{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,7,3]],"date-time":"2026-07-03T18:56:23Z","timestamp":1783104983461,"version":"3.54.6"},"reference-count":116,"publisher":"Geological Society of London","issue":"2","license":[{"start":{"date-parts":[[2021,10,28]],"date-time":"2021-10-28T00:00:00Z","timestamp":1635379200000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"content-domain":{"domain":["www.lyellcollection.org"],"crossmark-restriction":true},"short-container-title":["JGS"],"published-print":{"date-parts":[[2022,3]]},"abstract":"<jats:p>The Jurassic\u2013Cretaceous Tsoltak Formation of the eastern borderlands of Ladakh Himalaya consists of conglomerates, sandstones and shales, and is intruded by norite sills. It is the oldest sequence of continent-derived sedimentary rocks within the Shyok Suture. It also represents a rare outcrop of the basement rocks to the voluminous Late Cretaceous\u2013Eocene Ladakh Batholith. The Shyok Formation is a younger sequence of volcaniclastic rocks that overlie the Tsoltak Formation and record the Late Cretaceous closure of the Mesotethys Ocean. The petrogenesis of these formations, ophiolite-related harzburgites and norite sill is investigated through petrography, whole-rock geochemistry and U\u2013Pb zircon geochronology. The youngest detrital zircon grains from the Tsoltak Formation indicate an Early Cretaceous maximum depositional age and a distinctly Gondwanan, Lhasa microcontinent-related provenance with no Eurasian input. The Shyok Formation has a Late Cretaceous maximum depositional age and displays a distinct change in provenance to igneous detritus characteristic of the Jurassic\u2013Cretaceous magmatic arc along the southern margin of Eurasia. This is interpreted as a sign of collision of the Lhasa microcontinent and the Shyok ophiolite with Eurasia along the once continuous Shyok\u2013Bangong Suture. The accreted terranes became the new southernmost margin of Eurasia and the basement to the Trans-Himalayan Batholith associated with the India\u2013Eurasia convergence.<\/jats:p>\n          <jats:p content-type=\"supplementary-material\">\n            Supplementary material: Supplementary figures and Tables S1\u2013S3 are available at\n            <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"uri\" specific-use=\"dataset is-supplemented-by\" xlink:href=\"https:\/\/doi.org\/10.6084\/m9.figshare.c.5633162\">https:\/\/doi.org\/10.6084\/m9.figshare.c.5633162<\/jats:ext-link>\n          <\/jats:p>","DOI":"10.1144\/jgs2021-035","type":"journal-article","created":{"date-parts":[[2021,9,29]],"date-time":"2021-09-29T20:21:36Z","timestamp":1632946896000},"update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":4,"title":["Jurassic\u2013Cretaceous arc magmatism along the Shyok\u2013Bangong Suture of NW Himalaya: formation of the peri-Gondwana basement to the Ladakh Arc"],"prefix":"10.1144","volume":"179","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-7198-7776","authenticated-orcid":false,"given":"Wanchese M.","family":"Saktura","sequence":"first","affiliation":[{"name":"GeoQuEST Research Centre, School of Earth, Atmospheric &amp; Life Sciences, University of Wollongong, Wollongong, NSW 2522, Australia"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-5314-1331","authenticated-orcid":false,"given":"Solomon","family":"Buckman","sequence":"additional","affiliation":[{"name":"GeoQuEST Research Centre, School of Earth, Atmospheric &amp; Life Sciences, University of Wollongong, Wollongong, NSW 2522, Australia"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Allen P.","family":"Nutman","sequence":"additional","affiliation":[{"name":"GeoQuEST Research Centre, School of Earth, Atmospheric &amp; Life Sciences, University of Wollongong, Wollongong, NSW 2522, Australia"}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Renjie","family":"Zhou","sequence":"additional","affiliation":[{"name":"School of Earth and Environmental Sciences, The University of Queensland, St Lucia, QLD 4072, Australia"}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"1881","published-online":{"date-parts":[[2021,10,28]]},"reference":[{"key":"e_1_3_5_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.gr.2011.04.002"},{"key":"e_1_3_5_3_1","doi-asserted-by":"publisher","DOI":"10.1038\/307017a0"},{"key":"e_1_3_5_4_1","doi-asserted-by":"publisher","DOI":"10.1093\/petrology\/egw036"},{"key":"e_1_3_5_5_1","doi-asserted-by":"publisher","DOI":"10.1144\/0016-76492008-128"},{"key":"e_1_3_5_6_1","doi-asserted-by":"publisher","DOI":"10.1086\/628815"},{"key":"e_1_3_5_7_1","doi-asserted-by":"publisher","DOI":"10.1007\/BF00375292"},{"key":"e_1_3_5_8_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.jseaes.2008.03.013"},{"key":"e_1_3_5_9_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.chemgeo.2004.01.003"},{"key":"e_1_3_5_10_1","doi-asserted-by":"publisher","DOI":"10.1002\/2015TC003933"},{"key":"e_1_3_5_11_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.epsl.2013.01.023"},{"key":"e_1_3_5_12_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.gr.2018.07.003"},{"key":"e_1_3_5_13_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.epsl.2006.12.006"},{"key":"e_1_3_5_14_1","doi-asserted-by":"publisher","DOI":"10.2113\/gsecongeo.51.7.712"},{"key":"e_1_3_5_15_1","doi-asserted-by":"publisher","DOI":"10.1046\/j.1440-1738.2002.00371.x"},{"key":"e_1_3_5_16_1","doi-asserted-by":"publisher","DOI":"10.1086\/323191"},{"key":"e_1_3_5_17_1","doi-asserted-by":"publisher","DOI":"10.1016\/0012-821X(86)90186-X"},{"key":"e_1_3_5_18_1","doi-asserted-by":"publisher","DOI":"10.1016\/0012-821X(75)90223-X"},{"key":"e_1_3_5_19_1","doi-asserted-by":"publisher","DOI":"10.1007\/978-94-017-2809-6_15"},{"key":"e_1_3_5_20_1","first-page":"2164","article-title":"Plate tectonics and sandstone compositions","volume":"63","author":"Dickinson W.R.","year":"1979","unstructured":"Dickinson, W.R. and Suczek, C.A. 1979. 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