{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,3,20]],"date-time":"2026-03-20T21:28:35Z","timestamp":1774042115869,"version":"3.50.1"},"reference-count":103,"publisher":"Geological Society of London","issue":"2","license":[{"start":{"date-parts":[[2018,11,27]],"date-time":"2018-11-27T00:00:00Z","timestamp":1543276800000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"funder":[{"DOI":"10.13039\/501100001809","name":"National Natural Science Foundation of China","doi-asserted-by":"crossref","award":["41421002, 41190074 and 41772226"],"award-info":[{"award-number":["41421002, 41190074 and 41772226"]}],"id":[{"id":"10.13039\/501100001809","id-type":"DOI","asserted-by":"crossref"}]},{"name":"National Key Research and Development Program of China","award":["2016YFC0601003 and 2016YFC0600202"],"award-info":[{"award-number":["2016YFC0601003 and 2016YFC0600202"]}]}],"content-domain":{"domain":["www.lyellcollection.org"],"crossmark-restriction":true},"short-container-title":["JGS"],"published-print":{"date-parts":[[2019,3]]},"abstract":"<jats:p>\n            The East Kunlun Orogenic Belt of the northern Tibetan Plateau can be divided by the Qimantagh\u2013Xiangride, Aqikekulehu\u2013Kunzhong and Muztagh\u2013Buqingshan sutures into, from north to south, the Northern Qimantagh, Central Kunlun and Southern Kunlun belts. The Yazidaban ophiolitic m\u00e9lange, located in the westernmost region of the Qimantagh\u2013Xiangride suture between the Northern Qimantagh and Central Kunlun belts, consists predominantly of serpentinite, basalt, diabase and andesite. The serpentinites are characterized by low total rare earth element (\u03a3REE) concentrations and depletion of mid-REEs, showing an ophiolitic ultramafic affinity. The basalts have low \u03a3REE concentrations, a slight enrichment in light REEs, depletion of large ion lithophile elements and insignificant fractionation of high field strength elements, which are attributed to an incompatible element-enriched mid-ocean ridge basalt. Both diabases and andesites are characterized by high \u03a3REE, strong enrichment in light REEs, depletion of Nb, Ta, P and Ti, and significant fractionation of high field strength elements. These geochemical characteristics indicate that the diabase and andesite were mostly generated in a subduction-related setting. Igneous zircons from the diabase yielded a\n            <jats:sup>206<\/jats:sup>\n            Pb\/\n            <jats:sup>238<\/jats:sup>\n            U age of 421.5\u2009\u00b1\u20092.2\u2005Ma (MSWD\u2009=\u20090.44), representing the formation time of the subduction-related rocks. Together with the regional geology, these constraints on the ultramafic rock, basalt, andesite and diabase suggest that the Yazidaban ophiolitic m\u00e9lange represents the remnants of oceanic crust from a back-arc basin and the associated subduction-related magmatic rocks.\n          <\/jats:p>\n          <jats:p content-type=\"supplementary-material\">\n            <jats:bold>Supplementary material:<\/jats:bold>\n            Details of U\u2013Th\u2013Pb laser ablation inductively coupled plasma mass spectrometry data of zircons from the diabase, and major and trace element compositions for the samples from the Qimantagh m\u00e9lange, East Kunlun Orogen 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.4283219\">https:\/\/doi.org\/10.6084\/m9.figshare.c.4283219<\/jats:ext-link>\n          <\/jats:p>","DOI":"10.1144\/jgs2018-145","type":"journal-article","created":{"date-parts":[[2018,11,5]],"date-time":"2018-11-05T14:06:14Z","timestamp":1541426774000},"page":"306-322","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":54,"title":["Geochronology and geochemistry of the Yazidaban ophiolitic m\u00e9lange in Qimantagh: constraints on the Early Paleozoic back-arc basin of the East Kunlun Orogen, northern Tibetan Plateau"],"prefix":"10.1144","volume":"176","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-5002-2123","authenticated-orcid":false,"given":"Yunpeng","family":"Dong","sequence":"first","affiliation":[{"name":"State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Northern Taibai Street 229, Xi'an 710069, China"},{"name":"Department of Earth Sciences, Western University, 1151 Richmond Street, London, Ontario, Canada N6A 3K7"}]},{"given":"Shengsi","family":"Sun","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Northern Taibai Street 229, Xi'an 710069, China"}]},{"given":"Xiaoming","family":"Liu","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Northern Taibai Street 229, Xi'an 710069, China"}]},{"given":"Dengfeng","family":"He","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Northern Taibai Street 229, Xi'an 710069, China"}]},{"given":"Xiaohu","family":"Zhou","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Northern Taibai Street 229, Xi'an 710069, China"}]},{"given":"Feifei","family":"Zhang","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Northern Taibai Street 229, Xi'an 710069, China"}]},{"given":"Zhao","family":"Yang","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Northern Taibai Street 229, Xi'an 710069, China"}]},{"given":"Dingwu","family":"Zhou","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Northern Taibai Street 229, Xi'an 710069, China"}]}],"member":"1881","published-online":{"date-parts":[[2018,11,27]]},"reference":[{"key":"e_1_3_4_2_1","doi-asserted-by":"publisher","DOI":"10.1007\/BF00371381"},{"key":"e_1_3_4_3_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0009-2541(02)00195-X"},{"key":"e_1_3_4_4_1","doi-asserted-by":"publisher","DOI":"10.1016\/0009-2541(85)90076-2"},{"key":"e_1_3_4_5_1","first-page":"283","volume-title":"Komatiities","author":"Beswick A.E.","year":"1982","unstructured":"Beswick, A.E. 1982. Some geochemical aspects of alteration and genetic relations in komatiitic suites. In: Arndt, N.T. & Nisbet, E.G. (eds) Komatiities. George Allen & Unwin, London, 283\u2013308."},{"key":"e_1_3_4_6_1","doi-asserted-by":"publisher","DOI":"10.1007\/BF03187200"},{"key":"e_1_3_4_7_1","first-page":"501","article-title":"A preliminary study of the Kunlun\u2013Qilian\u2013Qinling suture system","volume":"23","author":"Bian Q.T.","year":"2002","unstructured":"Bian, Q.T., Zhao, D.S., Ye, Z.R., Chang, C.F., Luo, X.Q. & Gao, S.L. 2002. A preliminary study of the Kunlun\u2013Qilian\u2013Qinling suture system. 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Geological Bulletin of China, 25, 1311\u20131314 [in Chinese with English abstract].","journal-title":"Geological Bulletin of China"},{"key":"e_1_3_4_15_1","first-page":"1","article-title":"Lithological characteristics of the Baishahe Formation to the south of Xiangride town, eastern Kunlun Mountains and its age constrained from zircon Pb-Pb dating","volume":"25","author":"Chen N.S.","year":"2006","unstructured":"Chen, N.S., Li, X.Y., Zhang, K.X., Wang, G.C., Zhu, Y.H., Hou, G.J. & Bai, Y.S. 2006b. Lithological characteristics of the Baishahe Formation to the south of Xiangride town, eastern Kunlun Mountains and its age constrained from zircon Pb-Pb dating. 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