{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,3,6]],"date-time":"2026-03-06T18:28:49Z","timestamp":1772821729332,"version":"3.50.1"},"reference-count":129,"publisher":"Geological Society of London","issue":"2","license":[{"start":{"date-parts":[[2019,11,19]],"date-time":"2019-11-19T00:00:00Z","timestamp":1574121600000},"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":["41702199"],"award-info":[{"award-number":["41702199"]}],"id":[{"id":"10.13039\/501100001809","id-type":"DOI","asserted-by":"crossref"}]},{"DOI":"10.13039\/501100001809","name":"National Natural Science Foundation of China","doi-asserted-by":"crossref","award":["41890830, 41890834"],"award-info":[{"award-number":["41890830, 41890834"]}],"id":[{"id":"10.13039\/501100001809","id-type":"DOI","asserted-by":"crossref"}]},{"DOI":"10.13039\/501100004543","name":"China Scholarship Council","doi-asserted-by":"crossref","award":["201708515142"],"award-info":[{"award-number":["201708515142"]}],"id":[{"id":"10.13039\/501100004543","id-type":"DOI","asserted-by":"crossref"}]}],"content-domain":{"domain":["www.lyellcollection.org"],"crossmark-restriction":true},"short-container-title":["JGS"],"published-print":{"date-parts":[[2020,3]]},"abstract":"<jats:p>\n            The evolutionary history of the NW Yangtze Block is important in interpreting its location and relationship with the Rodinia supercontinent. Although a Neoproterozoic arc-related tectonothermal event is recognized in the Micangshan area of the NW Yangtze Block, its timing and\n            <jats:italic>P\u2013T<\/jats:italic>\n            conditions are poorly constrained. We address this issue by focusing on the garnet\u2013biotite gneiss that represents the main lithology of the Huodiya Group on the NW margin of the Yangtze Block. This gneiss is predominantly composed of garnet, biotite, feldspar and quartz. The peak mineral assemblage in the matrix consists of garnet\u2009+\u2009biotite\u2009+\u2009quartz\u2009+\u2009plagioclase\u2009+\u2009K-feldspar. The retrograde stage is characterized by embayed rims of the garnet and its associated biotite in the matrix. The\n            <jats:italic>P\u2013T<\/jats:italic>\n            conditions in the peak and retrograde stages are constrained to 7\u20138\u2005kbar and\n            <jats:italic>c.<\/jats:italic>\n            710\u00b0C and 5\u20136\u2005kbar and 650\u2013675\u00b0C, respectively, and suggest that 4\u20135\u2005vol.% melt was produced during an upper amphibolite\u2013granulite facies metamorphic event. The first report of monazite U\u2013Pb dating in the Huodiya Group of the Micangshan area yielded a weighted mean\n            <jats:sup>206<\/jats:sup>\n            Pb\/\n            <jats:sup>238<\/jats:sup>\n            U age of 802\u2009\u00b1\u20095\u2005Ma. The studied samples contained detrital igneous zircons with\n            <jats:sup>206<\/jats:sup>\n            Pb\/\n            <jats:sup>238<\/jats:sup>\n            U dates &gt;800\u2005Ma, whereas the metamorphic zircons yielded a weighted mean\n            <jats:sup>206<\/jats:sup>\n            Pb\/\n            <jats:sup>238<\/jats:sup>\n            U age of 797\u2009\u00b1\u20099\u2005Ma. Based on the compressional tectonic environment and previous studies, we propose that the Yangtze Block was probably located on the periphery of the Rodinia supercontinent.\n          <\/jats:p>\n          <jats:p content-type=\"supplementary-material\">\n            <jats:bold>Supplementary material:<\/jats:bold>\n            The analytical methods are summarized in\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.4698356\">Supplementary<\/jats:ext-link>\n            Text File 1. Representative mineral composition and the results of U\u2013Pb isotopic analyses of monazites and zircons are presented in\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.4698356\">supplementary table 1\u20137<\/jats:ext-link>\n            . The results of trace element concentrations in garnets are presented in\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.4698356\">Supplementary table 8<\/jats:ext-link>\n            .\n            <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"uri\" xlink:href=\"https:\/\/doi.org\/10.6084\/m9.figshare.c.4698356\">https:\/\/doi.org\/10.6084\/m9.figshare.c.4698356<\/jats:ext-link>\n          <\/jats:p>","DOI":"10.1144\/jgs2019-035","type":"journal-article","created":{"date-parts":[[2019,10,18]],"date-time":"2019-10-18T17:45:14Z","timestamp":1571420714000},"page":"424-441","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":21,"title":["Recognition and significance of\n            <i>c.<\/i>\n            800\u2005Ma upper amphibolite to granulite facies metamorphism in metasedimentary rocks from the NW margin of the Yangtze Block"],"prefix":"10.1144","volume":"177","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-6154-9561","authenticated-orcid":false,"given":"Wang","family":"Haozheng","sequence":"first","affiliation":[{"name":"School of Geoscience and Technology, Division of Key Laboratory of Carbonate Reservoirs, CNPC, Southwest Petroleum University, Chengdu 610500, China"},{"name":"Department of Earth Science, Federal Institute of Technology, Zurich 8049, Switzerland"},{"name":"Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China"}]},{"given":"Laurent","family":"Oscar","sequence":"additional","affiliation":[{"name":"Department of Earth Science, Federal Institute of Technology, Zurich 8049, Switzerland"}]},{"given":"Zhang","family":"Huafeng","sequence":"additional","affiliation":[{"name":"Department of Geoscience and Resource, China University of Geosciences, Beijing 100083, China"}]},{"given":"Zhang","family":"Hong","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Continental Dynamics, Department of Geology, Northwest University, Xi'an 710069, China"}]},{"given":"Chen","family":"Xi","sequence":"additional","affiliation":[{"name":"School of Geoscience and Technology, Division of Key Laboratory of Carbonate Reservoirs, CNPC, Southwest Petroleum University, Chengdu 610500, China"}]},{"ORCID":"https:\/\/orcid.org\/0000-0001-6341-3513","authenticated-orcid":false,"given":"Zhai","family":"Mingguo","sequence":"additional","affiliation":[{"name":"Institute of Geology and Geophysics, Chinese Academy of Sciences, Beijing 100029, China"}]}],"member":"1881","published-online":{"date-parts":[[2019,11,19]]},"reference":[{"key":"e_1_3_4_2_1","doi-asserted-by":"publisher","DOI":"10.1007\/s00410-002-0364-7"},{"key":"e_1_3_4_3_1","doi-asserted-by":"publisher","DOI":"10.1180\/minmag.2010.074.4.659"},{"key":"e_1_3_4_4_1","doi-asserted-by":"publisher","DOI":"10.1130\/G34395.1"},{"key":"e_1_3_4_5_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.earscirev.2017.06.001"},{"key":"e_1_3_4_6_1","doi-asserted-by":"publisher","DOI":"10.1111\/j.1525-1314.1998.00074.x"},{"key":"e_1_3_4_7_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.precamres.2018.01.010"},{"key":"e_1_3_4_8_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.gca.2003.07.012"},{"key":"e_1_3_4_9_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.jeurceramsoc.2010.12.019"},{"key":"e_1_3_4_10_1","doi-asserted-by":"publisher","DOI":"10.1016\/0012-821X(87)90227-5"},{"key":"e_1_3_4_11_1","doi-asserted-by":"publisher","DOI":"10.1046\/j.1525-1314.2002.00395.x"},{"key":"e_1_3_4_12_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.epsl.2005.04.033"},{"key":"e_1_3_4_13_1","doi-asserted-by":"publisher","DOI":"10.1029\/2009GC002540"},{"key":"e_1_3_4_14_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.lithos.2018.05.003"},{"key":"e_1_3_4_15_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.precamres.2011.05.002"},{"key":"e_1_3_4_16_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.precamres.2011.12.007"},{"key":"e_1_3_4_17_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.gr.2015.12.001"},{"key":"e_1_3_4_18_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.lithos.2014.03.002"},{"key":"e_1_3_4_19_1","doi-asserted-by":"publisher","DOI":"10.1007\/s00410-007-0201-0"},{"key":"e_1_3_4_20_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.lithos.2006.06.003"},{"key":"e_1_3_4_21_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0012-821X(00)00212-0"},{"key":"e_1_3_4_22_1","first-page":"201","article-title":"Ternary-feldspar modeling and thermometry","volume":"73","author":"Fuhrman M.L.","year":"1988","unstructured":"Fuhrman, M.L. & Lindsley, D.H. 1988. 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