Neoproterozoic(750–711 Ma)Tectonics of the South Qinling Belt,Central China:New Insights from Geochemical,Zircon U-Pb Geochronological,and Sr-Nd Isotopic Data from the Niushan Complex  

作　　者：WANG Shuo LIU Yunhua YANG Benzhao TAN Le LI Xiaoyan DENG Nan 

机构地区：[1]School of Earth Sciences and Resources,Chang'an University,Xi'an 710054,China [2]Geological Team No.1 of Shaanxi Bureau of Geology and Mineral Resources,Ankang,Shannxi 725000 China [3]Longshou Mine of Jinchuan Group Co.,Ltd,Jinchang,Gansu 737100,China [4]Xi'an Mineral Resources Survey Center,China Geological Survey,Xi'an 710100,China

出　　处：《Acta Geologica Sinica(English Edition)》2023年第1期106-121,共16页地质学报（英文版）

基　　金：supported by the National Natural Science Foundation of China(Grant No.41872219);the Key Research and Development Program of Shaanxi(Grant No.2019SF-245);the Natural Science Foundation of Shaanxi Province(Grant No.2023-JC-YB-222);an integrated research project of Integrated Exploration of China Geological Survey(Grant No.WKZB1911BJM300369/002)。

摘　　要：The Xiejiaba and Fuqiangbei plutons form part of the newly identified Neoproterozoic Niushan complex,which is located in the southern South Qinling belt(SQB).The plutons are compositionally similar,were emplaced at 750–711Ma,and provide insights into Neoproterozoic tectonism within the South Qinling belt.The Xiejiaba pluton contains diorite,quartz diorite,granodiorite,and granite phases,all of which are sub-alkaline and have variable major element compositions with negative correlations between SiO_(2)and MgO,TFe_(2)O_(3),Al_(2)O_(3),CaO,TiO_(2)and P_(2)O_(5).These rocks are enriched in light rare earth elements(LREEs)and large ion lithophile elements(LILEs)and have negative Nb,Ta,P and Ti anomalies,all of which are indicative of arc-type magmatism.The Fuqiangbei pluton contains granitoids that are compositionally similar to the rocks in the Xiejiaba pluton.Samples from these plutons have similarε_(Nd)(t)values(1.24–5.99)but very variable(^(87)Sr/^(86)Sr)i values(0.7010–0.7054).Combining these data with the geochemical data for these rocks suggests that the magmas that formed the Niushan complex were derived from the crust–mantle boundary.This,combined with the results of previous research,suggests that the transition from low pressure-low temperature to low pressure-high temperature conditions within a subduction zone caused melting during a period of late subduction and backarc extension.This constrain the timing of subduction within the South Qinling belt and the northern Yangtze Block(YB)to 750–711 Ma,with this Neoproterozoic subduction associated with an ocean to the north overprinting an existing continental rift-type tectonic setting within the northern margin of the Yangtze Block and the South Qinling belt.

关 键 词：geochronology geochemistry magmatism TECTONICS PRECAMBRIAN South Qinling 

分 类 号：P534.3[天文地球—古生物学与地层学] P587[天文地球—地质学] P597.3