Late Cambrian to Early Silurian Granitic Rocks of the Gemuri Area, Central Qiangtang, North Tibet: New Constraints on the Tectonic Evolution of the Northern Margin of Gondwana  

作　　者：WANG Haitao ZHAI Qingguo HU Peiyuan ZENG Lingsen TANG Yue ZHU Zhicai 

机构地区：[1]Key Laboratory of Deep–Earth Dynamaics of the Ministry of Nature Resources,Institute of Geology,Chinese Academy of Geological Sciences,Beijing 100037,China

出　　处：《Acta Geologica Sinica(English Edition)》2020年第4期1007-1019,共13页地质学报（英文版）

基　　金：supported by the Second Tibetan Plateau Scientific Expedition and Research(STEP)(Grant Nos.2019QZKK0703 and 2019QZKK0702);National Science Foundation of China(Grant Nos.91755103 and 41872240);Ministry of Science and Technology of China(Grant No.2016YFC0600304);the Chinese Geological Survey Project(Grant Nos.DD20190060,DD20190370 and DD20190057)。

摘　　要：The Paleozoic tectonic framework and paleo–plate configuration of the northern margin of Gondwana remain controversial. The South Qiangtang terrane is located along the northern margin of Gondwana and records key processes in the formation and evolution of this supercontinent. Here, we present new field, petrological, zircon U-Pb geochronological, and Lu-Hf isotopic data for granitic rocks of the Gemuri pluton, all of which provide new insights into the evolution of the northern margin of Gondwana. Zircon U-Pb dating of the Gemuri pluton yielded three concordant ages of 488.5 ± 2.1, 479.9 ± 8.9, and 438.5 ± 3.5 Ma. Combining these ages with the results of previous research indicates that the South Qiangtang terrane records two magmatic episodes at 502–471 and 453–439 Ma. These two episodes are associated with enriched zircon Hf isotopic compositions(εHf(t) =-10.1 to-3.9 and-16.6 to-6.5, respectively), suggesting the granites were formed by the partial melting of Paleoproterozoic–Mesoproterozoic metasedimentary rocks(Two–stage Hf model ages(TCDM) = 2094–1704 and 2466–1827 Ma, respectively). Combining these data with the presence of linearly distributed, contemporaneous Paleozoic igneous rocks along the northern margin of Gondwana, we suggest that all of these rocks were formed in an active continental margin setting. This manifests that the two magmatic episodes within the Gemuri area were associated with southward subduction in the Proto-(Paleo-) Tethys Ocean.

关 键 词：granitic rocks Early Paleozoic South Qiangtang TIBET GONDWANA 

分 类 号：P534.4[天文地球—古生物学与地层学] P542[天文地球—地质学] P588.121