Underthrusting and Pure Shear Mechanisms Dominate the Crustal Deformation Beneath the Core of the Eastern Himalayan Syntaxis as Inferred From High‐Resolution Receiver Function Imaging

How the crust in the core of the Eastern Himalayan Syntaxis (EHS) deforms responding to the India‐Asia collision remains ambiguous. Here we present the first high‐resolution receiver functions image of crustal structure along a new NW‐SE trending dense nodal array crossing the core of the EHS. Two s...

Celý popis

Uložené v:

Podrobná bibliografia
Vydané v:	Geophysical research letters Ročník 49; číslo 24
Hlavní autori:	Xu, Qiang, Ding, Lin, Pei, Shunping, Yuan, Xiaohui, Zhao, Junmeng, Liu, Hongbing, Liu, Hanlin, Li, Lei, Zuo, Hong
Médium:	Journal Article
Jazyk:	English
Vydavateľské údaje:	Washington John Wiley & Sons, Inc 28.12.2022
Predmet:	Arrays Collision dynamics Crustal deformation Crustal shortening Crustal structure Deformation Dipping Discontinuity Eastern Himalayan Syntaxis Exhumation Fluids Geological processes intra‐crustal interface Moho Moho offset pure shear receiver functions Resolution Shear zone Subduction Subduction (geology) Tectonics underthrusting of the Indian lower crust Velocity
ISSN:	0094-8276, 1944-8007
On-line prístup:	Získať plný text
Tagy:	Pridať tag Žiadne tagy, Buďte prvý, kto otaguje tento záznam!

Abstract	How the crust in the core of the Eastern Himalayan Syntaxis (EHS) deforms responding to the India‐Asia collision remains ambiguous. Here we present the first high‐resolution receiver functions image of crustal structure along a new NW‐SE trending dense nodal array crossing the core of the EHS. Two sets of low velocity zones (LVZs) are clearly observed: one with a flat style beneath the western Lhasa terrane and Higher Himalaya at 18–20 km depth and the other with two west‐dipping shapes below the western Yarlung‐Zangbo suture within 10–30 km depth. These LVZs caused by partial melting and aqueous fluids are disconnected, impeding the formation of crustal flow. A discontinuous east‐dipping intra‐crustal discontinuity and a sharp Moho offset of 7 km under the Aniqiao‐Motuo shear zone are identified, suggesting that the underthrusting of the Indian lower crust and pure shear mechanisms jointly dominate crustal deformation in the core of the EHS. Plain Language Summary The tectonic evolution of the Eastern Himalayan Syntaxis (EHS) involves complex tectonic activities such as collision, subduction, and rapid exhumation, making the EHS an ideal site for studying the dynamics of continental collision processes. Strong crustal shortening occurs during the formation of the EHS, but the specific mechanism that accommodates this crustal deformation remains unclear. In this study, we construct a novel seismic image of crustal structure with unprecedented details along a recently deployed dense nodal array that traverses the core of the EHS. We observe two unconnected groups of low velocity zones, which call into question the validity of the crustal flow model in the core of the EHS. Our observations indicate that the underthrusting of the Indian lower crust and pure shear mechanisms, rather than a model of vertically coherent deformation, account for the present crustal deformation in the core of the EHS. Key Points First high‐resolution image of crustal structure in the core of the Eastern Himalayan Syntaxis is constructed from P receiver functions Two disconnected groups of low velocity zones are observed in upper to middle crust, which prevents the development of crust flow An intra‐crustal interface and a Moho offset we find suggest that underthrusting and pure shear mechanisms dominate crustal deformation
AbstractList	How the crust in the core of the Eastern Himalayan Syntaxis (EHS) deforms responding to the India‐Asia collision remains ambiguous. Here we present the first high‐resolution receiver functions image of crustal structure along a new NW‐SE trending dense nodal array crossing the core of the EHS. Two sets of low velocity zones (LVZs) are clearly observed: one with a flat style beneath the western Lhasa terrane and Higher Himalaya at 18–20 km depth and the other with two west‐dipping shapes below the western Yarlung‐Zangbo suture within 10–30 km depth. These LVZs caused by partial melting and aqueous fluids are disconnected, impeding the formation of crustal flow. A discontinuous east‐dipping intra‐crustal discontinuity and a sharp Moho offset of 7 km under the Aniqiao‐Motuo shear zone are identified, suggesting that the underthrusting of the Indian lower crust and pure shear mechanisms jointly dominate crustal deformation in the core of the EHS. How the crust in the core of the Eastern Himalayan Syntaxis (EHS) deforms responding to the India‐Asia collision remains ambiguous. Here we present the first high‐resolution receiver functions image of crustal structure along a new NW‐SE trending dense nodal array crossing the core of the EHS. Two sets of low velocity zones (LVZs) are clearly observed: one with a flat style beneath the western Lhasa terrane and Higher Himalaya at 18–20 km depth and the other with two west‐dipping shapes below the western Yarlung‐Zangbo suture within 10–30 km depth. These LVZs caused by partial melting and aqueous fluids are disconnected, impeding the formation of crustal flow. A discontinuous east‐dipping intra‐crustal discontinuity and a sharp Moho offset of 7 km under the Aniqiao‐Motuo shear zone are identified, suggesting that the underthrusting of the Indian lower crust and pure shear mechanisms jointly dominate crustal deformation in the core of the EHS. The tectonic evolution of the Eastern Himalayan Syntaxis (EHS) involves complex tectonic activities such as collision, subduction, and rapid exhumation, making the EHS an ideal site for studying the dynamics of continental collision processes. Strong crustal shortening occurs during the formation of the EHS, but the specific mechanism that accommodates this crustal deformation remains unclear. In this study, we construct a novel seismic image of crustal structure with unprecedented details along a recently deployed dense nodal array that traverses the core of the EHS. We observe two unconnected groups of low velocity zones, which call into question the validity of the crustal flow model in the core of the EHS. Our observations indicate that the underthrusting of the Indian lower crust and pure shear mechanisms, rather than a model of vertically coherent deformation, account for the present crustal deformation in the core of the EHS. First high‐resolution image of crustal structure in the core of the Eastern Himalayan Syntaxis is constructed from P receiver functions Two disconnected groups of low velocity zones are observed in upper to middle crust, which prevents the development of crust flow An intra‐crustal interface and a Moho offset we find suggest that underthrusting and pure shear mechanisms dominate crustal deformation How the crust in the core of the Eastern Himalayan Syntaxis (EHS) deforms responding to the India‐Asia collision remains ambiguous. Here we present the first high‐resolution receiver functions image of crustal structure along a new NW‐SE trending dense nodal array crossing the core of the EHS. Two sets of low velocity zones (LVZs) are clearly observed: one with a flat style beneath the western Lhasa terrane and Higher Himalaya at 18–20 km depth and the other with two west‐dipping shapes below the western Yarlung‐Zangbo suture within 10–30 km depth. These LVZs caused by partial melting and aqueous fluids are disconnected, impeding the formation of crustal flow. A discontinuous east‐dipping intra‐crustal discontinuity and a sharp Moho offset of 7 km under the Aniqiao‐Motuo shear zone are identified, suggesting that the underthrusting of the Indian lower crust and pure shear mechanisms jointly dominate crustal deformation in the core of the EHS. Plain Language Summary The tectonic evolution of the Eastern Himalayan Syntaxis (EHS) involves complex tectonic activities such as collision, subduction, and rapid exhumation, making the EHS an ideal site for studying the dynamics of continental collision processes. Strong crustal shortening occurs during the formation of the EHS, but the specific mechanism that accommodates this crustal deformation remains unclear. In this study, we construct a novel seismic image of crustal structure with unprecedented details along a recently deployed dense nodal array that traverses the core of the EHS. We observe two unconnected groups of low velocity zones, which call into question the validity of the crustal flow model in the core of the EHS. Our observations indicate that the underthrusting of the Indian lower crust and pure shear mechanisms, rather than a model of vertically coherent deformation, account for the present crustal deformation in the core of the EHS. Key Points First high‐resolution image of crustal structure in the core of the Eastern Himalayan Syntaxis is constructed from P receiver functions Two disconnected groups of low velocity zones are observed in upper to middle crust, which prevents the development of crust flow An intra‐crustal interface and a Moho offset we find suggest that underthrusting and pure shear mechanisms dominate crustal deformation
Author	Liu, Hongbing Xu, Qiang Liu, Hanlin Yuan, Xiaohui Ding, Lin Zhao, Junmeng Li, Lei Pei, Shunping Zuo, Hong
Author_xml	– sequence: 1 givenname: Qiang orcidid: 0000-0001-6506-2745 surname: Xu fullname: Xu, Qiang email: xuqiang@itpcas.ac.cn organization: Chinese Academy of Sciences – sequence: 2 givenname: Lin orcidid: 0000-0002-0265-9613 surname: Ding fullname: Ding, Lin organization: Chinese Academy of Sciences – sequence: 3 givenname: Shunping orcidid: 0000-0002-4924-1089 surname: Pei fullname: Pei, Shunping email: peisp@itpcas.ac.cn organization: Chinese Academy of Sciences – sequence: 4 givenname: Xiaohui orcidid: 0000-0002-2891-1354 surname: Yuan fullname: Yuan, Xiaohui organization: Deutsches GeoForschungsZentrum GFZ – sequence: 5 givenname: Junmeng orcidid: 0000-0003-2713-153X surname: Zhao fullname: Zhao, Junmeng organization: Chinese Academy of Sciences – sequence: 6 givenname: Hongbing surname: Liu fullname: Liu, Hongbing organization: Chinese Academy of Sciences – sequence: 7 givenname: Hanlin orcidid: 0000-0002-5326-2384 surname: Liu fullname: Liu, Hanlin organization: Chinese Academy of Sciences – sequence: 8 givenname: Lei surname: Li fullname: Li, Lei organization: Chinese Academy of Sciences – sequence: 9 givenname: Hong surname: Zuo fullname: Zuo, Hong organization: Chinese Academy of Sciences
BookMark	eNqFkc1uEzEQxy1UJNLCjQewxJWAP9br9RHSJo0UBErpeTXxzmZd7drF9gK58Qi8Dq_Dk7BNOCAOcJrRzG_-83VOznzwSMhzzl5xJsxrwYRYbTjjpdGPyIybophXjOkzMmPMTL7Q5RNyntIdY0wyyWfkx61vMOYujik7v6fgG_phjEhvOoRI36HtwLs0JHoZBuchI80d0sUDDz29xDbEAbILnr5Fj5C7Uz5MEqE9-leQMkZPr90APRzA05uDz_DVJQqJrn2LMWJDlzEME7Pvfn77vsUU-vGoukWL7jNGuhy9PUbWA-ynUZ-Sxy30CZ_9thfkdnn1cXE937xfrRdvNnOQpTZzLLmtqrLRWILYodQt4xYBeKUaMKUqhNVKygZ3dleoosKinULQVIpLXSkrL8iLk-59DJ9GTLm-C2P0U8taaFWVxqiCT9TLE2VjSCliW9_Had94qDmrH55T__mcCRd_4dbl4xlzBNf_p-iL6_Hwzwb1arsplaiM_AUjW6Zv
CitedBy_id	crossref_primary_10_1007_s11430_023_1158_5 crossref_primary_10_1007_s10712_025_09900_z crossref_primary_10_1016_j_epsl_2025_119302 crossref_primary_10_1029_2024JB030249 crossref_primary_10_1038_s41598_025_99763_6 crossref_primary_10_1016_j_pepi_2025_107363
Cites_doi	10.1214/ss/1177013815 10.1016/j.epsl.2016.07.043 10.1038/414738a 10.1002/2016jb013825 10.1016/j.tecto.2018.06.006 10.1016/j.epsl.2011.05.004 10.1029/98EO00426 10.1002/2017jb014490 10.1016/j.epsl.2013.09.038 10.1029/2022GL098331 10.1029/96jb03857 10.1016/B978-0-12-374739-6.00094-4 10.1016/S0012-821x(01)00463-0 10.1029/2021JB022574 10.1002/jgrb.50162 10.1126/science.274.5293.1684 10.1029/2021JB022435 10.1016/j.earscirev.2016.07.010 10.1016/j.epsl.2020.116700 10.1002/2014gl061026 10.1029/97jb02379 10.1016/j.jseaes.2018.07.027 10.1126/science.1259041 10.1016/j.gr.2011.06.010 10.1016/j.gr.2014.01.006 10.6038/cjg20170107 10.1016/j.gr.2012.05.011 10.1002/2015gl064568 10.1029/2019JB019215 10.1130/1052-5173(2001)011<0004:ehgatg>2.0.co;2 10.1029/2019JB018257 10.1029/2019tc005483 10.1007/s11430-016-5244-x 10.1016/j.epsl.2016.07.051 10.1146/annurev.earth.28.1.211 10.1016/j.gr.2021.05.011
ContentType	Journal Article
Copyright	2022. The Authors. 2022. This article is published under http://creativecommons.org/licenses/by-nc-nd/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.
Copyright_xml	– notice: 2022. The Authors. – notice: 2022. This article is published under http://creativecommons.org/licenses/by-nc-nd/4.0/ (the “License”). Notwithstanding the ProQuest Terms and Conditions, you may use this content in accordance with the terms of the License.
DBID	24P AAYXX CITATION 7TG 7TN 8FD F1W FR3 H8D H96 KL. KR7 L.G L7M
DOI	10.1029/2022GL101697
DatabaseName	Wiley Online Library Open Access (Activated by CARLI) CrossRef Meteorological & Geoastrophysical Abstracts Oceanic Abstracts Technology Research Database ASFA: Aquatic Sciences and Fisheries Abstracts Engineering Research Database Aerospace Database Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources Meteorological & Geoastrophysical Abstracts - Academic Civil Engineering Abstracts Aquatic Science & Fisheries Abstracts (ASFA) Professional Advanced Technologies Database with Aerospace
DatabaseTitle	CrossRef Aerospace Database Civil Engineering Abstracts Aquatic Science & Fisheries Abstracts (ASFA) Professional Meteorological & Geoastrophysical Abstracts Aquatic Science & Fisheries Abstracts (ASFA) 2: Ocean Technology, Policy & Non-Living Resources Oceanic Abstracts Technology Research Database ASFA: Aquatic Sciences and Fisheries Abstracts Engineering Research Database Advanced Technologies Database with Aerospace Meteorological & Geoastrophysical Abstracts - Academic
DatabaseTitleList	Aerospace Database CrossRef
Database_xml	– sequence: 1 dbid: 24P name: Wiley Online Library Open Access (Activated by CARLI) url: https://authorservices.wiley.com/open-science/open-access/browse-journals.html sourceTypes: Publisher
DeliveryMethod	fulltext_linktorsrc
Discipline	Geology Physics
EISSN	1944-8007
EndPage	n/a
ExternalDocumentID	10_1029_2022GL101697 GRL65289
Genre	article
GrantInformation_xml	– fundername: National Natural Science Foundation of China funderid: 42074113 – fundername: K.C. Wong Education Foundation funderid: GJTD‐2019‐04 – fundername: The Second Tibetan Plateau Scientific Expedition and Research Program funderid: 2019QZKK0708
GroupedDBID	-DZ -~X 05W 0R~ 1OB 1OC 24P 33P 50Y 5GY 5VS 702 8-1 8R4 8R5 A00 AAESR AAHHS AAIHA AAXRX AAZKR ABCUV ABPPZ ACAHQ ACCFJ ACCZN ACGFO ACGFS ACGOD ACIWK ACNCT ACPOU ACXBN ACXQS ADBBV ADEOM ADKYN ADMGS ADOZA ADXAS ADZMN ADZOD AEEZP AENEX AEQDE AEUQT AFBPY AFGKR AFPWT AFRAH AIURR AIWBW AJBDE ALMA_UNASSIGNED_HOLDINGS ALUQN ALXUD AMYDB AVUZU AZFZN AZVAB BENPR BFHJK BMXJE BRXPI CS3 DCZOG DPXWK DRFUL DRSTM DU5 EBS F5P G-S GODZA HZ~ LATKE LEEKS LITHE LOXES LUTES LYRES MEWTI MSFUL MSSTM MXFUL MXSTM MY~ O9- OK1 P-X P2P P2W PYCSY Q2X R.K RNS ROL SUPJJ TN5 TWZ UPT WBKPD WH7 WIH WIN WXSBR WYJ XSW ZZTAW ~02 ~OA ~~A AAFWJ AAMMB AAYXX ACTHY AEFGJ AFPKN AGXDD AIDQK AIDYY CITATION 7TG 7TN 8FD F1W FR3 H8D H96 KL. KR7 L.G L7M
ID	FETCH-LOGICAL-a3679-e61c886d7e6a2be37f01ceaa185da96542c7533debcb4548e4f42cad8513785c3
IEDL.DBID	DRFUL
ISICitedReferencesCount	8
ISICitedReferencesURI	http://www.webofscience.com/api/gateway?GWVersion=2&SrcApp=Summon&SrcAuth=ProQuest&DestLinkType=CitingArticles&DestApp=WOS_CPL&KeyUT=000924504900001&url=https%3A%2F%2Fcvtisr.summon.serialssolutions.com%2F%23%21%2Fsearch%3Fho%3Df%26include.ft.matches%3Dt%26l%3Dnull%26q%3D
ISSN	0094-8276
IngestDate	Fri Jul 25 10:47:17 EDT 2025 Tue Nov 18 21:28:26 EST 2025 Sat Nov 29 02:58:14 EST 2025 Wed Jan 22 16:19:58 EST 2025
IsDoiOpenAccess	true
IsOpenAccess	true
IsPeerReviewed	true
IsScholarly	true
Issue	24
Language	English
License	Attribution-NonCommercial-NoDerivs
LinkModel	DirectLink
MergedId	FETCHMERGED-LOGICAL-a3679-e61c886d7e6a2be37f01ceaa185da96542c7533debcb4548e4f42cad8513785c3
Notes	ObjectType-Article-1 SourceType-Scholarly Journals-1 ObjectType-Feature-2 content type line 14
ORCID	0000-0002-0265-9613 0000-0002-5326-2384 0000-0001-6506-2745 0000-0002-2891-1354 0000-0003-2713-153X 0000-0002-4924-1089
OpenAccessLink	https://onlinelibrary.wiley.com/doi/abs/10.1029%2F2022GL101697
PQID	2758699541
PQPubID	54723
PageCount	8
ParticipantIDs	proquest_journals_2758699541 crossref_primary_10_1029_2022GL101697 crossref_citationtrail_10_1029_2022GL101697 wiley_primary_10_1029_2022GL101697_GRL65289
PublicationCentury	2000
PublicationDate	28 December 2022
PublicationDateYYYYMMDD	2022-12-28
PublicationDate_xml	– month: 12 year: 2022 text: 28 December 2022 day: 28
PublicationDecade	2020
PublicationPlace	Washington
PublicationPlace_xml	– name: Washington
PublicationTitle	Geophysical research letters
PublicationYear	2022
Publisher	John Wiley & Sons, Inc
Publisher_xml	– name: John Wiley & Sons, Inc
References	2017; 60 2000; 28 2018; 744 2021; 126 2019; 38 2019; 169 2013; 383 2020; 125 2014; 41 2016; 160 2013; 5 2022; 49 1997; 102 1986; 1 2011; 307 2015; 27 2013b; 23 2001; 192 2021; 554 2013a; 118 2015; 42 2016; 454 2016; 452 1996; 274 2017; 122 2001; 11 2012; 21 2022; 104 2022; 127 2014; 346 2001; 414 1998; 79 e_1_2_8_28_1 e_1_2_8_29_1 e_1_2_8_24_1 e_1_2_8_25_1 e_1_2_8_26_1 e_1_2_8_27_1 e_1_2_8_3_1 e_1_2_8_2_1 e_1_2_8_5_1 e_1_2_8_4_1 e_1_2_8_7_1 e_1_2_8_6_1 e_1_2_8_9_1 e_1_2_8_8_1 e_1_2_8_20_1 e_1_2_8_21_1 e_1_2_8_22_1 e_1_2_8_23_1 e_1_2_8_17_1 e_1_2_8_18_1 e_1_2_8_19_1 e_1_2_8_13_1 e_1_2_8_36_1 e_1_2_8_14_1 e_1_2_8_35_1 e_1_2_8_15_1 e_1_2_8_16_1 e_1_2_8_37_1 e_1_2_8_32_1 e_1_2_8_10_1 e_1_2_8_31_1 e_1_2_8_11_1 e_1_2_8_34_1 e_1_2_8_12_1 e_1_2_8_33_1 e_1_2_8_30_1
References_xml	– volume: 42 start-page: 5813 issue: 14 year: 2015 end-page: 5819 article-title: Vertical coherence of deformation in lithosphere in the eastern Himalayan syntaxis using GPS, Quaternary fault slip rates, and shear wave splitting data publication-title: Geophysical Research Letters – volume: 79 issue: 47 year: 1998 article-title: New, improved version of generic mapping tools released publication-title: EOS, Transactions American Geophysical Union – volume: 60 start-page: 70 issue: 1 year: 2017 end-page: 85 article-title: Crustal structure under the eastern Himalayan syntaxis seismic array and its geodynamic implications derived from receiver functions publication-title: Chinese Journal of Geophysics‐Chinese Edition – volume: 127 issue: 6 year: 2022 article-title: Seismic imaging of crust beneath the western Tibet‐Pamir and western Himalaya using ambient noise and earthquake data publication-title: Journal of Geophysical Research‐Solid Earth – volume: 38 start-page: 3614 issue: 10 year: 2019 end-page: 3628 article-title: Deep structure of the eastern Himalayan collision zone: Evidence for underthrusting and delamination in the postcollisional stage publication-title: Tectonics – volume: 28 start-page: 211 issue: 1 year: 2000 end-page: 280 article-title: Geologic evolution of the Himalayan‐Tibetan orogen publication-title: Annual Review of Earth and Planetary Sciences – volume: 122 start-page: 8257 issue: 10 year: 2017 end-page: 8269 article-title: Detailed configuration of the underthrusting Indian lithosphere beneath Western Tibet revealed by receiver function images publication-title: Journal of Geophysical Research‐Solid Earth – volume: 102 start-page: 8313 issue: B4 year: 1997 end-page: 8327 article-title: Mantle discontinuity structure from midpoint stacks of converted P–S waves across the Yellowstone hotspot track publication-title: Journal of Geophysical Research – volume: 414 start-page: 738 issue: 6865 year: 2001 end-page: 742 article-title: Himalayan tectonics explained by extrusion of a low‐viscosity crustal channel coupled to focused surface denudation publication-title: Nature – volume: 744 start-page: 1 year: 2018 end-page: 9 article-title: Crustal velocity structure around the eastern Himalayan Syntaxis: Implications for the nucleation mechanism of the 2017 M‐s 6.9 Mainling earthquake and regional tectonics publication-title: Tectonophysics – volume: 41 start-page: 5861 issue: 16 year: 2014 end-page: 5867 article-title: Extreme localized exhumation at syntaxes initiated by subduction geometry publication-title: Geophysical Research Letters – volume: 192 start-page: 423 issue: 3 year: 2001 end-page: 438 article-title: Cenozoic structural and metamorphic evolution of the eastern Himalayan syntaxis (Namche Barwa) publication-title: Earth and Planetary Science Letters – volume: 554 year: 2021 article-title: Crustal‐scale wedge tectonics at the narrow boundary between the Tibetan Plateau and Ordos block publication-title: Earth and Planetary Science Letters – volume: 49 issue: 8 year: 2022 article-title: Tomographic imaging of the plate geometry beneath the Arunachal Himalaya and Burmese subduction zones publication-title: Geophysical Research Letters – volume: 307 start-page: 323 issue: 3–4 year: 2011 end-page: 333 article-title: Denudation of the Namche Barwa antiform, eastern Himalaya publication-title: Earth and Planetary Science Letters – volume: 1 start-page: 54 year: 1986 end-page: 75 article-title: Bootstrap methods for standard errors, confidence intervals, and other measures of statistical accuracy publication-title: Statistical Science – volume: 125 issue: 7 year: 2020 article-title: High‐resolution 3‐D shear wave velocity model of the Tibetan plateau: Implications for crustal deformation and porphyry Cu deposit formation publication-title: Journal of Geophysical Research‐Solid Earth – volume: 346 start-page: 978 issue: 6212 year: 2014 end-page: 981 article-title: Tectonic control of Yarlung Tsangpo gorge revealed by a buried canyon in southern Tibet publication-title: Science – volume: 23 start-page: 715 issue: 2 year: 2013b end-page: 725 article-title: Rapid Eocene erosion, sedimentation and burial in the eastern Himalayan syntaxis and its geodynamic significance publication-title: Gondwana Research – volume: 169 start-page: 130 year: 2019 end-page: 138 article-title: Source parameters and seismogenic structure of the 2017 Mw 6.5 mainling earthquake in the eastern Himalayan syntaxis (Tibet, China) publication-title: Journal of Asian Earth Sciences – volume: 5 start-page: 318 year: 2013 end-page: 349 article-title: Tectonic aneursms and mountain building publication-title: Treatise on Geomorphology – volume: 274 start-page: 1684 issue: 5293 year: 1996 end-page: 1688 article-title: Partially molten middle crust beneath southern Tibet: Synthesis of project INDEPTH results publication-title: Science – volume: 104 start-page: 4 year: 2022 end-page: 22 article-title: On the origin of high‐pressure mafic granulite in the Eastern Himalayan Syntaxis: Implications for the tectonic evolution of the Himalayan orogen publication-title: Gondwana Research – volume: 60 start-page: 635 issue: 4 year: 2017 end-page: 651 article-title: Processes of initial collision and suturing between India and Asia publication-title: Science China Earth Sciences – volume: 126 issue: 9 year: 2021 article-title: Middle crustal partial melting triggered since the mid‐miocene in southern Tibet: Insights from magnetotelluric data publication-title: Journal of Geophysical Research‐Solid Earth – volume: 160 start-page: 350 year: 2016 end-page: 385 article-title: Pliod publication-title: Earth‐Science Reviews – volume: 125 issue: 5 year: 2020 article-title: Direct surface wave radial anisotropy tomography the crust of the eastern himalayan syntaxis publication-title: Journal of Geophysical Research‐Solid Earth – volume: 102 start-page: 27491 issue: B12 year: 1997 end-page: 27500 article-title: Lithospheric and upper mantle structure of southern Tibet from a seismological passive source experiment publication-title: Journal of Geophysical Research – volume: 383 start-page: 113 year: 2013 end-page: 122 article-title: Crustal flow pattern beneath the Tibetan Plateau constrained by regional Lg‐wave Q tomography publication-title: Earth and Planetary Science Letters – volume: 454 start-page: 78 year: 2016 end-page: 85 article-title: Extensional extrusion: Insights into South‐eastward expansion of Tibetan Plateau from magnetotelluric array data publication-title: Earth and Planetary Science Letters – volume: 21 start-page: 19 issue: 1 year: 2012 end-page: 36 article-title: Kinematics and dynamics of the Namche Barwa syntaxis, eastern Himalaya: Constraints from deformation, fabrics and geochronology publication-title: Gondwana Research – volume: 118 start-page: 2323 issue: 5 year: 2013a end-page: 2332 article-title: Imaging lithospheric structure of the eastern Himalayan syntaxis: New insights from receiver function analysis publication-title: Journal of Geophysical Research‐Solid Earth – volume: 452 start-page: 171 year: 2016 end-page: 177 article-title: West‐East transition from underplating to steep subduction in the India‐Tibet collision zone revealed by receiver‐function profiles publication-title: Earth and Planetary Science Letters – volume: 122 start-page: 5082 issue: 7 year: 2017 end-page: 5100 article-title: Crustal structure beneath Namche Barwa, eastern Himalayan syntaxis: New insights from three‐dimensional magnetotelluric imaging publication-title: Journal of Geophysical Research‐Solid Earth – volume: 27 start-page: 1487 issue: 4 year: 2015 end-page: 1493 article-title: Mapping crustal structure beneath southern Tibet: Seismic evidence for continental crustal underthrusting publication-title: Gondwana Research – volume: 11 start-page: 4 issue: 1 year: 2001 end-page: 9 article-title: Erosion, Himalayan geodynamics, and the geomorphology of metamorphism publication-title: Geological Society of America Today – ident: e_1_2_8_11_1 doi: 10.1214/ss/1177013815 – ident: e_1_2_8_8_1 doi: 10.1016/j.epsl.2016.07.043 – ident: e_1_2_8_2_1 doi: 10.1038/414738a – ident: e_1_2_8_19_1 doi: 10.1002/2016jb013825 – ident: e_1_2_8_13_1 doi: 10.1016/j.tecto.2018.06.006 – ident: e_1_2_8_12_1 doi: 10.1016/j.epsl.2011.05.004 – ident: e_1_2_8_26_1 doi: 10.1029/98EO00426 – ident: e_1_2_8_30_1 doi: 10.1002/2017jb014490 – ident: e_1_2_8_37_1 doi: 10.1016/j.epsl.2013.09.038 – ident: e_1_2_8_9_1 doi: 10.1029/2022GL098331 – ident: e_1_2_8_10_1 doi: 10.1029/96jb03857 – ident: e_1_2_8_16_1 doi: 10.1016/B978-0-12-374739-6.00094-4 – ident: e_1_2_8_7_1 doi: 10.1016/S0012-821x(01)00463-0 – ident: e_1_2_8_17_1 doi: 10.1029/2021JB022574 – ident: e_1_2_8_28_1 doi: 10.1002/jgrb.50162 – ident: e_1_2_8_20_1 doi: 10.1126/science.274.5293.1684 – ident: e_1_2_8_27_1 doi: 10.1029/2021JB022435 – ident: e_1_2_8_4_1 doi: 10.1016/j.earscirev.2016.07.010 – ident: e_1_2_8_23_1 doi: 10.1016/j.epsl.2020.116700 – ident: e_1_2_8_3_1 doi: 10.1002/2014gl061026 – ident: e_1_2_8_34_1 doi: 10.1029/97jb02379 – ident: e_1_2_8_18_1 doi: 10.1016/j.jseaes.2018.07.027 – ident: e_1_2_8_25_1 doi: 10.1126/science.1259041 – ident: e_1_2_8_32_1 doi: 10.1016/j.gr.2011.06.010 – ident: e_1_2_8_29_1 doi: 10.1016/j.gr.2014.01.006 – ident: e_1_2_8_21_1 doi: 10.6038/cjg20170107 – ident: e_1_2_8_31_1 doi: 10.1016/j.gr.2012.05.011 – ident: e_1_2_8_5_1 doi: 10.1002/2015gl064568 – ident: e_1_2_8_15_1 doi: 10.1029/2019JB019215 – ident: e_1_2_8_35_1 doi: 10.1130/1052-5173(2001)011<0004:ehgatg>2.0.co;2 – ident: e_1_2_8_14_1 doi: 10.1029/2019JB018257 – ident: e_1_2_8_24_1 doi: 10.1029/2019tc005483 – ident: e_1_2_8_6_1 doi: 10.1007/s11430-016-5244-x – ident: e_1_2_8_22_1 doi: 10.1016/j.epsl.2016.07.051 – ident: e_1_2_8_33_1 doi: 10.1146/annurev.earth.28.1.211 – ident: e_1_2_8_36_1 doi: 10.1016/j.gr.2021.05.011
SSID	ssj0003031
Score	2.4520514
Snippet	How the crust in the core of the Eastern Himalayan Syntaxis (EHS) deforms responding to the India‐Asia collision remains ambiguous. Here we present the first...
SourceID	proquest crossref wiley
SourceType	Aggregation Database Enrichment Source Index Database Publisher
SubjectTerms	Arrays Collision dynamics Crustal deformation Crustal shortening Crustal structure Deformation Dipping Discontinuity Eastern Himalayan Syntaxis Exhumation Fluids Geological processes intra‐crustal interface Moho Moho offset pure shear receiver functions Resolution Shear zone Subduction Subduction (geology) Tectonics underthrusting of the Indian lower crust Velocity
Title	Underthrusting and Pure Shear Mechanisms Dominate the Crustal Deformation Beneath the Core of the Eastern Himalayan Syntaxis as Inferred From High‐Resolution Receiver Function Imaging
URI	https://onlinelibrary.wiley.com/doi/abs/10.1029%2F2022GL101697 https://www.proquest.com/docview/2758699541
Volume	49
WOSCitedRecordID	wos000924504900001&url=https%3A%2F%2Fcvtisr.summon.serialssolutions.com%2F%23%21%2Fsearch%3Fho%3Df%26include.ft.matches%3Dt%26l%3Dnull%26q%3D
hasFullText	1
inHoldings	1
isFullTextHit
isPrint
journalDatabaseRights	– providerCode: PRVWIB databaseName: Wiley Online Library customDbUrl: eissn: 1944-8007 dateEnd: 20231214 omitProxy: false ssIdentifier: ssj0003031 issn: 0094-8276 databaseCode: WIN dateStart: 19970101 isFulltext: true titleUrlDefault: https://onlinelibrary.wiley.com providerName: Wiley-Blackwell – providerCode: PRVWIB databaseName: Wiley Online Library - Journals customDbUrl: eissn: 1944-8007 dateEnd: 99991231 omitProxy: false ssIdentifier: ssj0003031 issn: 0094-8276 databaseCode: DRFUL dateStart: 19970101 isFulltext: true titleUrlDefault: https://onlinelibrary.wiley.com providerName: Wiley-Blackwell
link	http://cvtisr.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwpV3NbtQwELZoCxIX_hGFUvkAJxSxSRwnOUK32a60rFaFQm_RxJ6IlboJSlLE3ngEXofX4UmYcdJlOYCEuCXOxLbkGc839vwI8Uz7aKORUl5hC_BUVEQeqSHtlUrjyJoUSxfl-n4Wz-fJ-Xm6GA7cOBamzw-xOXBjyXD7NQs4FO2QbIBzZJLVHkxmbHym8Y7Y47gqMr72xqfZ2WyzF9MG3dfMSxXNIdaD6zv18HL7_9-V0i-kuY1XncLJbv_vVO-IWwPUlK963rgrrmF1T9yYuFK-a3pyzp-mvS--u-JH3UcOvyBNJqGycnHZoHTlruUb5OjgZbtq5bhmz5kOJcFGecT0NMAYNxGQ8jVtnYQp--81dVGX7vkYXEIGebJcwQWsoZJv11UHX5athFZOOeqwQSuzpl5Jdj358fUbXyz0YiEJ2yL7j8iMtLBrma5cdaUH4iw7fnd04g0lHTwIdZx6qH2TJNrGqCEoMIzLkW8QgFCDhZSLZxmyn0KLhSkUGVOoSmoCS7gwjJPIhA_FblVX-EhIGzI32UIliiAd6sQPC7AApQ9JYky4L15crWluhnznXHbjInf37kGaby_Lvni-of7U5_n4A93BFXvkg7S3eUBGl-bEej4N6hjhr33kk9OZjsjSffxP1E_ETW5nX5ogORC7XXOJT8V187lbts2h2AnU4nDgf3r7MJ3_BNs3CAc
linkProvider	Wiley-Blackwell
linkToHtml	http://cvtisr.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwpV3NbtQwELaggODCbxGFAj7ACUVsEsdJjtB2f0S6WkFBvUUTeyJW6iYoSRF74xF4HV6HJ2HGSZflABLiFjnjJFJmPN_YM_MJ8Uz7aKORUl5hC_BUVEQeuSHtlUrjyJoUS1fl-iGL5_Pk9DRdDDynXAvT94fYbLixZbj1mg2cN6SHbgPcJJPC9mCScfSZxpfFFUWOiXP6ArXYLMW0PveUeamiT4j1kPlO819uz_7dJ_0Cmttw1fmb8a3__tLb4uYANeWrXjfuiEtY3RXXJo7Kd01XLvnTtPfEd0d-1H3k8gvyZBIqKxfnDUpHdy2PkauDl-2qlYc1Z850KAk2ygOWpxcc4qYCUr6mpZMwZX-_pkfUpbs-AteQQU6XKziDNVTy3brq4MuyldDKGVcdNmjluKlXklNPfnz9xgcLvVlIwrbI-SNyTF7YjcxWjl1pV7wfH50cTL2B0sGDUMeph9o3SaJtjBqCAsO4HPkGAQg1WEiZPMtQ_BRaLEyhKJhCVdIQWMKFYZxEJrwvdqq6wgdC2pC1yRYqUQTpUCd-WIAFKH1IEmPCPfHi4qfmZuh3zrQbZ7k7dw_SfPu37InnG-lPfZ-PP8jtX-hHPlh7mwcUdGlurOfTS50m_PUZ-eRtpiOKdB_-k_RTcX16cpzl2Wz-5pG4wTKcVxMk-2Kna87xsbhqPnfLtnnijOAnZDAIdg
linkToPdf	http://cvtisr.summon.serialssolutions.com/2.0.0/link/0/eLvHCXMwpV3NbtQwELag_KgX_lELBeYAJxSxSRwnOUK32a5YViv-1Fvk2BOxUjepkhSxNx6B1-F1eBJmnHRZDiAhbpEzdizZ4_kmnplPiKfKRxuNpPQKW2hPRkXkkRlSXikVjqxJsXRZrh9n8XyenJyki4HnlHNh-voQmx9urBnuvGYFxzNbDtUGuEgmue3BZMbeZxpfFldkFDvNDORicxTT-dxT5qWSphCrIfKd-r_Y7v27TfoFNLfhqrM32c3_nuktcWOAmvCy3xu3xSWs7ohrE0flu6YnF_xp2rviuyM_6j5x-gVZMtCVhcV5g-DoruENcnbwsl21MK45cqZDINgIhyxPHxjjJgMSXtHRSZiyf1_TEHXpno-0K8gAx8uVPtVrXcG7ddXpL8sWdAtTzjps0ELW1Cvg0JMfX7_xxUKvFkDYFjl-BDKywq5lunLsSvfEh-zo_eGxN1A6eDpUceqh8k2SKBuj0kGBYVyOfINaE2qwOmXyLEP-U2ixMIUkZwplSU3aEi4M4yQy4X2xU9UV7gmwIe8mW8hEEqRDlfhhoa3Wpa-TxJhwXzy_WNTcDPXOmXbjNHf37kGaby_Lvni2kT7r63z8Qe7gYn_kg7a3eUBOl-LCej591O2Ev46RT97OVESe7oN_kn4iri_GWT6bzl8_FLsswmE1QXIgdrrmHB-Jq-Zzt2ybx04HfgLh1gfx
openUrl	ctx_ver=Z39.88-2004&ctx_enc=info%3Aofi%2Fenc%3AUTF-8&rfr_id=info%3Asid%2Fsummon.serialssolutions.com&rft_val_fmt=info%3Aofi%2Ffmt%3Akev%3Amtx%3Ajournal&rft.genre=article&rft.atitle=Underthrusting+and+Pure+Shear+Mechanisms+Dominate+the+Crustal+Deformation+Beneath+the+Core+of+the+Eastern+Himalayan+Syntaxis+as+Inferred+From+High%E2%80%90Resolution+Receiver+Function+Imaging&rft.jtitle=Geophysical+research+letters&rft.au=Xu%2C+Qiang&rft.au=Ding%2C+Lin&rft.au=Pei%2C+Shunping&rft.au=Yuan%2C+Xiaohui&rft.date=2022-12-28&rft.issn=0094-8276&rft.eissn=1944-8007&rft.volume=49&rft.issue=24&rft.epage=n%2Fa&rft_id=info:doi/10.1029%2F2022GL101697&rft.externalDBID=10.1029%252F2022GL101697&rft.externalDocID=GRL65289
thumbnail_l	http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/lc.gif&issn=0094-8276&client=summon
thumbnail_m	http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/mc.gif&issn=0094-8276&client=summon
thumbnail_s	http://covers-cdn.summon.serialssolutions.com/index.aspx?isbn=/sc.gif&issn=0094-8276&client=summon