https://m2.mtmt.hu/ hun 2026-09-22 05:02 JournalArticle 3273926 VALIDATED true N1 Funding details: ETH, Eidgenössische Technische Hochschule Zürich N1 Funding details: 200021_143467, SNF, Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung N1 Funding text: Comments by Roger Bilham and one anonymous reviewer helped to improve the manuscript and are thankfully acknowledged. We thank S. Schmid, J.-P. Burg, C. Cauzzi, and T. Tormann for helpful discussions. This work and the deployment of the temporary seismic GANSSER network in Bhutan were funded by the Swiss National Science Foundation (SNF), Grant 200021_143467 (G. Hetényi). The GANSSER acronym was chosen to commemorate the famous geologist Augusto Gansser (1910–2012). D. Grujic thanks the ETH Zurich Visiting Professorship Fund for financial support during the preparation of the manuscript at the Institute of Geophysics (ETH Zurich). The instrument pool of the SED and Seismology and Geodynamics (SEG) group at ETH Zurich provided the station hardware. We thank D. Drukpa and his colleagues at the Department of Geology and Mines of the Kingdom of Bhutan for support during the fieldwork. We thankfully acknowledge also the GANSSER fieldwork team. We thank S. Mitra from the Indian Institute of Science Education and Research Kolkata (IISER Kolkata) for providing phase data for selected events of stations in Sikkim and West Bengal. Moment tensor inversions were derived by the SCMTV-software provided by GFZ Potsdam/GEMPA GmbH. Megjegyzés-26723440 Group Author: GANSSER Working Grp Megjegyzés-26766825 Group Author: GANSSER Working Grp Megjegyzés-26766826 Group Author: GANSSER Working Grp Megjegyzés-26767115 Group Author: GANSSER Working Grp Megjegyzés-26876796 Group Author: GANSSER Working Grp Swiss Seismological Service, ETH-Zürich, Zurich, 8092, Switzerland Institute of Geophysics, ETH-Zürich, Zurich, 8092, Switzerland Institute of Earth Sciences, University of Lausanne1015, Switzerland Department of Earth Sciences, Dalhousie University, Halifax, NS B3H 4R2, Canada Cited By :22 Export Date: 13 January 2021 Correspondence Address: Diehl, T.; Swiss Seismological Service, ETH-ZürichSwitzerland; email: tobias.diehl@sed.ethz.ch Funding details: Eidgenössische Technische Hochschule Zürich, ETH Funding details: Indian Institute of Science Education and Research Kolkata, IISER-K Funding details: Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, SNF Funding details: Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung, SNF, 200021_143467 Funding details: Indian Institute of Science Education and Research Kolkata, IISER-K Funding text 1: Comments by Roger Bilham and one anonymous reviewer helped to improve the manuscript and are thankfully acknowledged. We thank S. Schmid, J.-P. Burg, C. Cauzzi, and T. Tormann for helpful discussions. This work and the deployment of the temporary seismic GANSSER network in Bhutan were funded by the Swiss National Science Foundation (SNF), Grant 200021_143467 (G. Het?nyi). The GANSSER acronym was chosen to commemorate the famous geologist Augusto Gansser (1910?2012). D. Grujic thanks the ETH Zurich Visiting Professorship Fund for financial support during the preparation of the manuscript at the Institute of Geophysics (ETH Zurich). The instrument pool of the SED and Seismology and Geodynamics (SEG) group at ETH Zurich provided the station hardware. We thank D. Drukpa and his colleagues at the Department of Geology and Mines of the Kingdom of Bhutan for support during the fieldwork. We thankfully acknowledge also the GANSSER fieldwork team. We thank S. Mitra from the Indian Institute of Science Education and Research Kolkata (IISER Kolkata) for providing phase data for selected events of stations in Sikkim and West Bengal. Moment tensor inversions were derived by the SCMTV-software provided by GFZ Potsdam/GEMPA GmbH. 0 2018-10-02T08:54:25.000+0000 false 3273926 2026-05-17T23:46:00.104+0000 2025-01-08T11:27:54.386+0000 2017-10-03T11:40:33.000+0000 true 10001690 Hetényi György /api/author/10001690 Author true 10001690 2024-11-14T18:51:29.136+0000 2018-03-12T14:38:06.000+0000 true 10017066 Vasvári Lilian /api/admin/10017066 Admin true 10017066 2025-01-08T11:27:54.648+0000 true 10003134 Wolf György /api/admin/10003134 Admin true 10003134 Admin 10067876 /api/admin/10067876 Ladányi Gusztáv true true 2025-01-02T12:11:03.448+0000 true false true 24 24 /api/publicationtype/24 PublicationType 1 true 24 JournalArticle true 10000059 Article true 24 24 /api/publicationtype/24 PublicationType 1 true 24 JournalArticle /api/subtype/10000059 Szakcikk SubType 101 true 10000059 true 1 /api/category/1 Category true 1 Diehl, T Seismotectonics of Bhutan: Evidence for segmentation of the Eastern Himalayas and link to foreland deformation true true /api/journal/1358 REVIEWED true false 1358 false 1358 true 0012-821X 1385-013X Journal FOREIGN 471 54 64 54 11 2017 The instrumental record of Bhutan is characterized by a lower seismicity compared to other parts of the Himalayan arc. To understand this low activity and its impact on the seismic hazard, a seismic network was installed in Bhutan for 22 months between 2013 and 2014. Recorded seismicity, earthquake moment tensors and local earthquake tomography reveal along-strike variations in structure and crustal deformation regime. A thickened crust imaged in western Bhutan suggests lateral differences in stresses on the Main Himalayan Thrust (MHT), potentially affecting the interseismic coupling and deformation regime. Sikkim, western Bhutan and its foreland are characterized by strike-slip faulting in the Indian basement. Strain is particularly localized along a NW–SE striking mid-crustal fault zone reaching from Chungthang in northeast Sikkim to Dhubri at the northwestern edge of the Shillong Plateau in the foreland. The dextral Dhubri–Chungthang fault zone (DCF) causes segmentation of the Indian basement and the MHT between eastern Nepal and western Bhutan and connects the deformation front of the Himalaya with the Shillong Plateau by forming the western boundary of the Shillong block. The Kopili fault, the proposed eastern boundary of this block, appears to be a diffuse zone of mid-crustal seismicity in the foreland. In eastern Bhutan we image a seismogenic, flat portion of the MHT, which might be either related to a partially creeping segment or to increased background seismicity originating from the 2009 MW6.1 earthquake. In western-central Bhutan clusters of micro-earthquakes at the front of the High-Himalayas indicate the presence of a mid-crustal ramp and stress buildup on a fully coupled MHT. The area bounded by the DCF in the west and the seismogenic MHT in the east has the potential for M7–8 earthquakes in Bhutan. 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<span class="author-name" >Singer J </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" mtid="10001690"><a href="/gui2/?type=authors&mode=browse&sel=10001690" target="_blank">Hetényi G (<span class="authorship-author-name">Hetényi György</span> <span class="authorAux-mtmt"> geofizikus</span>) </a> </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Grujic D </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Clinton J </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Giardini D </span> ;&nbsp;&nbsp;&nbsp; <span class="author-name" >Kissling E </span> </div> </div> <div class="title"><a href="/gui2/?mode=browse&params=publication;3273926" target="_blank">Seismotectonics of Bhutan: Evidence for segmentation of the Eastern Himalayas and link to foreland deformation</a></div> <div> <span class="journal-title">EARTH AND PLANETARY SCIENCE LETTERS</span> <span class="journal-issn">(<a target="_blank" href="https://portal.issn.org/resource/ISSN/0012-821X">0012-821X</a> <a target="_blank" href="https://portal.issn.org/resource/ISSN/1385-013X">1385-013X</a>)</span>: <span class="journal-volume">471</span> <span class="page"> pp 54-64 </span> <span class="year">(2017)</span> </div> <div class="pub-footer"> <span class="language" xmlns="http://www.w3.org/1999/html">Nyelv: Angol | </span> <span class="identifiers"> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="10.1016/j.epsl.2017.04.038" target="_blank" href="https://doi.org/10.1016/j.epsl.2017.04.038"> DOI </a> </span> <span class="id identifier oa_CLOSED" title=" Zárt "> <a style="color:black" title="74511" target="_blank" href="http://real.mtak.hu/74511"> REAL </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="000403625300006" target="_blank" href="https://www.webofscience.com/wos/woscc/full-record/000403625300006"> WoS </a> </span> <span class="id identifier oa_none" title="none"> <a style="color:blue" title="85019601872" target="_blank" href="http://www.scopus.com/record/display.url?origin=inward&eid=2-s2.0-85019601872"> Scopus </a> </span> </span> <OnlyViewableByAuthor><div class="ratings"> <div class="journal-subject">Folyóirat szakterülete: Scopus - Earth and Planetary Sciences (miscellaneous)&nbsp;&nbsp;&nbsp;SJR indikátor:&nbsp;D1</div> <div class="journal-subject">Folyóirat szakterülete: Scopus - Geochemistry and Petrology&nbsp;&nbsp;&nbsp;SJR indikátor:&nbsp;D1</div> <div class="journal-subject">Folyóirat szakterülete: Scopus - Geophysics&nbsp;&nbsp;&nbsp;SJR indikátor:&nbsp;D1</div> <div class="journal-subject">Folyóirat szakterülete: Scopus - Space and Planetary Science&nbsp;&nbsp;&nbsp;SJR indikátor:&nbsp;Q1</div> <div class="journal-subject">X. 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We thank S. Schmid, J.-P. Burg, C. Cauzzi, and T. Tormann for helpful d...</pre> </div></div>