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U-Pb Zircon Geochronology and Geochemistry of Granitoids in the Douling Group in the Eastern Qinling

ZHANG Chengli LI Miao WANG Tao YUAN Honglin YAN Yunxiang LIU Xiaoming WANG Jianqi LIU Ye

地质学报(英文版)2004,Vol.78Issue(1):83-95,13.
地质学报(英文版)2004,Vol.78Issue(1):83-95,13.

U-Pb Zircon Geochronology and Geochemistry of Granitoids in the Douling Group in the Eastern Qinling

U-Pb Zircon Geochronology and Geochemistry of Granitoids in the Douling Group in the Eastern Qinling

ZHANG Chengli 1LI Miao 2WANG Tao 1YUAN Honglin 3YAN Yunxiang 1LIU Xiaoming 1WANG Jianqi 1LIU Ye1

作者信息

  • 1. The Key Laboratory of Continental Dynamics, Ministry of Education, Department of Geology, Northwest University, Xi'an, Shaanxi 710069
  • 2. State Key Laboratory for Mineral Deposits Research, Nanjing University, Nanjing, Jiangsu 210093
  • 3. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037
  • 折叠

摘要

Abstract

LA-ICPMS U-Pb zircon dating of the Sanpinggou, Gangou and Fengzishan granitoids in the Douling Group of the Eastern Qinling yields ages of 760-685 Ma, which represents a strong tectono-magmatic event in the southern Qinling during the late Neoproterozoic. Geochemical data show that these intrusions have wide compositions ranging from minor gabbros through diorites to granodiorites. They are relatively enriched in LILE, poor in HFSE and strongly depleted in Nb and Ta, displaying affinities of I-type granites formed in an active continental margin with oceanic subduction. In contrast to granitoids, gabbros and enclaves in the granitoids have higher REE abundances, relatively flat REE patterns, lower LILE, slightly higher HFSE and more depletion in Nb and Ta. All these suggest that the gabbros were formed by partial melting of the upper mantle above the subduction zone and the granitoids by the partial melting of the lower crust. Combined with regional geological data, the subduction-related granitoids in the Douling Group, together with the Tuwushan A-type granite with an age of 725 Ma and contemporaneous basic dikes in the Wudang Block, provide evidence for local subduction of oceanic basins between different blocks during the rifling in the Southern Qinling in the Neoproterozoic. Thus, the coexistences of various magmatic rocks formed in different tectonic environments indicate a complicated tectonic evolution and variety of tectonic frameworks in the Qinling area in the Neoproterozoic.

关键词

Granitoids/LA-ICPMS zircon U-Pb dating/Geochemistry/Douling Group/Eastern Qinling

Key words

Granitoids/LA-ICPMS zircon U-Pb dating/Geochemistry/Douling Group/Eastern Qinling

引用本文复制引用

ZHANG Chengli,LI Miao,WANG Tao,YUAN Honglin,YAN Yunxiang,LIU Xiaoming,WANG Jianqi ,LIU Ye..U-Pb Zircon Geochronology and Geochemistry of Granitoids in the Douling Group in the Eastern Qinling[J].地质学报(英文版),2004,78(1):83-95,13.

基金项目

This research is jointly supported by the National Natural Science Foundation of China (grant Nos. 40032010-C,40072065 and 40372039) and the Foundation of Senior Visiting Scholarship of Western Colleges, Ministry of Education, China. (grant Nos. 40032010-C,40072065 and 40372039)

地质学报(英文版)

1000-9515

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