FDSN

The Seismological Network of Albania was founded in 1974 and belongs to the Department of Seismology, Institute of Geosciences, Polytechnic University of Tirana, Albania. It comprises 13 seismological stations, seven of which are equipped with broadband sensors, 24 bits digitizers (Trident), transmitting in real time via satellite communications. For additional details, please see:
http://www.geo.edu.al/

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.
http://www.azgs.az.gov/

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

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).
http://gs.sbras.ru/en

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.
http://wcatwc.arh.noaa.gov

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.
http://www.ga.gov.au

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
http://www.avo.alaska.edu.

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.
http://eqinfo.ucsd.edu/

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.
http://www.seismologie.be

The Black Forest Observatory is a geodynamic observatory operated jointly by both the Universities of Karlsruhe and Stuttgart, Germany.
http://www-gpi.physik.uni-karlsruhe.de/pub/widmer/BFO/

Feng, M., S. Van der Lee and M. Assumpção, 2007. Upper mantle structure of South America from joint inversion of waveforms and fundamental-mode group velocities of Rayleigh waves. J. Geophys. Res.,112, B04312, doi:10.1029/2006JB004449

Assumpção, M., M. Heintz, A. Vauchez and M.Egydio-Silva, 2006. Upper mantle anisotropy in SE and Central Brazil from SKS splitting: Evidence of asthenospheric flow around a cratonic keel. Earth Planet. Sci. Lett., 250, 224-240, doi: 10.1016/j.epsl.2006.07.038.

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.

http://vulcan.wr.usgs.gov

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.
http://www.seismo.ethz.ch/

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:
http://earthquakescanada.nrcan.gc.ca/cite-eng.php

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
http://www.dias.ie/insn

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.
http://EMScope.org

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:
http://www.ees.nmt.edu/Geop/Erebus/erebus.html

Information about ET can be found here:
http://www.ceri.memphis.edu

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
http://factor.gps.caltech.edu

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:
http://geoscope.ipgp.fr

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
http://spot.colorado.edu/~kristine/gps_seismology.html

The GEOFON network is funded and operated by GFZ Potsdam, Germany, in co-operation with almost 50 institutions worldwide.
http://geofon.gfz-potsdam.de/geofon/

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.

http://earthquake.usgs.gov/monitoring/anss/

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).
http://www.iris.edu/hq/programs/gsn

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: http://www.hko.gov.hk/

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

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.
http://ida.ucsd.edu/

The IU stations are the part of the Global Seismic Network (GSN) that are installed, maintained and operated by the USGS Albuquerque Seismological Laboratory.
http://earthquake.usgs.gov/regional/asl/ and
http://www.liss.org

IW network data are freely available from the U.S. Geological Survey's Earthquake Hazards Program, Geologic Hazards Science Center.

http://earthquake.usgs.gov/monitoring/anss/

The Central Asian Seismic network was organized for research on seismic activity in the Central Asian region.
http://www.caiag.kg

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
http://www.gdirc.ru/index.htm

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. More detailed information can be found here:
http://www.seismo.kg

The latest information on KZ and data availability may be viewed on the Web at:
http://www.kndc.kz

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:
http://www.ldeo.columbia.edu/LCSN

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.

For information about the Montana Regional Sesimograph Network: http://mbmgquake.mtech.edu/

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.
http://www.geociencias.unam.mx

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: http://mednet.rm.ingv.it/

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.

View on the Web at http://www.seisme.nc

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.

Information about the NESN can be viewed on the Web at:
http://quake.bc.edu:8000/

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:
http://www.eas.slu.edu/Earthquake_Center/

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.
http://www.seismo.unr.edu

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.
http://www.norsardata.no.

http://www.ineter.gob.ni

Monitor de Sismos en Nicaragua:
http://www.ineter.gob.ni/geofisica/sis/monitor.html

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: http://www.zamg.ac.at

OVSICORI-UNA. Universidad Nacional. Heredia. Costa Rica. 2346-3000.

URL: http://www.ovsicori.una.ac.cr

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.
http://www.earthscope.org/observatories/pbo

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: http://www.igf.edu.pl

URL: http://www.rimes.int/

The latest information on RO and data availability may be viewed on the Web at:
http://www.infp.ro

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.
http://www.infp.ro

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:
http://nees.ucsb.edu/publications

The latest information on SC may be viewed on the Web at:
http://www.ees.nmt.edu/Geop/NM_Seismology.html

Superconducting gravimeters: great tools for low frequency seismology

The latest information on SG may be viewed on the Web at:
http://www.seismology.be

The latest information on SJ may be viewed on the Web at:
http://www.seismo.gov.rs

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.

The latest information on TJ may be viewed on the Web at: http://www.gst.tj/

The latest information on TO and data availability may be viewed on the Web at: http://www.tectonics.caltech.edu/

The latest information on TW and data availability may be viewed on the Web at:
http://bats.earth.sinica.edu.tw/

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)
http://www.ess.washington.edu/SEIS/PNSN

The latest information on US and data availability may be viewed on the Web at: http://earthquake.usgs.gov/anss/

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.
http://www.seis.utah.edu

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.
http://osso.univalle.edu.co/index.php/informacion

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.
http://www.pnsn.org

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 instruments used in the field program were provided by the PASSCAL facility of the Incorporated Research Institutions for Seismology (IRIS) through the PASSCAL Instrument Center at New Mexico Tech. Data collected during this experiment will be available through the IRIS Data Management Center. The facilities of the IRIS Consortium are supported by the National Science Foundation under Cooperative Agreement EAR-0004370.

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.

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.dtm.ciw.edu/research/HLP/

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.

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.

Sheehan, A. F., G. A. Abers, A. L. Lerner-Lam, and C. H. Jones, Crustal thickness variations across the Colorado Rocky Mountains from teleseismic receiver functions, J. Geophys. Res., 100, 20,391-20,404, 1995.

Ghosh, A., J. E. Vidale, J. R. Sweet, K. C. Creager, and A. G. Wech, 2009, Tremor patches in Cascadia revealed by seismic array analysis, Geophys. Res. Lett., 36, L17316, doi:10.1029/2009GL039080, 1-5.

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.

Gomberg, J. and the Cascadia 2007 and Beyond Working Group, 2010, Slow-slip phenomena in Cascadia from 2007 and beyond: A review, GSA Bulletin, 122 p. 963?978; doi: 10.1130/B30287.1.

Sheehan, A. F., C. H. Jones, M. K. Savage, S. Ozalaybey, and J. M. Schneider, Contrasting lithospheric structure beneath the Colorado Plateau and Great Basin: Initial results from Colorado Plateau - Great Basin PASSCAL experiment, Geophysical Research Letters, 24 (21), 2609-2612, 1997.

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).

Zhu, L., B. J. Mitchell, N. Akyol, I. Cemen, and K. Kekovali, 2006, Crustal Thickness Variation in the Aegean Region and its Implications for the Extension of Continental Crust, J. Geophys. Res., 111, B01301, doi:10.1029/2005JB003770.

Zhu, L., N. Akyol, B. J. Mitchell, and H. Sozbilir, 2006, Seismotectonics of Western Turkey from High Resolution Earthquake Relocations and Moment Tensor Determinations, Geophys. Res. Lett., 33, L07316, doi:10.1029/2006GL025842

Akyol, N., L. Zhu, B. J. Mitchell, H. Sozbilir, and K. Kekovali, 2006, Crustal Structure and Local Seismicity in Western Anatolia, Geophys. J. Int., 166, 1259-1269, doi:10.1111/j.1365-246X.2006.03053.x.

Nyblade, A.A., and C. A. Langston, Broadband seismic experiments probe the East African rift, EOS Trans. AGU,83,405-408, 2002.

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).

Boyd, O., C. H. Jones, A. F. Sheehan, Foundering Lithosphere Imaged Beneath the Southern Sierra Nevada, California, USA, Science, 305, 660-662, 2004.

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.

Levin, V., J. Park, J. Lees, M. T. Brandon, V. Peyton, E. Gordeev, and A. Ozerov, Crust and upper mantle of Kamchatka from teleseismic receiver functions, Tectonophysics, v358, 233-265, 2002.

Walker, K., Bokelmann, G., and Klemperer, S., Shear-wave splitting beneath the Snake River suggests a mantle upwelling beneath eastern Nevada, USA, Earth Planet. Sci. Lett., 222, 529-542.

Karlstrom, K. E., et al., Structure and evolution of the lithosphere beneath the Rocky Mountains: Initial results from the CD-ROM experiment, GSA Today, v. 12, no. 3, p. 4-10, March 2002.

Sheehan, A. F., V. Schulte-Pelkum, O. Boyd, and C. Wilson, Passive source seismology of the Rocky Mountain region, in The Rocky Mountain Region: An Evolving Lithosphere, Geophysical Monograph Series 154, 10.1029/154GM23, p.309-315, 2005.

O'Neel, S., Pfeffer W.T., Columbia Glacier IPY seismic experiement.

Walter, F., J. M. Amundson, M. Jason, S. O'Neel, M. Truffer, M. Fahnestock, and H. A. Fricker. 2012. Analysis of low-frequency seismic signals generated during a multiple-iceberg calving event at Jakobshavn Isbræ, Greenland J. Geophys. Res., 117, F1, F01036, 11 pp. doi: 10.1029/2011JF002132

Wilson et al., Broadband Seismic Background Noise at Temporary Seismic Stations Observed on a Regional Scale in the Southwestern United States, Bull. Seismol. Soc. Amer., v.92, n.8, p.3335-3341, 2002.

Wilson et al., Imaging crust and upper mantle seismic structure in the southwestern United States using teleseismic receiver functions, The Leading Edge, v.22, n.3, p.232-237, 2003

http://www.ees.nmt.edu/Geop/Ristra/ristra.html

Cornwell, D.G., Maguire, P.K.H., England, R.W. & Stuart, G.W. (2009) Imaging detailed crustal structure and magmatic intrusion across the Ethiopian Rift using a dense linear broadband array. Geochemisty, Geophysics, Geosystems, 11, doi:10.1029/2009GC002382

http://www.agu.org/pubs/crossref/2010/2009GC002637.shtml

Kohler, M. D., and B. C. Kerr, Report for passive data acquired in the 1998-1999 Los Angeles Region Seismic Experiment II: a transect from Santa Monica Bay to the Westernmost Mojave Desert, USGS Open-File Report, 02-329, 2002.

Fouch, M. J., K. M. Fischer, E. M. Parmentier, M. E. Wysession, and T. J. Clarke. Shear-wave splitting, continental keels, and patterns of mantle flow, J. Geophys. Res., 105, 6255-6275, 2000.

63 Short period instruments recording continuously for a two month period in central North Island, New Zealand. Instruments operated by the University of Cambridge.

French, S. W., K. M. Fischer, E. M. Syracuse, and M. E. Wysession , Crustal structure beneath the Florida-to-Edmonton broadband seismometer array, Geophys. Res. Lett., 36, L08309, doi:10.1029/2008GL036331, 2009. http://epsc.wustl.edu/seismology/FLED/

Rowe, C., Aster, R., Kyle, P., Schlue, J., Dibble, R., Broadband recording of Strombolian explosions and associated very-long-period seismic signals on Mount Erebus volcano, Ross Island, Antarctica, Geophys. Res. Lett., 25, 2297-2300, 1998.

http://www.ees.nmt.edu/Geol/volcanology/erebus.html

Masy, J.,Tabare, T., Ruiz, S., Bidimensional model in the colission zone of the Caribbean and South American Plate, along the Leeward Antilles and Trinidad (Work in Progress)

Creager, K. C. and T. Melbourne, 2007, Episodic Tremor and Slip in the Pacific Northwest, EarthScope OnSite Newsletter, Winter/Spring, p.1-2.

Rubinstein, J. L., M. La Rocca, J. E. Vidale, K. C. Creager and A. G. Wech, 2008, Tidal modulation of nonvolcanic tremor, Science, 319, 186-189.

Wech, A. G., and K. C. Creager, 2008, Automatic detection and location of Cascadia tremor, Geophys. Res. Lett., 34, doi:10.1029/2008GL035458, 1-5.

Wech, A. G., K. C. Creager and T. I. Melbourne, 2009, Seismic and geodetic constraints on Cascadia slow slip, J. Geophys. Res., 114, B10316, doi:10.1029/2008JB006090, 1-9.

Abers, G. A., L. S. MacKenzie, S. Rondenay, Z. Zhang, A. G. Wech, and K. C. Creager, 2009, Imaging the source region of Cascadia tremor and intermediate-depth earthquakes, Geology, 37, doi: 10.1130/G30143A.1, 1119-1122.

Gomberg, J. and the Cascadia 2007 and Beyond Working Group, 2010, Slow-slip phenomena in Cascadia from 2007 and beyond: A review, GSA Bulletin, 122 p. 963?978; doi: 10.1130/B30287.1.

Yeck, W. L., Sheehan, A. F., Anderson, M. L., Siddoway, C. S., Erslev, E., Harder, S. H., Miller, K. C., 2009, BASE Flexible Array preliminary lithospheric structure analysis: Eos, v. 90, n. 52, Fall Meet. Suppl., Abstract U53A-0055.

http://cires.colorado.edu/science/groups/sheehan/pubs/

Haslinger, F., C. Thurber, M. Mandernach and P. Okubo, Tomographic image of P-velocity structure beneath Kilauea's East Rift Zone and South Flank: seismic evidence for a deep magma body, Geophys. Res. Lett., 28, 375-378, 2001.

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.

http://www.ees.nmt.edu/Geol/volcanology/erebus.html

Tiberi, C., S. Leroy, E. d?Acremont, N. Bellahsen, C. Ebinger, A. Pointu, Structure of the northeastern Gulf of Aden from receiver functions, Geophys. J. Int., doi: 10.1111/j.1365-246X.2006.03294.x, 2007.

Wilson, C. K., C. H. Jones, and H. J. Gilbert, A single-chamber silicic magma system inferred from shear-wave discontinuities of the crust and uppermost mantle, Coso geothermal area, California, J. Geophysical Research, 108 [B5], 10.1029/2002JB001798, 2003.

F. Brenguier, P. Kowalski, T. Staudacher, V. Ferrazzini, F. Lauret, P. Boissier, P. Catherine, A. Lemarchand, C. Pequegnat, O. Meric, C. Pardo, A. Peltier, S. Tait, N. M. Shapiro, M. Campillo, and A. Di Muro, First Results from the UnderVolc High Resolution Seismic and GPS Network Deployed on Piton De La Fournaise Volcano (2012), Seismo. Res. Lett, Volume 83 · Number 1, 2012.

http://srl.geoscienceworld.org/content/83/1/97.extract

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

Cara F., G. Di Giulio, G. Milana, P. Bordoni, J. Haines and Antonio Rovelli, (2010), On the Stability and Reproducibility of the Horizontal-to-Vertical Spectral Ratios on Ambient Noise: Case Study of Cavola, Northern Italy, Bulletin of the Seismological Society of America, 100-3, 1263-1275, DOI: 10.1785/0120090086

J. Wang, F. Tilmann, R. S. White, and P. Bordoni, (2009). Application of frequency-dependent multi-channel Wiener filters to event detection in 2D three-component seismometer arrays, Geophysics, vol. 74, 6 , 133-141, doi 10.1190/1.3256282.

P. Bordoni, J. Haines, G. Di Giulio, G. Milana, P. Augliera, M. Cercato, L. Martelli, F. Cara, and the Cavola Experiment Team, (2007). Cavola experiment site: geophysical investigation and deployment of a dense seismic array on a landslide. Annals of Geophysics, 50, 5, 627-649.

http://legacy.ingv.it/roma/reti/rms/progetti/cavola/intro.htm

Waite, G. P., B. A. Chouet, and P. B. Dawson (2008), Eruption dynamics at Mount St. Helens imaged from broadband seismic waveforms: Interaction of the shallow magmatic and hydrothermal systems, J. Geophys. Res., 113, B02305, doi:10.1029/2007JB005259.

Van der Lee, S., F. Marone, M. van der Meijde, D. Giardini, A. Deschamps, L. Margheriti, P. Burkett, S.C. Solomon, P.M. Alves, M. Chouliaras, A. Eshwehdi, A.S. Suleiman, H. Gashut, M. Herak, R. Ortiz, J.M. Davila, A. Ugalde, J. Vila, K. Yelles, Eurasia-Africa Plate Boundary Region Yields New Seismographic Data, Eos Trans. AGU, 82, 637 645 646, 2001. http://www.seg.ethz.ch/

Margheriti ,L., S. Pondrelli, D. Piccinini, N. Piana Agostinetti, F.P. Lucente, A. Amato, P. Baccheschi, L. Giovani, S. Salimbeni, J. Park, M. Brandon, V. Levin, J. Plomerova, P. Jedlicka, L. Vecsey, V. Babuska, A. Fiaschi, B Carpani And P. Ulbricht (2006). The Subduction Structure of the Northern Apennines: Results from the RETREAT Seismic Deployment. Annals of Geophysics 49, N 4/5 August/October 2006 pp1005-1017

Schulte-Pelkum, V., G. Monsalve, A. Sheehan, M. R. Pandey, S. Sapkota, R. Bilham, and F. Wu, Imaging the Indian subcontinent beneath the Himalaya, Nature, v. 435, pp. 1222-1225, 30 June 2005, doi:10.1038/nature03678.

De la Torre, T. L., and A. F. Sheehan, Broadband seismic noise analysis of the Himalayan Nepal Tibet Seismic Experiment, Bull. Seismol. Soc. Am., v. 95, 1202-1208, June 2005, doi:10.1785/0120040098.

Sheehan, A. F., F. T. Wu, F. Blume, G. Monsalve, H. Gilbert, T. de la Torre, R. Bendick, V. Schulte-Pelkum, R. Bilham, G. C. Huang, M. R. Pandey, H. B. Liu, Himalayan Nepal Tibet broadband seismic experiment (HIMNT), Eos Trans. Am. Geophys. Union, Fall meeting 2002.

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.

Wech, A. G., and K. C. Creager, 2007, Cascadia tremor polarization evidence for plate interface slip , Geophys. Res. Lett., 34, doi:10.1029/2007GL031167, 1-6.

Rubinstein, J. L., M. La Rocca, J. E. Vidale, K. C. Creager and A. G. Wech, 2008, Tidal modulation of nonvolcanic tremor, Science, 319, 186-189.
Wech, A. G., and K. C. Creager, 2008, Automatic detection and location of Cascadia tremor, Geophys. Res. Lett., 34, doi:10.1029/2008GL035458, 1-5.

Wech, A. G., K. C. Creager and T. I. Melbourne, 2009, Seismic and geodetic constraints on Cascadia slow slip, J. Geophys. Res., 114, B10316, doi:10.1029/2008JB006090, 1-9.

Tiberi, C., Leroy, S., d'Acremont, E., Bellahsen, N., Ebinger, C., Al-Lazki, A. and Pointu, A., 2007. Crustal geometry of the northeastern Gulf of Aden passive margin: localization of the deformation inferred from receiver function analysis. Geophys. J. Int., 168(doi:10.1111/j.1365-246X.2006.03294.x): 1247-1260.

Lucazeau, F., Leroy, S., Bonneville, A., Goutorbe, B., Rolandone, F., d'Acremont, E., Watremez, L., Düsünur, D., Tuchais, P., Huchon, P., Bellahsen, N. & Al-Toubi, K. (2008). Persistent thermal activity at the Eastern Gulf of Aden after continental break-up, Nature Geosciences. 854-858

Basuyau, C. Tiberi, C., S. Leroy, G. Stuart, A. Al-Lazki, K. Al-Toubi, C. Ebinger, Evidence of partial melting beneath a continental margin: case of Dhofar, in the Northern Gulf of Aden (Sultanante of Oman), J. Geophys. Res.(in revision).

Tilmann, F.; Craig, T. J.; Grevemeyer, I.; Suwargadi, B.; Kopp, H. & Flueh, E., 2010, The updip seismic/aseismic transition of the Sumatra megathrust illuminated by aftershocks of the 2004 Aceh-Andaman and 2005 Nias events, Geophys. J. Int., 181, 1261-1274, doi:10.1111/j.1365-246X.2010.04597.x

http://dx.doi.org/10.1111/j.1365-246X.2010.04597.x

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.

Ebinger, C., Keir, D., Ayele, A., Belachew, M., Calais, E., Wright, T., Campbell, E., Buck, R., Magma intrusion and faulting processes in a zone of continental rupture: Seismicity of the Dabbahu (Afar) rift, Geophys. J. Int., doi: 10.1111/j.1365-246X.2008.03877.x, 2008.

Ebinger, C., A. Ayele, D. Keir, J.V. Rowland, G. Yirgu, T. Wright, M. Belachew, I. Hamling, Length and timescales of rift faulting and magma intrusion: the Afar rifting Cycle from 2005 to Present, Ann. Revs. Earth Planet Sci., 38, doi:10.1146/annrev-earth-040809-152333, 2010.

http://www.ees.rochester.edu/ebinger/SEARIFT.html

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. http://www.dstu.univ-montp2.fr/PERSO/barruol/polynesia/

Tolstoy, M., F. Waldhauser, D.R. Bohnenstiehl, R.T. Weekly, W.-Y. Kim, Seismic identification of along-axis hydrothermal flow on the East Pacific Rise, Nature, 451, doi:10.1038/nature06424, 2008.

Array of Arrays: Elusive ETS in the Cascadia Subduction Zone

Big Skidder experiment: tracking non-volcanic tremor through beamforming

Ghosh, A., J. E. Vidale, J. R. Sweet, K. C. Creager, and A. G. Wech, 2009, Tremor patches in Cascadia revealed by seismic array analysis, Geophys. Res. Lett., 36, L17316, doi:10.1029/2009GL039080, 1-5. [ PDF ]

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. [ PDF ]

Gomberg, J. and the Cascadia 2007 and Beyond Working Group, 2010, Slow-slip phenomena in Cascadia from 2007 and beyond: A review, GSA Bulletin, 122 p. 963?978; doi: 10.1130/B30287.1.

Temporary CMG6-TD data from Aruba at the Meteorological Service of Aruba in collaboration with Rice Univ.
Program ends October 2009.

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