Journal of Jilin University(Earth Science Edition) ›› 2019, Vol. 49 ›› Issue (6): 1658-1671.doi: 10.13278/j.cnki.jjuese.20190037

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Indosinian Metamorphic Deformation Sequence of Badu Group in Suichang-Dazhe Region,Southwestern Zhejiang

Shi Lei1,2, Zhou Xiwen3, Zheng Changqing1,2, Dong Yunfeng1,2, Zhou Xiao1,2, Guo Tengda1,2   

  1. 1. College of Earth Sciences, Jilin University, Changchun 130061, China;
    2. Key Laboratory of Mineral Resources Evaluation in Northeast Asia, Ministry of Natural Resources, Changchun 130061, China;
    3. Institute of Geology, Chinese Academy of Geological Sciences, Beijing 100037, China
  • Received:2019-03-03 Published:2019-11-30
  • Supported by:
    Supported by National Natural Science Foundation of China (41472164, 41872192) and Project of China Geological Survey (121201102000150020-06)

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Abstract: The Badu Group in Suichang-Dazhe region of southwestern Zhejiang underwent metamorphism and deformation under the influence of Indosinian metamorphic event. Through a detailed field investigation and lithofacies study, it can be divided into three metamorphism-deformation sequences:for S1 deformation period,the residual tight folds are recorded by NW-trending gneisses,and the symbiotic mineral assemblages are garnet metamorphic phenocrysts with inclusion minerals of garnet+biotite+quartz (argillaceous) and garnet + amphibole+plagioclase+quartz (feldspar) distributed directionally; for S2 deformation period,the regional wide-gentle folds and NE-trending gently inclined permeable gneisses are developed,and the symbiotic mineral assemblages are garnet metamorphic phenocrysts and matrix minerals of garnet+biotite+silica+quartz+K-feldspar+plagioclase (argillaceous) and garnet+K-feldspar+plagioclase+biotite+quartz (feldspar); for S3 deformation period,the NE-trending steeply inclined permeable gneisses and ductile-brittle fractures are mostly filled by granite porphyry veins, and the symbiotic mineral assemblages are garnet metamorphic phenocrysts and their retrograde edge minerals of garnet+cordierite+sillimanite+plagioclase+biotite+quartz+K-feldspar (argillaceous) and amphibole+plagioclase+biotite+ilmenite (feldspar). Combined with the previous research results, the peak metamorphic degree of Indosinian metamorphic event of Badu Group reached granulite facies,showing a clockwise near isothermal decompression (ITD) type p-T evolution track. The S1-S3 metamorphism and deformation reflect the evolution from subduction collision to rapid re-cooling. The zircon U-Pb dating results of granite porphyry restrict the completion time of the evolution process to 229.7 Ma, which may be the response of southwestern Zhejiang to the subduction-collision between the Indosinian-South China-North China plate to the Paleo-Tethyan Ocean during Indosinian.

Key words: Badu Group, metamorphism-deformation sequence, symbiotic mineral asse-mblages, zircon U-Pb dating, southwestern Zhejiang Province

CLC Number: 

  • P588.34
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[7] DONG Chun-yan,MA Rui,CHI Xiao-guo,LIU Jian-feng,LI Guang-rong. An Experimental Study on the Relationship Between Stress and Rock Melt[J]. J4, 2006, 36(02): 177 -0182 .
[8] WANG Guo-ping,ZHANG Yu-xia,ZHAI Zheng-li,JIA Lin. Ratios of Specific Elements and Their Implications for Original Source of Sediments and Redox Condition within Sedimentation Profile of the Marsh in Semiarid Areas[J]. J4, 2006, 36(03): 449 -454 .
[9] XIAO Chang-lai , ZHANG Li-chun ,FANG Zhang ,JIA Tao. Research on Transform Relationship Between Surface Water and Groundwater in Taoer River Fan[J]. J4, 2006, 36(02): 234 -0239 .
[10] YANG Jun-peng, HU Ke, LIU Yu-ying. The Stable Carbon Isotopic Characteristics of Carbonates in Salini alkani Soil in the West Jilin Province[J]. J4, 2006, 36(02): 245 -0249 .
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