2016/12/17 10:59:01.5-1.5

T

146.60.90mb 5.7
GFZ
JMA
∅
BLDU43.33228.8a

P2016/12/17 10:59:01.9-1.4

T

698.81.30mb 6.2
GFZ
AUST
∅
KSM43.60276.8a

P2016/12/17 10:59:05.40.0

T

774.52.30mb 6.0
GFZ
KLM
∅
JHS43.74335.6a

P2016/12/17 10:59:06.3-0.4

T

183.00.80mb 5.9
GFZ
JMA
∅
JMM43.80345.4a

P2016/12/17 10:59:06.7-0.4

T

196.40.90mb 5.8
GFZ
JMA
∅
NWAO44.12225.6a

P2016/12/17 10:59:08.3-1.4

T

714.62.00mb 6.1
GFZ
AUST
∅
CTJI44.19264.6a

P2016/12/17 10:59:10.50.4

T

991.71.20mb 6.4
GFZ
∅
∅
SCJI44.22263.6a

P2016/12/17 10:59:10.50.2

T

976.01.10mb 6.5
GFZ
∅
∅
MUN44.38227.4m

P2016/12/17 10:59:10.6-1.1

T




MAD
AUST
∅
KPJI44.45264.1a

P2016/12/17 10:59:12.40.3

T

1466.30.80mb 6.8
GFZ
DJA
∅
JSD44.65342.8a

P2016/12/17 10:59:14.10.2

T

232.01.00mb 5.9
GFZ
JMA
∅
CMJI44.93263.5a

P2016/12/17 10:59:14.9-1.1

T

2814.70.90mb 7.0
GFZ
DJA
∅
JTU45.00331.5a

P2016/12/17 10:59:17.50.9

T

167.51.40mb 5.6
GFZ
JMA
∅
JCJI45.09265.3a

P2016/12/17 10:59:17.80.5

T

2206.90.90mb 6.9
GFZ
DJA
∅
RKGY45.21223.8a

P2016/12/17 10:59:18.2-0.2

T

1296.30.80mb 6.8
GFZ
AUST
∅
LEM45.74264.9a

P2016/12/17 10:59:22.90.3

T

851.10.80mb 6.6
GFZ
DJA
∅
CBJI46.51265.4a

P2016/12/17 10:59:29.20.8

T

1163.71.00mb 6.7
GFZ
DJA
∅
JTM46.51347.0a

P2016/12/17 10:59:29.71.1

T

94.50.70mb 5.8
GFZ
JMA
∅
TNG46.71265.8a

P2016/12/17 10:59:27.7-2.3

T

1094.70.50mb 7.0
GFZ
DJA
∅
SKJI46.80264.6a

P2016/12/17 10:59:31.50.8

T

1549.40.90mb 6.9
GFZ
DJA
∅
HKPS46.83306.3a

P2016/12/17 10:59:32.01.0

T

717.11.30mb 6.4
GFZ
∅
∅
SBJI47.23265.8a

P2016/12/17 10:59:32.4-1.6

T

305.11.50mb 6.0
GFZ
DJA
∅
TJN47.47331.2mceP2016/12/17 10:59:35.1-0.9

T




GSRC
∅
∅
BLSI48.12266.8a

P2016/12/17 10:59:39.8-1.1

T

367.61.20mb 6.1
GFZ
DJA
∅
RAR48.33114.5a

P2016/12/17 10:59:43.51.0

T

169.80.90mb 5.9
GFZ
WEL
∅
KLI48.52267.5a

P2016/12/17 10:59:42.8-1.1

T

576.01.30mb 6.3
GFZ
DJA
∅
PMBI48.69270.0a

P2016/12/17 10:59:46.10.9

T

1235.91.20mb 6.7
GFZ
DJA
∅
PMBI48.69270.0a

pP2016/12/17 11:00:06.40.8

T




NEIR
DJA
∅
INCN48.71331.4a

P2016/12/17 10:59:45.2-0.4

T

1143.21.00mb 6.8
GFZ
SEO
∅
YUK48.82352.7mceP2016/12/17 10:59:44.5-2.0

T




GSRC
SKHL
∅
KASI48.86266.6a

P2016/12/17 10:59:44.5-2.1

T

1233.70.90mb 6.8
GFZ
DJA
∅
DSRI49.07273.2a

P2016/12/17 10:59:48.0-0.2

T

475.81.30mb 6.3
GFZ
DJA
∅
MDSI49.21267.9a

P2016/12/17 10:59:47.1-2.1

T

583.31.20mb 6.4
GFZ
DJA
∅
TPRI49.27275.1a

P2016/12/17 10:59:49.5-0.2

T

707.62.30mb 6.2
GFZ
∅
∅
LWLI49.31267.2a

P2016/12/17 10:59:50.60.5

T

2052.70.90mb 7.1
GFZ
∅
∅
JKA49.40349.7a

P2016/12/17 10:59:51.10.2

T

298.70.80mb 6.3
GFZ
∅
∅
XMAS49.5183.5a

P2016/12/17 10:59:52.40.9

T

684.40.90mb 6.6
GFZ
∅
∅
JMBI49.90271.6a

P2016/12/17 10:59:57.02.5

T

560.41.10mb 6.4
GFZ
∅
∅
MYKOM50.05276.1a

P2016/12/17 10:59:55.60.0

T

408.41.20mb 6.2
GFZ
KLM
∅
BTDF50.07275.5a

P2016/12/17 10:59:55.5-0.3

T

201.70.70mb 6.2
GFZ
∅
∅
MCQ50.06175.8a

P2016/12/17 10:59:56.30.2

T

1512.01.00mb 6.9
GFZ
AUST
∅
MNAI50.43268.1a

P2016/12/17 10:59:57.6-0.9

T




KAN
DJA
∅
EGSI51.08266.7a

P2016/12/17 11:00:02.5-0.8

T

935.91.00mb 6.8
GFZ
∅
∅
UBSI51.14268.8a

P2016/12/17 11:00:02.3-1.5

T

810.11.20mb 6.6
GFZ
∅
∅
MASI51.20269.6a

P2016/12/17 11:00:02.7-1.6

T

640.90.70mb 6.7
GFZ
∅
∅
UBPT51.50293.5a

P2016/12/17 11:00:08.11.5

T

213.71.30mb 6.0
GFZ
∅
∅
YSS52.13350.7a

P2016/12/17 11:00:12.41.0

T

222.41.00mb 6.1SC3
SKHL
∅
SDSI52.17272.3a

P2016/12/17 11:00:10.4-1.1

T

1459.00.80mb 7.0
GFZ
DJA
∅
BKNI52.68273.8a

P2016/12/17 11:00:15.0-0.2

T

1316.61.00mb 6.9SC3
DJA
∅
PDSI53.14272.2a

P2016/12/17 11:00:16.2-2.4

T

1283.20.70mb 7.0
GFZ
∅
∅
IPM53.22279.0a

P2016/12/17 11:00:18.7-0.6

T

668.91.50mb 6.4
GFZ
KLM
∅
PPSI53.45269.9a

P2016/12/17 11:00:20.7-0.2

T

907.51.20mb 6.7
GFZ
DJA
∅
KULM53.72279.9a

P2016/12/17 11:00:22.2-0.7

T

806.81.40mb 6.6
GFZ
KLM
∅
KIP54.0959.5a

P2016/12/17 11:00:27.62.0

T

1232.71.60mb 6.7
GFZ
HON
∅
MNSI54.18274.2a

P2016/12/17 11:00:25.1-1.1

T

591.40.90mb 6.6
GFZ
DJA
∅
TRSI54.93275.6a

P2016/12/17 11:00:33.01.2

T

1465.90.80mb 7.1
GFZ
DJA
∅
SBSI54.95275.0a

P2016/12/17 11:00:27.2-4.6

T

866.61.20mb 6.7
GFZ
∅
∅
SLVN54.99299.9a

P2016/12/17 11:00:32.90.7

T

348.72.20mb 6.0
GFZ
PLV
∅
PSI55.05276.4a

P2016/12/17 11:00:31.1-1.6

T

2445.61.30mb 7.1
GFZ
DJA
∅
SKR55.032.0mdeP2016/12/17 11:00:32.70.1

T




GSRC
SKHL
∅
POHA55.6562.5a

P2016/12/17 11:00:39.11.9

T

2013.51.50mb 6.9
GFZ
HVO
∅
GSI56.23274.6a

P2016/12/17 11:00:39.2-1.7

T

1194.11.90mb 6.6
GFZ
DJA
∅
LASI56.23278.4a

P2016/12/17 11:00:41.70.7

T

2555.11.80mb 7.0
GFZ
∅
∅
KCSI56.30277.2a

P2016/12/17 11:00:39.2-2.3

T

769.80.90mb 6.7
GFZ
∅
∅
COCO56.54258.4a

P2016/12/17 11:00:44.71.5

T

1912.41.90mb 6.8SC3
AUST
∅
KLR56.78343.1mceP2016/12/17 11:00:44.1-1.0

T




GSRC
OBN
∅
PPTF57.24108.0a

P2016/12/17 11:00:50.22.0

T

484.11.40mb 6.3
GFZ
∅
∅
LHMI57.36279.1a

P2016/12/17 11:00:48.7-0.2

T

1777.50.90mb 7.1
GFZ
DJA
∅
PET57.493.7a

P2016/12/17 11:00:51.41.3

T

225.60.70mb 6.3SC3
KRSC
∅
PETK57.523.0a

P2016/12/17 11:00:49.0-1.4

T




NEIR
RIPT
∅
PEA0B57.523.0a

P2016/12/17 11:00:50.40.0

T




NEIR
RIPT
∅
MLSI57.75277.9a

P2016/12/17 11:00:49.7-2.0

T

1287.80.80mb 7.0
GFZ
∅
∅
CMAR58.43294.8m
iP2016/12/17 11:00:57.10.6

T




GSRC
OBN
∅
CHTO58.54295.2a

P2016/12/17 11:00:57.50.3

T

12.51.30
SC3
BKK
∅
SMY59.6414.4a

P2016/12/17 11:01:07.92.8

T

510.21.40mb 6.4SC3
PMR
∅
NPW61.36295.3a

P2016/12/17 11:01:17.40.9

T

969.71.00mb 6.8
GFZ
∅
∅
ADK61.6720.5a

P2016/12/17 11:01:19.10.3

T

513.91.50mb 6.4
GFZ
PMR
∅
ZEA62.08342.7mceP2016/12/17 11:01:20.9-0.7

T




GSRC
SKHL
∅
MA263.92358.5a

P2016/12/17 11:01:32.1-1.8

T

413.70.70mb 6.5
GFZ
NERS
∅
TAOE66.0697.7a

P2016/12/17 11:01:48.51.0

T

508.51.00mb 6.5
GFZ
PPT
∅
ULN66.13327.8a

P2016/12/17 11:01:47.8-0.6

T

234.11.90mb 5.8
GFZ
OBM
∅
SHL66.81300.2a

P2016/12/17 11:01:52.1-0.4

T

1070.91.10mb 6.7
GFZ
NDI
∅
UNV67.0824.4a

P2016/12/17 11:01:54.0-0.2

T




NEIR
GIA
∅
SEY67.26359.5mceP2016/12/17 11:01:53.5-1.9

T




GSRC
NERS
∅
AKUT67.5924.5a

P2016/12/17 11:01:58.61.2

T

639.81.40mb 6.4SC3
PMR
∅
CASY68.50197.2a

P2016/12/17 11:02:01.4-1.9

T

655.92.70mb 6.1
GFZ
AUST
∅
YAK68.83348.2a

P2016/12/17 11:02:04.3-0.9

T

361.61.10mb 6.2SC3
YARS
∅
SDPT70.6725.8a

P2016/12/17 11:02:16.1-0.3

T




NEIR
PMR
∅
CCD72.64187.8a

P2016/12/17 11:02:27.2-1.9

T




KAN
∅
∅
BILL72.935.0a

P2016/12/17 11:02:28.8-1.4

T

508.81.40mb 6.2
GFZ
NERS
∅
VNDA73.09178.1a

P2016/12/17 11:02:30.1-1.1

T

648.40.90mb 6.5
GFZ
WEL
∅
HALK73.53277.7a

P2016/12/17 11:02:33.80.6

T

209.82.10mb 5.6
GFZ
∅
∅
PALK73.65278.9a

P2016/12/17 11:02:34.50.6

T

256.11.10mb 6.0SC3
∅
II
SBA73.62177.1a

P2016/12/17 11:02:35.10.8

T

444.40.90mb 6.3
GFZ
WEL
∅
MALK73.94280.0a

P2016/12/17 11:02:35.90.3

T

398.61.10mb 6.2
GFZ
∅
∅
OHAK74.9826.8a

P2016/12/17 11:02:42.60.6

T

382.30.80mb 6.3SC3
PMR
∅
TNA75.3215.5ac
P2016/12/17 11:02:44.70.7

T




INGV
GIA
∅
KDAK75.6126.5a

P2016/12/17 11:02:45.90.3

T

374.21.30mb 6.1
GFZ
GIA
∅
AIS76.17232.2a

P2016/12/17 11:02:50.01.3

T

4661.11.80mb 7.1
GFZ
STR
∅
TTA77.2421.2ac
P2016/12/17 11:02:53.5-1.5

T




INGV
PMR
∅
DGZ78.29322.7mciP2016/12/17 11:02:59.2-1.6

T




GSRC
∅
∅
HIN79.6525.9a

pP2016/12/17 11:03:32.01.8

T




NEIR
AGS
∅
MKAR80.58318.8a

P2016/12/17 11:03:12.0-1.1

T

1882.00.80mb 7.0
GFZ
NNC
KZ
MK3180.58318.8m
iP2016/12/17 11:03:12.1-1.0

T




GSRC
NNC
∅
KAAM80.65271.2a

P2016/12/17 11:03:15.32.2

T

812.81.30mb 6.4
GFZ
∅
∅
MAKZ80.79318.8a

P2016/12/17 11:03:13.2-1.0

T

814.21.30mb 6.4
GFZ
NNC
II KZ
HMDM81.02277.6a

P2016/12/17 11:03:16.71.6

T

931.71.20mb 6.5
GFZ
∅
∅
SHLS81.25314.8m
eP2016/12/17 11:03:16.6-0.3

T




GSRC
∅
∅
ZALV81.30326.2m
iP2016/12/17 11:03:14.5-2.4

T




GSRC
RIPT
∅
COLA81.3221.6a

P2016/12/17 11:03:14.5-2.6

T

708.41.00mb 6.5
GFZ
NEIC
∅
PDGK81.57314.9m
iP2016/12/17 11:03:17.2-1.0

T




GSRC
NNC
KZ
UZB81.86314.6m
eP2016/12/17 11:03:19.3-0.7

T




GSRC
∅
∅
KPKS82.17314.9m
eP2016/12/17 11:03:22.10.5

T




GSRC
∅
∅
PAF82.24220.9a

P2016/12/17 11:03:22.70.8

T

6412.51.30
GFZ
STR
∅
TARG82.41313.0a

P2016/12/17 11:03:22.9-0.2

T

347.71.20mb 6.1
GFZ
∅
∅
ASAI83.18312.0a

P2016/12/17 11:03:26.8-0.3

T

526.72.10mb 6.2
GFZ
∅
∅
AAA83.36314.4m
eP2016/12/17 11:03:28.81.1

T




GSRC
KAZK
∅
EGAK83.8123.0a

P2016/12/17 11:03:29.3-0.8

T

360.11.20mb 6.2
GFZ
GIA
∅
CRAG84.3733.2ad
PcP2016/12/17 11:03:34.0-2.4

T




INGV
PMR
∅
CRAG84.3733.2a

P2016/12/17 11:03:35.12.3

T

113.52.10mb 5.5SC3
PMR
∅
AAK85.00313.4a

P2016/12/17 11:03:35.7-0.4

T

2335.11.10mb 7.1
GFZ
KYRG
II
SGDS85.05314.2m
eP2016/12/17 11:03:35.5-0.8

T




GSRC
∅
∅
WHY85.0127.9a

P2016/12/17 11:03:35.9-0.4

T

149.52.10mb 5.6
GFZ
OTT
∅
BTLS85.76315.7m
eP2016/12/17 11:03:38.6-1.1

T




GSRC
∅
∅
NRIK85.89341.0mceP2016/12/17 11:03:38.1-2.4

T




GSRC
∅
∅
MAW86.08202.5a

P2016/12/17 11:03:39.7-1.9

T

156.40.90mb 6.0
GFZ
AUST
∅
OTUK87.47318.7m
iP2016/12/17 11:03:45.0-3.1

T




GSRC
∅
∅
HOPS87.7650.7a

pP2016/12/17 11:04:15.23.5

T




NEIR
BRK
∅
KK3187.96313.4m
iP2016/12/17 11:03:48.8-1.6

T




GSRC
NNC
∅
INK87.9220.8a

P2016/12/17 11:03:48.3-2.1

T

281.41.30mb 6.2
GFZ
OTT
∅
KBL88.01304.8a

P2016/12/17 11:03:48.9-1.9

T

165.30.90mb 6.1
GFZ
∅
∅
IUG88.19312.4m
eP2016/12/17 11:03:51.1-0.5

T




GSRC
∅
∅
COR88.3345.1a

P2016/12/17 11:03:52.80.7

T

59.31.00mb 5.6
GFZ
COR
∅
NLWA88.3342.3ac
P2016/12/17 11:03:52.80.6

T




INGV
NEIC
∅
NLWA88.3342.3ad
PcP2016/12/17 11:03:53.0-0.9

T




INGV
NEIC
∅
CHGR88.41308.9a

P2016/12/17 11:03:51.5-1.0

T

1751.21.00mb 7.1
GFZ
∅
∅
TAS88.63311.5a

P2016/12/17 11:03:55.11.6

T

410.82.30mb 6.1SC3
UZBK
∅
BRVK89.49323.3a

P2016/12/17 11:03:55.2-2.5

T

645.91.10mb 6.7
GFZ
NNC
II KZ
EMB90.0651.0a

pP2016/12/17 11:04:26.03.2

T




NEIR
REN
∅
WVOR91.4747.7a

P2016/12/17 11:04:06.6-0.3

T

59.11.00mb 5.8
GFZ
NEIC
∅
TKX92.3857.6a

pP2016/12/17 11:04:36.63.3

T




NEIR
∅
∅
PFO92.5756.6a

P2016/12/17 11:04:12.00.1

T

54.21.20mb 5.7
GFZ
LJC
∅
HLID94.6346.7a

P2016/12/17 11:04:21.60.0

T

26.42.10
GFZ
NEIC
∅
Y14A95.4656.4a

pP2016/12/17 11:04:50.63.1

T




NEIR
FLAG
∅
RER95.67248.2a

pP2016/12/17 11:04:50.01.6

T




NEIR
PAR
∅
DUG95.7550.1a

P2016/12/17 11:04:26.4-0.2

T

25.92.10mb 5.4
GFZ
SLC
∅
ARU96.45326.2a

P2016/12/17 11:04:26.2-3.6

T

196.11.10mb 6.6
GFZ
OBN
II
HWUT96.7048.7a

P2016/12/17 11:04:30.8-0.2

T

24.00.90mb 5.7
GFZ
SLC
∅
AKTK96.95320.2m
iP2016/12/17 11:04:27.8-4.2

T




GSRC
NNC
KZ
AHID97.0447.5a

P2016/12/17 11:04:32.60.0

T

20.81.00mb 5.6
GFZ
SLC
∅
TUC97.2958.1a

P2016/12/17 11:04:35.52.1

T

16.91.90
GFZ
NEIC
∅
SLBS97.8966.8a

P2016/12/17 11:04:34.3-1.7

T

17.61.30mb 5.5
GFZ
ECX
∅
X18A98.0055.8a

pP2016/12/17 11:05:02.63.4

T




NEIR
FLAG
∅
UOSS98.56294.5a

P2016/12/17 11:04:37.7-1.2

T

92.61.60mb 6.1
GFZ
∅
∅
MVCO99.1453.1a

P2016/12/17 11:04:43.11.2

T

32.21.30mb 5.8
GFZ
NEIC
∅
ANMO100.8655.3mdeP2016/12/17 11:04:50.71.2

T




GSRC
ALQ
∅
KIRV101.13328.9mceP2016/12/17 11:04:49.1-1.7

T




GSRC
RMOD
∅
ISCO101.2850.4a

P2016/12/17 11:04:52.81.2

T

12.81.10
GFZ
NEIC
∅
MNTX101.8958.6a

P2016/12/17 11:04:56.32.5

T

8.71.60
GFZ
∅
∅
RSSD102.1045.9a

P2016/12/17 11:04:55.1-0.1

T

29.80.80
GFZ
NEIC
∅
SNAA102.34187.4a

P2016/12/17 11:04:54.7-1.9

T

72.51.20
GFZ
AWIB
∅
NOR102.73358.5a

P2016/12/17 11:04:56.5-1.6

T

23.31.30
GFZ
DNK
∅
VNA3103.51185.5a

P2016/12/17 11:04:59.6-2.1

T

78.00.90
GFZ
AWIB
∅
VNA2103.58186.3a

P2016/12/17 11:05:00.2-1.8

T

65.01.10
GFZ
AWIB
∅
VOI103.86246.0a

P2016/12/17 11:05:02.5-0.1

T

39.71.50
GFZ
∅
∅
ABPO103.91249.2a

P2016/12/17 11:05:03.00.1

T

27.41.70
GFZ
TAN
∅
VNA1103.92186.1a

P2016/12/17 11:05:02.4-1.1

T

148.51.20
GFZ
AWIB
∅
TULEG104.329.3a

P2016/12/17 11:05:02.2-3.0

T

44.61.40
GFZ
OTT
∅
KMBO116.18266.5a

PKPdf2016/12/17 11:09:44.30.8

T




NEIR
NAI
GE IU
ANTO116.23312.6a

PKPdf2016/12/17 11:09:43.1-0.5

T




NEIR
DDA
TU
WCI116.3549.2a

PKPdf2016/12/17 11:09:42.8-0.9

T




NEIR
SLM
∅
BOSA120.40232.9a

PKPdf2016/12/17 11:09:50.4-1.2

T




NEIR
PRE
∅
SSPA121.6344.1a

PKPdf2016/12/17 11:09:53.0-0.9

T




NEIR
SCP
∅
JTS121.9680.7a

PKPdf2016/12/17 11:09:54.70.4

T




NEIR
HDC
∅
MBAR122.72266.4a

PKPdf2016/12/17 11:09:56.10.2

T




NEIR
ENT
II
KHC124.00329.5mceP2016/12/17 11:09:57.5-1.1

T




GSRC
GFU
CZ
GRFO124.80331.2a

PKPdf2016/12/17 11:09:59.5-0.6

T




NEIR
GRF
IU GR
HRV124.9839.5a

PKPdf2016/12/17 11:10:00.50.2

T




NEIR
CAM
∅
ESK125.88343.9a

PKPdf2016/12/17 11:10:02.1-0.1

T




NEIR
BGS
II
LCO126.09131.2a

PKPdf2016/12/17 11:10:01.7-1.1

T




NEIR
DTM
∅
BFO127.11331.6a

PKPdf2016/12/17 11:10:03.6-1.0

T




NEIR
KRW
GR
NNA127.47108.8a

PKPdf2016/12/17 11:10:05.70.8

T




NEIR
LIM
∅
GIVF127.38335.2a
eP2016/12/17 11:10:04.8-0.3

T

125.51.16
LDG
LDG
∅
CDF127.55332.3a
eP2016/12/17 11:10:04.7-0.8

T

85.91.32
LDG
LDG
∅
BAIF127.67335.6a
eP2016/12/17 11:10:05.4-0.2

T

104.21.40
LDG
LDG
∅
HINF128.17332.1a
eP2016/12/17 11:10:06.90.3

T

153.21.28
LDG
LDG
∅
HAU128.27332.5a
eP2016/12/17 11:10:06.3-0.5

T

170.41.36
LDG
LDG
∅
MEZF128.49333.8a
eP2016/12/17 11:10:07.30.1

T

235.41.36
LDG
LDG
∅
LOR129.94333.5a
eP2016/12/17 11:10:10.00.0

T

71.31.16
LDG
LDG
∅
SSF130.26333.6a
eP2016/12/17 11:10:08.9-1.6

T

78.71.00
LDG
LDG
∅
MBDF130.40329.3a
eP2016/12/17 11:10:07.1-3.9

T

43.21.00
LDG
LDG
∅
SMF130.42333.0a
eP2016/12/17 11:10:10.8-0.1

T

145.11.28
LDG
LDG
∅
AVF130.53333.4a
eP2016/12/17 11:10:11.50.5

T

30.81.00
LDG
LDG
∅
LDF130.56337.3a
eP2016/12/17 11:10:10.6-0.5

T

244.91.88
LDG
LDG
∅
FLN130.56337.7a
eP2016/12/17 11:10:10.9-0.2

T

296.81.80
LDG
LDG
∅
SBF130.66328.0a
eP2016/12/17 11:10:10.9-0.4

T

57.00.80
LDG
LDG
∅
PGF130.68325.8a
eP2016/12/17 11:10:11.40.0

T

194.00.96
LDG
LDG
∅
ORIF130.72330.1a
eP2016/12/17 11:10:11.50.0

T

71.40.80
LDG
LDG
∅
VIVF131.36330.8a
eP2016/12/17 11:10:09.3-3.3

T

57.90.96
LDG
LDG
∅
TCF131.42333.8a
eP2016/12/17 11:10:13.00.2

T

87.20.92
LDG
LDG
∅
LMR131.51328.2a
eP2016/12/17 11:10:11.2-1.6

T

129.61.00
LDG
LDG
∅
SGMF131.75338.8a
eP2016/12/17 11:10:13.2-0.2

T

37.20.88
LDG
LDG
∅
ROSF131.93339.4a
eP2016/12/17 11:10:14.50.8

T

102.31.56
LDG
LDG
∅
MFF132.18335.8a
eP2016/12/17 11:10:13.5-0.7

T

90.71.32
LDG
LDG
∅
QUIF132.25339.1a
eP2016/12/17 11:10:15.41.1

T

44.61.08
LDG
LDG
∅
LASF132.33330.7a
eP2016/12/17 11:10:14.1-0.4

T

100.10.88
LDG
LDG
∅
RJF132.49333.5a
eP2016/12/17 11:10:13.5-1.3

T

278.52.08
LDG
LDG
∅
LFF133.12333.7a
eP2016/12/17 11:10:15.2-0.7

T

35.30.92
LDG
LDG
∅
EPF134.79332.4a
eP2016/12/17 11:10:19.90.8

T

32.61.04
LDG
LDG
∅
SJPF135.43333.7a
eP2016/12/17 11:10:19.9-0.4

T

24.40.80
LDG
LDG
∅
PAB139.69333.4a

PKPdf2016/12/17 11:10:26.5-1.7

T




NEIR
MDD
IU
CDVI140.4567.3a

PKPdf2016/12/17 11:10:29.20.1

T




NEIR
RSPR
∅
BOAV146.1692.4a

PKPdf2016/12/17 11:10:37.0-2.1

T




NEIR
∅
∅
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