FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2151979402> ?p ?o ?g. }

• W2151979402 endingPage "1074" @default.
• W2151979402 startingPage "1071" @default.
• W2151979402 abstract "Research Article| October 01, 2013 Synchronous Oligocene–Miocene metamorphism of the Pamir and the north Himalaya driven by plate-scale dynamics Michael A. Stearns; Michael A. Stearns 1Earth Science Department, University of California–Santa Barbara, Santa Barbara, California 93106, USA Search for other works by this author on: GSW Google Scholar Bradley R. Hacker; Bradley R. Hacker 1Earth Science Department, University of California–Santa Barbara, Santa Barbara, California 93106, USA Search for other works by this author on: GSW Google Scholar Lothar Ratschbacher; Lothar Ratschbacher 2Geologie, Technische Universität Bergakademie Freiberg, 09599 Freiberg, Germany Search for other works by this author on: GSW Google Scholar Jeffrey Lee; Jeffrey Lee 3Geological Sciences, Central Washington University, Ellensburg, Washington 98926, USA Search for other works by this author on: GSW Google Scholar John M. Cottle; John M. Cottle 1Earth Science Department, University of California–Santa Barbara, Santa Barbara, California 93106, USA Search for other works by this author on: GSW Google Scholar Andrew Kylander-Clark Andrew Kylander-Clark 1Earth Science Department, University of California–Santa Barbara, Santa Barbara, California 93106, USA Search for other works by this author on: GSW Google Scholar Geology (2013) 41 (10): 1071–1074. https://doi.org/10.1130/G34451.1 Article history received: 04 Feb 2013 rev-recd: 27 May 2013 accepted: 30 May 2013 first online: 09 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share MailTo Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation Michael A. Stearns, Bradley R. Hacker, Lothar Ratschbacher, Jeffrey Lee, John M. Cottle, Andrew Kylander-Clark; Synchronous Oligocene–Miocene metamorphism of the Pamir and the north Himalaya driven by plate-scale dynamics. Geology 2013;; 41 (10): 1071–1074. doi: https://doi.org/10.1130/G34451.1 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGeology Search Advanced Search Abstract Gneiss domes in the Pamir (Central Asia) and the Himalaya provide key data on mid- to deep-crustal processes operating during the India-Asia collision. Laser ablation split-stream inductively coupled plasma–mass spectrometry (LASS-ICP-MS) data from monazite in these domes yield a time record from U/Th-Pb dates and a petrologic record from rare earth element (REE) abundances. Seven samples from the Pamir and six samples from the north Himalayan gneiss domes yield almost identical monazite dates of ca. 28–15 Ma. Most monazite has invariant heavy REE (HREE) abundances; two samples, however, have older monazite that records progressive HREE depletion and two samples have younger monazite that records progressive HREE enrichment. These variations in HREE are compatible with increasing garnet abundance—prograde metamorphism—until ca. 20 Ma, and decreasing garnet abundance thereafter. The change from HREE depletion to enrichment may record a transition from crustal thickening and heating to dome exhumation and cooling. This documentation of synchronous Barrovian metamorphism within domes of Indian crust along the margin of the orogen (Himalaya) and within domes of Asian crust within the core of the orogen (Pamir) is best explained by a plate-scale driving force rather than by local events. We propose that widespread, synchronous thickening was initiated by the resumption of Indian subduction following slab breakoff and then terminated by a second slab-tearing event—both plate-scale events inferred from tomography. You do not have access to this content, please speak to your institutional administrator if you feel you should have access." @default.
• W2151979402 created "2016-06-24" @default.
• W2151979402 creator A5002379406 @default.
• W2151979402 creator A5012947471 @default.
• W2151979402 creator A5024521229 @default.
• W2151979402 creator A5024788787 @default.
• W2151979402 creator A5051857603 @default.
• W2151979402 creator A5089288874 @default.
• W2151979402 date "2013-07-30" @default.
• W2151979402 modified "2023-09-23" @default.
• W2151979402 title "Synchronous Oligocene-Miocene metamorphism of the Pamir and the north Himalaya driven by plate-scale dynamics" @default.
• W2151979402 cites W1944113931 @default.
• W2151979402 cites W1977966931 @default.
• W2151979402 cites W1988337184 @default.
• W2151979402 cites W2003346743 @default.
• W2151979402 cites W2011893217 @default.
• W2151979402 cites W2015509055 @default.
• W2151979402 cites W2020159892 @default.
• W2151979402 cites W2020631504 @default.
• W2151979402 cites W2025750942 @default.
• W2151979402 cites W2046223350 @default.
• W2151979402 cites W2046809141 @default.
• W2151979402 cites W2049451277 @default.
• W2151979402 cites W2058958898 @default.
• W2151979402 cites W2070404541 @default.
• W2151979402 cites W2078758544 @default.
• W2151979402 cites W2094414093 @default.
• W2151979402 cites W2103631538 @default.
• W2151979402 cites W2105755619 @default.
• W2151979402 cites W2125124494 @default.
• W2151979402 cites W2125411571 @default.
• W2151979402 cites W2135818211 @default.
• W2151979402 cites W2144583290 @default.
• W2151979402 cites W2154135181 @default.
• W2151979402 cites W2166860096 @default.
• W2151979402 cites W2167590372 @default.
• W2151979402 cites W2168591219 @default.
• W2151979402 cites W2334467792 @default.
• W2151979402 doi "https://doi.org/10.1130/g34451.1" @default.
• W2151979402 hasPublicationYear "2013" @default.
• W2151979402 type Work @default.
• W2151979402 sameAs 2151979402 @default.
• W2151979402 citedByCount "74" @default.
• W2151979402 countsByYear W21519794022013 @default.
• W2151979402 countsByYear W21519794022014 @default.
• W2151979402 countsByYear W21519794022015 @default.
• W2151979402 countsByYear W21519794022016 @default.
• W2151979402 countsByYear W21519794022017 @default.
• W2151979402 countsByYear W21519794022018 @default.
• W2151979402 countsByYear W21519794022019 @default.
• W2151979402 countsByYear W21519794022020 @default.
• W2151979402 countsByYear W21519794022021 @default.
• W2151979402 countsByYear W21519794022022 @default.
• W2151979402 countsByYear W21519794022023 @default.
• W2151979402 crossrefType "journal-article" @default.
• W2151979402 hasAuthorship W2151979402A5002379406 @default.
• W2151979402 hasAuthorship W2151979402A5012947471 @default.
• W2151979402 hasAuthorship W2151979402A5024521229 @default.
• W2151979402 hasAuthorship W2151979402A5024788787 @default.
• W2151979402 hasAuthorship W2151979402A5051857603 @default.
• W2151979402 hasAuthorship W2151979402A5089288874 @default.
• W2151979402 hasConcept C111919701 @default.
• W2151979402 hasConcept C112764850 @default.
• W2151979402 hasConcept C127313418 @default.
• W2151979402 hasConcept C151730666 @default.
• W2151979402 hasConcept C161191863 @default.
• W2151979402 hasConcept C199360897 @default.
• W2151979402 hasConcept C2778447006 @default.
• W2151979402 hasConcept C2778805511 @default.
• W2151979402 hasConcept C41008148 @default.
• W2151979402 hasConcept C52119013 @default.
• W2151979402 hasConcept C86844869 @default.
• W2151979402 hasConcept C95457728 @default.
• W2151979402 hasConceptScore W2151979402C111919701 @default.
• W2151979402 hasConceptScore W2151979402C112764850 @default.
• W2151979402 hasConceptScore W2151979402C127313418 @default.
• W2151979402 hasConceptScore W2151979402C151730666 @default.
• W2151979402 hasConceptScore W2151979402C161191863 @default.
• W2151979402 hasConceptScore W2151979402C199360897 @default.
• W2151979402 hasConceptScore W2151979402C2778447006 @default.
• W2151979402 hasConceptScore W2151979402C2778805511 @default.
• W2151979402 hasConceptScore W2151979402C41008148 @default.
• W2151979402 hasConceptScore W2151979402C52119013 @default.
• W2151979402 hasConceptScore W2151979402C86844869 @default.
• W2151979402 hasConceptScore W2151979402C95457728 @default.
• W2151979402 hasIssue "10" @default.
• W2151979402 hasLocation W21519794021 @default.
• W2151979402 hasOpenAccess W2151979402 @default.
• W2151979402 hasPrimaryLocation W21519794021 @default.
• W2151979402 hasRelatedWork W1001487360 @default.
• W2151979402 hasRelatedWork W2010494433 @default.
• W2151979402 hasRelatedWork W2069196149 @default.
• W2151979402 hasRelatedWork W2087881480 @default.
• W2151979402 hasRelatedWork W2127665746 @default.
• W2151979402 hasRelatedWork W2151614148 @default.
• W2151979402 hasRelatedWork W2153573251 @default.
• W2151979402 hasRelatedWork W2156221353 @default.
• W2151979402 hasRelatedWork W2763108616 @default.

• next