FDSN is moving to use Digital Object Identifers for network citations. If you are looking for (or want to update) the citation information for a particular network, please look in the network listings first.
As the distribution of seismic data becomes simpler and more widespread, the International Federation of Digital Seismographic Networks (FDSN) is developing a mechanism whereby people requesting and receiving data from a given network are periodically reminded of the network from which their data originated. In this manner, proper attribution can be given to the operating networks in scientific articles or reports.
The FDSN is compiling a set of citations that the various networks would like to have referenced whenever data from their network is used.
Here is the list of citations
Submit your data center or network’s citation
For more information about this service, please review this IRIS Data Services Electronic Newsletter article.
The Seismological Network of Albania was founded in 1974 and belongs to the Department of Seismology, Institute of Geosciences, Energy, Water and Environment, Polytechnic University of Tirana, Albania.
There are 7 TA legacy broadband stations operated and maintained by the Arizona Geological Survey. This network is referred to as the Arizona Broadband Seismic Network (ABSN) and was originally funded through a grant from FEMA.
The Arkansas Seismic Network (ASN) consists of six state-of-the-art permanent broadband seismic stations strategically placed within selected State Parks across Arkansas. The ASN was funded through the Arkansas Governor’s General Improvement Fund in response to the Magnet Cove earthquake swarm in 2008. The goal of the ASN is to establish better and more uniform earthquake detection outside of the New Madrid seismic zone (NMSZ). The network was installed in spring of 2010 and is seamlessly integrated with the regional and national seismic networks. The ASN is operated and maintained in cooperation with the Arkansas Geological Survey (AGS), Center for Earthquake Research and Information (CERI) at the University of Memphis and Arkansas State Parks (ASP). For more information:
http://www.geology.ar.gov/geohazards/ark_seismic_network.htm
Please include a citation to "OGS – Istituto Nazionale di Ocenografia e Geofisica Sperimentale/ IAA -Instituto Antartico Argentino" in your work. It would be helpful if you would send a citable reference for any publications that use ASAIN data to Milton Plasencia (mplasencia@inogs.it), who is maintaining a database of ASAIN data usage. Alternatively, you could send a paper reprint to him:
Milton Plasencia
Sezione Centro Ricerche Sismologiche
OGS – Istituto Nazionale di Oceanografia e Geofisica Sperimentale
Borgo Grotta Gigante 42c
34010 Sgonico (TS)
Italy
The Altay-Sayan Seismic Network was established in 1963, since 2002 converted to digital registration. Nowadays the network consists of 35 seismic stations; most of the stations have real-time data transmission. The Altay-Sayan Seismic Network is operated by the Altay-Sayan Branch of the Geophysical Survey Siberian Branch of the Russian Academy of Sciences (ASB GS SB RAS).
The West Coast/Alaska Tsunami Warning Center (WC/ATWC) operates a network of seismometers in Alaska as part of its mission to issue tsunami warnings and information messages to its area-of- responsibility. The WC/ATWC is a part of the NOAA/National Weather Service.
Geoscience Australia operates the Australian National Seismic Network within Australia, its Territories and across its local region. The network supports the Joint Australian Tsunami Warning Centre, operated by Geoscience Australia and the Australian Bureau of Meteorology, which is responsible for issuing tsunami warning bulletins for Australia and its Territories. The network also contributes to monitoring earthquakes in the Australian region.
The Alaska Volcano Observatory (AVO) is a cooperative program of the United States Geological Survey (USGS), The Geophysical Institute of the University of Alaska Fairbanks (UAFGI) and the State of Alaska Division of Geological and Geophysical Surveys (ADGGS). AVO currently operates seismic networks on 27 historically active volcanoes in Alaska. More information is available at
The ANZA Seismic Network is a regional network of broadband seismometers and strong motion accelerometers operated by the Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego and funded by the USGS.
The Royal Observatory of Belgium (ROB) operates the Belgian seismic and accelerometric networks, as well as three short period seismometers in Luxembourg and one seismic station in the Netherlands. The ROB operates also a superconducting gravimeter.
The Black Forest Observatory is a geodynamic observatory operated jointly by both the Universities of Karlsruhe and Stuttgart, Germany.
The BK network includes the Berkeley Digital Seismic Network (BDSN) and some borehole sites in the Bay Area, operated by the UC Berkeley Seismological Laboratory (BSL). The BDSN is an array of high dynamic range, broadband seismometers with collocated strong-motion accelerometers in northern and central California. The borehole stations are deployed along the Hayward Fault at free-field and Bay Area bridge locations. See the BP network for information about the other borehole sites operated by BSL. If you use BK data, please include the following in the acknowledgments: "Data for this study comes from the Berkeley Digital Seismic Network operated by UC Berkeley Seismological Laboratory and archived at the Northern California Earthquake Data Center."
Pirchiner, M., B. Collaço, J. Calhau, M. Assumpção & J.C. Dourado, 2011. BRAzilian Seismographic Integrated Systems (BRASIS): infrastructure and data management. Annals of Geophysics, 54, 1, 2011; doi:10.4401/ag-4865
The High Resolution Seismic Network is operated by the UC Berkeley Seismological Laboratory. Located in Parkfield, California, the HRSN is a small network of closely spaced 3-component borehole sensors. If you use BP data, please include the following in the acknowledgments: "Data for this study comes from the Berkeley Digital Seismic Network operated by UC Berkeley Seismological Laboratory and archived at the Northern California Earthquake Data Center".
ROCHA, M. P.; ASSUMPÇÃO, M. ; CARVALHO, J. M. ; BARBOSA, J. R. ; FRANÇA, G. S. L. A. ; BIANCHI, M. ; BARROS, L. V. ; AZEVEDO, P. A. ; COLLAÇO, B. B. . Intensificação do monitoramento sismológico nas Regiões Centro-Oeste e Norte do país pela implantação da Rede Sismográfica Brasileira (RSBR). In: XV Simpósio Nacional de Estudos Tectônicos, 2015, Vitória, ES. Anais do XV Simpósio Nacional de Estudos Tectônicos, 2015.
The Cascades Volcano Observatory (CVO) operates several seismic stations at two volcanoes; Mount St. Helens in Washington, and Three Sisters in Oregon. Seismic stations on these and other Cascade volcanoes are also operated by other groups, primarily the University of Washington. CVO is a node of the Pacific Northwest Seismograph Network, with data from ‘CC’ stations sent in real time to the PNSN for processing.
Moran, S.C., 2004, Seismic Monitoring at Cascade Volcanic Centers, 2004: Status and Recommendations: U.S. Geological Survey Scientific Investigations Report 2004-5211, 28 p.
The CH Seismic Network is the National network for Switzerland, comprising of broadband seismometers and strong motion accelerometers operated by the Swiss Seismological Service, ETH Zurich.
The Southern California Seismic Network (SCSN) is a cooperative project of Caltech and the US Geological Survey. The SCSN has benefited from numerous upgrade projects. TERRAscope, funded by the L. K. Whittier and ARCO Foundations, and NSF, provided the first 28 broadband and strong motion stations in the late 1980s and early 1990s. The TriNet project, 1997 to 2002, funded by FEMA, California OES, USGS, and other partners, increased the number of broadband and strong motion stations to 155 and significantly improved the data communications and processing infrastructure. The California Integrated Seismic Network (CISN) project of Caltech, CGS, USGS, and UC Berkeley (2001 to present) provides funds for continued operation of the SCSN, improved robustness, and migration of operations toward statewide processing. The Southern California Earthquake Data Center (SCEDC), funded by the Southern California Earthquake Center (SCEC) and other sources, holds the complete data archives for SCSN/CISN from 1932 to present. The SCSN operates one IRIS/GSN station, PAS in Pasadena, California. If you use SCSN data, please include a citation to "Southern California Seismic Network operated by Caltech and USGS" in your work.
http://www.scsn.org/
http://www.cisn.org
http://www.data.scec.org
The GSC currently makes digital data from the Canadian National Seismograph Network (CNSN) available FREE to anyone on the Internet. In order for us to maintain this service, we need to enlist the support of our users. Please include a citation to "The Geological Survey of Canada" in your work. It would be helpful if you would send a citable reference for any publications that use CNSN data to John Cassidy (cassidy@pgc.NRCan.gc.ca), who is maintaining a database of CNSN data usage. Alternatively, you could send a paper reprint to him:
Dr. John Cassidy
Pacific Geoscience Centre
P.O. Box 6000,
9860 West Saanich Road,
Sidney, B.C.
V8L 4B2
The latest information on CNSN data citation policy may be viewed on the Web at:
The CO Network is operated by the South Carolina Seismic Network (SCSN) at the University of South Carolina with financial support from the United States Geological Survey, the Savannah River Site, and the University of South Carolina.
The Czech Regional Seismic Network (CRSN) is a regional network of broadband seismometers operated by the Geophysical Institute, Academy of Sciences of the Czech Republic, Prague, and the Institute of Physics of the Earth, Masaryk University, Brno.
http://www.ig.cas.cz
http://www.ipe.muni.cz
The Irish Nationals Seismic Network (INSN ) monitors earthquakes that occur in the North East Atlantic as well as teleseismic events. The data collected by the INSN is available through the IRIS Data Management Center. The INSN is based in the Dublin Institute for Advanced Studies at the School of Cosmic Physics . The recent development and expansion of INSN to five permanent broadband seismic stations has been funded by the Irish Government. Please include a citation to "The Irish National Seismic Network (INSN)" in your published work. Please send a copy of any publications that use INSN data to Mr Thomas Blake, Director, INSN at tb@cp.dias.ie
The data contained herein comprise either MT time series and/or MT transfer functions acquired using instruments managed and operated by Oregon State University on behalf of the NSF EarthScope Program through a subcontract from IRIS, or instruments owned by Oregon State University and provided to investigators through the National Geoelectromagnetic Facility (ngf.coas.oregonstate.edu), or from instruments operated through the former University of Washington EMSOC instrument pool and (since 2011) managed and provided to investigators by Oregon State University. EarthScope and the National Geoelectromagnetic Facility are supported by the National Science Foundation.
Mount Erebus Volcano Observatory, operated by the New Mexico Institute of Mining and Technology under funding from the National Science Foundation Office of Polar Programs.
Aster, R., McIntosh, W., Kyle, P., Esser, R., Bartel, B., Dunbar, N., Johns, B., Johnson, J., Karstens, R., Kurnik, C.,McGowan, M., McNamara, S., Meertens, C., Pauly, B., Richmond, M., Ruiz, M., New instrumentation delivers multidisciplinary real-time data from Mount Erebus, Antarctica, EOS trans. AGU, 85, no. 10, 9 March, 2004.
Aster, R., Mah, S.Y., Kyle, P., McIntosh, W.., Dunbar, N., Johnson, J., Ruiz, M., McNamara, S., Very long period oscillations of Mount Erebus Volcano, J. Geophys. Res., 108 (B11), 2522, doi:10.1029/2002JB002101, 2003.
More information about ER can be found here:
Information about ET can be found here:
The UCLA Factor building is a 17-story moment-resisting steel frame structure with an embedded 72-channel accelerometer array. Since 2002, the array has been operated and maintained by personnel from the NSF UCLA Center for Embedded Networked Sensing and the USGS. If you use Factor Array data, please credit the NSF UCLA Center for Embedded Networked Sensing and the USGS ANSS program for financial support.
Kohler, M. D., P. M. Davis, and E. Safak, Earthquake and ambient vibration monitoring of the steel frame UCLA Factor building, Earthquake Spectra, 21, 715-736, 2005.
Information about the array can be found at
Programme GEOSCOPE
Département de Sismologie
Institut de Physique du globe de Paris
4, Place Jussieu
75252 Paris cedex 05
FRANCE
The latest information on GEOSCOPE data citation policy may be viewed on the Web at:
The University of Colorado was funded by NSF (EAR-0337206 and EAR-0538116) to analyze high-rate GPS data for seismic events. Methods to reduce the impact of multipath were supported by EAR-0003943. The analysis of Denali records was supported by a NSF graduate student research fellowship (Andria Bilich). The analysis of the Tokachi-Oki records was also supported by NEHRP USGS 05HQGR0015. Research collaboration with GSI and the University of Tokyo is gratefully acknowledged.
The raw GPS observations for the Denali event are archived at UNAVCO (http://www.unavco.org)
The raw GPS observations for the Tokachi-Oki event are archived at the Geographical Survey Institute of Japan (http://www.gsi.go.jp/ENGLISH/)
For additional details, please see
The GEOFON network is funded and operated by GFZ Potsdam, Germany, in co-operation with almost 50 institutions worldwide.
The Ghana Digital Seismic Network, funded by the Government of Ghana, consists of six Libra V-Sat broadband stations. Five of these seismic stations have been distributed along and around the active Akuapim fault zone in the south-eastern parts of Ghana. For a better coverage area,the other station have been located in the mid section of Ghana. The seismic data which is being generated will be used to obtain Ground Motion Estimates to generate a new National Seismic Hazard map to form the basis for the sustainable socio-economic mitigation of the hazard/risk through effective land use planning, sound engineerig practice etc. We are also commited to open data sharing within the Seismological community.
The Georgian national Seismic Network (GO) is a regional network of broadband and short period seismometers operated by the Seismic Monitoring Center, Institute of Earth Sciences, Ilia State University.
First station was founded in 1899 year in Tbilisi.
Data from the GS network are freely available from the U.S. Geological Survey Earthquake hazards Program, Geologic Hazards Science Center.
Global Seismographic Network is a cooperative scientific facility operated jointly by the Incorporated Research Institutions for Seismology (IRIS), the United States Geological Survey (USGS), and the National Science Foundation (NSF).
Duennebier, F.K., David W. Harris, James Jolly, James Babinec, David Copson, Kurt Stiffel, The Hawaii-2 Observatory Seismic System, IEEE Jnl. Ocean Engineering, V 27, # 2, pp 212-217, Apr 2002
The Hong Kong Observatory (HKO) operates the Hong Kong Seismograph Network and provides earthquake information services for Hong Kong.
For more information see:
The Seismological Network of A.U.TH. was founded in 1978 and belongs to the Department of Geophysics of the School of Geology of the Aristotle University of Thessaloniki, Greece. It consists of a network of 25 seismological stations, which covers the largest part of Greece. The primary target of the Seismological Station is the 24-hour monitoring of seismic activity in Greece and surrounding countries, as well as the dissemination of fast and reliable information about earthquakes to the authorities and the public.
For additional details, please see:
http://seismology.geo.auth.gr/ or
http://seismology.geo.auth.gr/the_seisnet/WEBSITE_2005/station_index_en.html
ISMN, Iranian Strong Motion Network, Road, Housing, and Urban Development Research Center, http://ismn.bhrc.ac.ir/
Global Seismographic Network is a cooperative scientific facility operated jointly by the Incorporated Research Institutions for Seismology (IRIS), the United States Geological Survey (USGS), and the National Science Foundation (NSF).
Project IDA operated a global network of digital LaCoste Romberg gravimeters from 1975-1995 with financial support from the Cecil and Ida Green Foundation for Earth Science and the US National Science Foundation. A complete description of the IDA La Coste network can be found in Eos, Transactions, April 22, 1986, Vol. 67, No. 16, Pages 203-212. Inquiries can be directed to Dr. Duncan Agnew, dagnew@ucsd.edu. These data may be obtained from the IRIS Data Management Center.
Project IDA currently operates a global network of broadband and very broadband seismometers for the IRIS Consortium. Project IDA is based at the Cecil and Ida Green Institute of Geophysics and Planetary Physics, Scripps Institution of Oceanography, University of California, San Diego.
The IU stations are the part of the Global Seismic Network (GSN) that are installed, maintained and operated by the USGS Albuquerque Seismological Laboratory.
See http://earthquake.usgs.gov/regional/asl/, http://www.liss.org
The IV network refers to the Italian national seismic network (Rete Sismica Nazionale, RSN) which consists of more than 300 stations in Italy. The sensors include short period, extended short period, broadband and very broadband types of instrumentation. In more than 100 stations, there are also strong motion instruments installed. The data loggers include both house made manufactured (GAIA) and commercial ones. The data transmission is insured through many means (satellite, wifi, dedicated phone lines, …). CGPS data loggers are co-located in many sites. The data are available through the European Integrated Data Archive (EIDA). If you use IV data, please include the following in the acknowledgments: “Data for this study comes from the Italian national seismic network operated by Istituto Nazionale di Geofisica e Vulcanologia and archived at the European Integrated Data Archive (EIDA).
IW network data are freely available from the U.S. Geological Survey’s Earthquake Hazards Program, Geologic Hazards Science Center.
The Central Asian Seismic network was organized for research on seismic activity in the Central Asian region.
The KIGAM Seismic Network is a international network of broadband seismometers, strong motion accelerometers and infrasound arrays operated by the Korea Institute of Geoscience and Mineral Resources (KIGAM).
The KNET Seismic Network is a regional network of broadband seismometers funded by IRIS and jointly operated by the IVTAN, KIS, and IGPP, SIO, UCSD.
Research Station RAS
The Kyrgyz Digital Network (KRNET) consists of 16 permanent broadband seismic stations 7 of which are equipped by the the GPRS-routers (under IRIS support) and transfer the data in the real time mode to the IRIS DMC.
The latest information on KZ and data availability may be viewed on the Web at:
Lamont-Doherty Cooperative Seismographic Network (LCSN) monitors earthquakes that occur primarily in the Eastern United States and make the data available to scientific community and to general public. The network is operated jointly by the Lamont-Doherty Earth Observatory (LDEO) and many other educational institutions and public organizations in the Eastern United States. LCSN is a component of the Advanced National Seismic System (ANSS). Major funds to operate the network have been provided by the US Geological Survey under the National Earthquake Hazard Reduction Program (NEHRP). Please include a citation to "The Lamont-Doherty Cooperative Seismographic Network (LCSN)" in your work. It would be helpful if you would send a citable reference for any publications that use LCSN data to Won-Young Kim (wykim@ldeo.columbia.edu). You could send a paper reprint to him:
Dr. Won-Young Kim
Lamont-Doherty Earth Observatory
of Columbia University
61 Route 9W,
Palisades, NY 10964-8000
USA
The latest information on LCSN and data availability may be viewed on the Web at:
Instituto Dom Luiz, Faculdade de Ciências, Universidade de Lisboa, Portugal
The Montana Regional Sesimograph Network monitors seismicity in the state of Montana (USA) and surrounding areas with support from the State of Montana, the U.S. Geological Survey, and the Confederated Salish and Kootenai Tribes.
The operation and maintenance of the Calipso Borehole Geophysical Instrument Facility on the Soufriere Hills Volcano was supported in part by NSF-1063248 from the EAR-IF program and several previously expired awards.
http://www.uta.edu/faculty/mattioli/research/CALIPSO/Intro.html
The north-eastern Mexico regional seismic network is operated by the Centro de Geociencias (CGEO) of the National Autonomous University of México (UNAM). This network monitors earthquake activity throughout the Sierra Madre Oriental and surrounded areas. This network is projected to complete 20 stations until 2014. It will include broadband and short period seismographs most of them in real time.
The Mediterranean Broad Band Seismographic Network Anno 2005/06
Salvatore Mazza, M. Olivieri, A. Mandiello, and P. Casale, chapter 9 of Earthquake Monitoring and Seismic Hazard Mitigation in Balkan Countries, Sprinter Sciences + Business B.V. 2008.
For information about Mednet:
Data from the CEUSN (N4) network were made freely available as part of the EarthScope USArray facility, operated by Incorporated Research Institutions for Seismology (IRIS) and supported by the National Science Foundation, under Cooperative Agreements EAR-0733069 and EAR-1261681.
Funded by European Commission, New Caledonia Broadband Seismic Network started in 2010. It is composed of seven stations (Broadband+strong motion) spread over New Caledonia, mainly in Loyalty islands and the southern part of mainland. All stations’ data is distributed at IRIS and stations are part of PTWC. For additional info/request, please email Pierre.Lebellegard@ird.fr.
The New England Seismic Network (NESN) monitors earthquakes that occur in New England and adjacent areas. The data collected by the NESN is available through the IRIS Data Management Center. The NESN is a part of the Advanced National Seismic System. Operation of the network has been funded by the US Geological Survey under the National Earthquake Hazard Reduction Program. Please include a citation to "The New England Seismic Network (NESN)" in your published work. Please send a copy of any publications that use NESN data to Dr. John Ebel at john.ebel.1@bc.edu.
The Centre for Geodesy and Geodynamics, under the National Space Research and Development Agency (NASRDA), has been managing the Nigerian National Network of Seismological Stations since 2006. Available data from the network is freely available to interested researchers since 2008. The network’s URL is under construction.
Saint Louis University monitors earthquakes in the central United States with support from Saint Louis University and the U. S. Geological Survey. Other stations sponsored by Saint Louis University are integral parts of the IRIS IU and USGS US networks. All data are available through the IRIS Data Management Center.
For information about the network and earthquake monitoring in the region:
The Nevada regional seismic network monitors earthquake activity throughout Nevada and many areas of Eastern California. The complete network includes about 450 channels of real-time waveform data collected from a variety of instrumentation. About 30 ANSS strong motion stations are now operating in the Reno-Carson City and Las Vegas urban areas.
NORSAR operates 3 seismic arrays (NOA, ARCES, SPITS) and one threcomponent station (JMIC) in Norway as part of its mission to operate and maintain IMS stations on Norwegian territory as well as providing a range of activities related to the verification of compliance with the CTBT.
Trampert J., Paulssen H., van Wettum A., Ritsema J., Clayton R., Castro R., Rebollar C., Perez-Vertti A., 2003. New array monitors seismic activity near Gulf of California, Mexico, Eos, 84, 4, pp 29,32.
The Austrian Seismic Network is operated by the Central Institute for Meteorology and Geodynamics (ZAMG) in Vienna, Austria, which also manages the Conrad Observatory. More on the observatory can be found on www.zamg.ac.at/conrad_observatory.
Information about the Central Institute for Meteorology and Geodynamics is available at:
The Oklahoma Seismic Network is managed and operated by the Oklahoma Geological Survey in the Mewbourne College of Earth and Energy at the University of Oklahoma.
OVSICORI-UNA. Universidad Nacional. Heredia. Costa Rica. 2346-3000.
URL:
Seismic data from the PB network were made freely available by the EarthScope Plate Boundary Observatory, which is funded by the National Science Foundation under Cooperative Agreement EAR-0732947 to UNAVCO, Inc.
Institute of Geophysics, Polish Academy of Sciences operates two seismic networks with network codes PL and PD.
The PL network is currently (Oct.2009) composed of 7 broadband stations contributing real time data and 6 short period sites with off-line data access.
URL:
The Romanian Seismic Network (ROSN) is a regional network of broadband seismometers and strong motion accelerometers operated by the National Institute for Earth Physics (NIEP), Bucharest, Romania. ROSN currently operates 60 seismic stations, 76 strong motion accelerometers networks, one seismic array in cooperation with AFTAC and one small aperture seismic array installed by NIEP in a national project framework.
The AGS / AER currently produces digital data from the Regional Alberta Observatory for Earthquake Studies Network (RAVEN) that is available free to anyone through IRIS DMC (http://www.iris.edu/ds/nodes/dmc/). If you use RAVEN data, please include a citation to "Regional Alberta Observatory for Earthquake Studies Network operated by The Alberta Geological Survey / Alberta Energy Regulator" in your work.
http://www.ags.gov.ab.ca/geohazards/earthquakes_project.html
http://www.aer.ca/
The SB network consists of data recorded at instrumented geotechnical test sites designed to improve our understanding of the effects of surface geology on strong ground motion. The instrumentation at these sites includes surface and borehole arrays of accelerometers and pore pressure transducers to record strong ground motions and excess pore pressure generation during large earthquakes. The sites are part of a research program, and improve our ability to predict dynamic soil behavior from future large earthquakes, and improve our understanding of the liquefaction phenomena.
The latest information on SB may be viewed on the Web at:
The latest information on SC may be viewed on the Web at:
Superconducting gravimeters: great tools for low frequency seismology
The latest information on SG may be viewed on the Web at:
The latest information on SJ may be viewed on the Web at:
Data from the TA network were made freely available as part of the EarthScope USArray facility, operated by Incorporated Research Institutions for Seismology (IRIS) and supported by the National Science Foundation, under Cooperative Agreements EAR-0323309, EAR-0323311, EAR-0733069, EAR-1261681.
The National Seismological Network of Costa Rica (RSN) is a joint effort between the Seismology, Volcanology, and Geophysics Laboratory of the School of Geology at the University of Costa Rica (UCR) and the Seismology and Volcanology Division of the Costa Rican Electricity Institute (ICE). The RSN seismic catalog extends from 1973 to the present.
Phone (506) 2253-8407
Fax: (506) 2253-2586
P.O.BOX 214-2060
Ciudad Universitaria Rodrigo Facio, San Pedro de Montes de Oca
Costa Rica.
Belongs to the Tajik Academy of Sciences of Republic of Tajikistan.
MASE (2007): Meso America Subduction Experiment. Caltech. Dataset. doi:10.7909/C3RN35SP
VEOX (2010): Veracruz-Oaxaca Subduction Experiment. Caltech. Dataset. doi:10.7909/C3MW2F2C
PeruSE (2013): Peru Subduction Experiment. Caltech. Dataset. doi:10.7909/C3H41PBZ
The latest information on TW and data availability may be viewed on the Web at:
Bureau of Economic Geology, The University of Texas at Austin (2016): Texas Seismological Network. doi:10.7914/SN/TX
Caribbean Andesite Lava Island Precision Seismo-geodetic Observatory
The Pacific Northwest Seismograph Network monitors seismicity in the states of Washington and Oregon (USA) with support from the U.S. Geological Survey, U.S. Department of Energy and the State of Washington. University of Oregon helps to operate stations in southern Oregon as part of the PNSN. (See UW citation)
The latest information on US and data availability may be viewed on the Web at:
The University of Utah Regional/Urban Seismic Network monitors seismicity in the Utah Region (with special focus on the Wasatch Front urban corridor of north-central Utah) and neighboring parts of the Intermountain Seismic Belt. Financial support is provided by the U.S. Geological Survey, including funding under the Advanced National Seismic System (ANSS), and by the State of Utah.
The seismological network in the southwest of Colombia (REDSW) Is a regional network founded in 1987 and restructured in 2008 with digital technology for the monitoring of seismic activity in southwestern Colombia, considered one of the most seismically active regions of the country and exchanges data with the National Seismological Network of Colombia (RSNC). It supports national and regional systems of disaster prevention and warning, providing information for timely attention in emergency situations in case of a strong earthquake.
The Pacific Northwest Seismic Network monitors seismicity in the states of Washington and Oregon (USA) with support from the U.S. Geological Survey, U.S. Department of Energy and the State of Washington.
The Western Mediterranean Seismic Network (WM) is a regional network of broadband seismometers and strong motion accelerometers operated by the Royal Spanish Navy Observatory (ROA) with the following partners: ROA, UCM (Complutense University of Madrid, Spain), GFZ (GeoForschungsZentrum Potsdam, Germany), UEVORA (Evora University, Portugal) and ISRABAT (Institu Scientifique of Rabat, Morocco). The WM network is deployed around the Ibero-Maghrebian region.
Earthquake data for the Yellowstone National Park and surrounding area provided courtesy of the Univeristy of Utah Seismograph Stations and the Yellowstone Volcano Observatory (a partnership of the University of Utah, the U.S.Geol. Survey and Yellowstone National Park).
The Seismology and Mathematical Geophysics research group within the Earth Physics area has broad interests ranging from elucidating lithospheric structures, to studying the inner core, to developing new methods for imaging Earth’s interior.
http://rses.anu.edu.au/research-areas/seismology-mathematical-geophysics
The Seismology and Mathematical Geophysics research group within the Earth Physics area has broad interests ranging from elucidating lithospheric structures, to studying the inner core, to developing new methods for imaging Earth’s interior.
http://rses.anu.edu.au/research-areas/seismology-mathematical-geophysics
Toomey, D.R., R.M. Allen, A.H. Barclay, S.W. Bell, P.D. Bromirski, R.L. Carlson, X. Chen, J.A. Collins, R.P. Dziak, B. Evers, D.W. Forsyth, P. Gerstoft, E.E.E. Hooft, D. Livelybrooks, J.A. Lodewyk, D.S. Luther, J.J. McGuire, S.Y. Schwartz, M. Tolstoy, A.M. Tréhu, M. Weirathmueller, and W.S.D. Wilcock. 2014. The Cascadia Initiative: A sea change in seismological studies of subduction zones. Oceanography 27(2):138 – 150
Wysession, M. E., K. M. Fischer, T. J. Clarke, G. I. Al-eqabi, M. J. Fouch, P. J. Shore, R. W. Valenzuela, A. Li, and J. M. Zaslow, Slicing into the Earth, Eos Trans. AGU, 77(48), 477-482, 1996.
Williams, M.C., Trehu, A.M., Braunmiller, J., Seismicity at the Cascadia plate boundary beneath the Oregon continental shelf, Bull. Seis. Soc. Am., v. 101, p. 940-950, 2011.
Wilson, C. K., C. H. Jones, A. F. Sheehan, P. Molnar, and O. Boyd, Distributed deformation in the lower crust and upper mantle beneath a continental strike-slip fault zone: Marlborough fault system, South Island, New Zealand, “Geology, 32, 837-840, 2004”:
http://www.colorado.edu/GeolSci/faculty/pdf/wilson_et_al_marlbor_geology04.pdf.
Abers, G.A., A. Ferris, M. Craig, H. Davies, A.L. Lerner-Lam, J.C. Mutter, and B. Taylor, Mantle compensation of a region of active metamorphic core complexes, Woodlark Rift, Papua New Guinea, Nature, 418, 862-865, 2002.
Stachnik, J. C., G. A. Abers, and D. Christensen (2004), Seismic attenuation and mantle wedge temperatures in the Alaska subduction zone, J. Geophys. Res., 109, B10304, doi:10310.11029/12004JB003018.
Technical report: Soosalu, H., Torfajokull 2002 – seismological project, Technical report, NVI Research Report 0302, 27 p., 2003. http://www.norvol.hi.is/pdf/torfa-tech-rep.pdf
Low-frequency earthquakes: Soosalu, H., R. Lippitsch and P. Einarsson, Low-frequency earthquakes at the Torfajokull volcano, south Iceland, submitted to J. Volcanol. Geotherm. Res., 2005.
High-frequency earthquakes: Lippitsch, R., R.S. White and H. Soosalu, Precise hypocentre relocation of microearthquakes in a high-temperature geothermal field: the Torfajokull central volcano, Iceland, Geophys. J. Intern., 160, 371-388, 2005.
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Data acquisition and analyses were supported by NSF grant EAR-0838467 and the Charles Darwin Foundation. The facilities of the IRIS Data Management System, and specifically the IRIS Data Management Center, were used for access to waveform and metadata required in this study. The IRIS DMS is funded through the National Science Foundation and specifically the GEO Directorate through the Instrumentation and Facilities Program of the National Science Foundation under Cooperative Agreement EAR-0004370.
Lerner-Lam, A., A. Sheehan, and E. Humphreys, Mantle structure at the edge of a craton: Seismological studies of the crust and upper mantle at the transition between the southern Rockies and the Great Plains, Rocky Mountain Geology, 33, 199-216, 1998.
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Ghosh, A., J. E. Vidale, J. R. Sweet, K. C. Creager, A. G. Wech, and H. Houston, 2010, Tremor bands sweep Cascadia, Geophys. Res. Lett., 37, L08301, doi:10.1029/2009GL042301, 1-5.
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The 2002-2003 W Anatolia Seismic Recording Experiment is supported by US NSF grant INT-0217493 at the Saint Louis Unversity and TUBITAK of Turkey at the Dokuz Eylul Universtiy. Short-period instrumentation is provided by the PASSCAL program. The data was collected by a dedicated field crew which includes N. Akyol (DEU), M. Fort (PASSCAL), B. J. Mitchell (SLU), and L. Zhu (SLU).
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Dhaka University Earth Observatory (DUEO) was established in 2003 under joint research program between Geology Department of Dhaka University, Bangladesh and Lamont Doherty Earth Observatory (LDEO) of Columbia University at New York, USA. DUEO is a consortium formed in co-operation with Rajshahi University, Khulna University, Chittagong University, Chittagong University of Engineering and Technology (CUET), Patuakhali Science and Technology University (PSTU), Shajalal University of Science and Technology (SUST).
DUEO operates network of 6 permanent seismic stations, 6 portable seismographs and 18 continuous geodetic GPS stations in the country. The objectives of the Observatory is to carryout research on crustal dynamics, plate motions and to monitor the seismic activity in Bangladesh and surrounding countries, as well as to disseminate information of earthquakes to the government and the public. Data is open to scientific community.
For additional information, please browse: http://sites.google.com/site/shadueo
Please include a citation to "Dhaka University Earth Observatory (DUEO)" in your work. It would be appreciated if you would send a citable reference for any publications that use DUEO data to Syed Humayun Akhter (shakhter@univdhaka.edu).
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IRIS Newsletter article: Kamchatka: Edge of the Plate Jonathan M. Lees, Mark Brandon, Jeffrey Park, Vadim Levin, Yale University Alexei Ozerov, Evgenii Gordeev, Russian Academy of Sciences http://www.iris.iris.edu/volume2000no1/page-17-19.htm
papers: Peyton, V., V. Levin, J. Park, M. T. Brandon, J. Lees, E. Gordeev, and A. Ozerov, Mantle flow at a slab edge: Seismic anisotropy in the Kamchatka region, Geophysical Research Letters, v28, 379-382, 2001. http://www.geology.yale.edu/~vadim/Kamchatka-GRL.pdf
Park, J., V. Levin, M. T. Brandon, J. M. Lees, V. Peyton, E. Gordeev, and A. Ozerov, A dangling slab, amplified arc volcanism, mantle flow and seismic anisotropy near the Kamchatka plate corner, Plate Boundary Zones, Seth Stein and Jeffrey Freymueller, editors, AGU Geodynamics Series No. 30, AGU, Washington DC, pp. 295-324, 2002.
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63 Short period instruments recording continuously for a two month period in central North Island, New Zealand. Instruments operated by the University of Cambridge.
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The UCR SGP network was used for a passive source study with 30 short-period L-22 seismometers from 2013-2014, using UCR/SCEC funds. Inquiries can be directed to Dr. David Oglesby, david.oglesby@ucr.edu. These data may be obtained from the IRIS Data Management Center.
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These studies were supported by the John D. and Catherine T. MacArthur Foundation, University of Rochester, and RIT. The facilities of the IRIS Data Management System, and specifically the IRIS Data Management Center, were used for access to waveform and metadata required in this study. The IRIS DMS is funded through the National Science Foundation and specifically the GEO Directorate through the Instrumentation and Facilities Program of the National Science Foundation under Cooperative Agreement EAR-0004370.
P. Bordoni, G. Di Giulio, J. A. Haines, F. Cara, G. Milana, and A. Rovelli (2010). Issues in choosing the references to use for spectral ratios from observations and modeling, at Cavola landslide northern Italy, Bulletin of the Seismological Society of America, 100-4, 1578-1613, doi:10.1785/0120090116
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Temporary seismic experiment was conducted from 2005 to 2008. 39 broadband seismic stations were placed at the North of Central Anatolia. The data of the experiment are used to investigate the velocity structure under the North Anatolian Fault region.
Abers, G.A., L. Auger, E. Syracuse, T. Plank, K.M. Fischer, C. Rychert, A. Walker, J.M. Protti, V. Gonzalez, W. Strauch and P. Perez, Imaging the subduction factory beneath Central America: The TUCAN Broadband Seismic Experiment, EOS Trans. AGU, Fall Meet. Suppl., 2004.
SEIS-UK is a NERC funded facility providing on-shore seismic equipment and expertise to UK based academics for research around the world.
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Array of 37 texans deployed for 2 days in a line north from the old dome and 8 three-component instruments deployed for 1+ months within and around the crater.
The support of National Science Foundation grant EAR-384 0635789; NERC grants NE/D008611/1, NE/D01039X/1, and NE/E007414/1 are gratefully acknowledged. The facilities of the IRIS Data Management System, and specifically the IRIS Data Management Center, were used for access to waveform and metadata required in this study. The IRIS DMS is funded through the National Science Foundation and specifically the GEO Directorate through the Instrumentation and Facilities Program of the National Science Foundation under Cooperative Agreement EAR-0004370.
Yang, Z., A. F. Sheehan, W. L. Yeck, K. C. Miller, E. A. Erslev, L. L. Worthington, and S. H. Harder (2012), Imaging basin structure with teleseismic virtual source reflection profiles, Geophys. Res. Lett., 39, L02303, doi:10.1029/2011GL050035.
http://onlinelibrary.wiley.com/doi/10.1029/2011GL050035/abstract
PLUME was funded by the French Ministère de la Recherche. Many thanks to the Centre National de la Recherche Scientifique (CNRS), to the Université de Polynésie Française (UPF), and to the Commissariat à l’Energie Atomique (CEA) for having made this experiment possible.
Yang, Z., A. F. Sheehan, W. L. Yeck, K. C. Miller, E. A. Erslev, L. L. Worthington, and S. H. Harder (2012), Imaging basin structure with teleseismic virtual source reflection profiles, Geophys. Res. Lett., 39, L02303, doi:10.1029/2011GL050035.
http://onlinelibrary.wiley.com/doi/10.1029/2011GL050035/abstract
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Array of Arrays: Elusive ETS in the Cascadia Subduction Zone
Big Skidder experiment: tracking non-volcanic tremor through beamforming
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Temporary CMG6-TD data from Aruba at the Meteorological Service of Aruba in collaboration with Rice Univ. Program ends October 2009.
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The facilities of IRIS Data Services, and specifically the IRIS Data Management Center, were used for access to waveform, metadata or products required in this study. The IRIS DS is funded through the National Science Foundation and specifically the GEO Directorate through the Instrumentation and Facilities Program of the National Science Foundation under Cooperative Agreement EAR-1063471. Some activities of are supported by the National Science Foundation EarthScope Program under Cooperative Agreements EAR-0733069, EAR-1261681.
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