浙西南遂昌—大柘地区八都岩群印支期变质变形序列

doi:10.13278/j.cnki.jjuese.20190037

吉林大学学报(地球科学版) ›› 2019, Vol. 49 ›› Issue (6): 1658-1671.doi: 10.13278/j.cnki.jjuese.20190037

浙西南遂昌—大柘地区八都岩群印支期变质变形序列

石磊^1,2, 周喜文³, 郑常青^1,2, 董云峰^1,2, 周枭^1,2, 郭腾达^1,2

1. 吉林大学地球科学学院, 长春 130061;
2. 自然资源部东北亚矿产资源评价重点实验室, 长春 130061;
3. 中国地质科学院地质研究所, 北京 100037

收稿日期:2019-03-03 发布日期:2019-11-30
通讯作者: 郑常青(1962-),男, 教授, 博士生导师,主要从事矿物学、岩石学和矿床学方面的研究, E-mail:zhengchangqing@jlu.edu.cn E-mail:zhengchangqing@jlu.edu.cn
作者简介:石磊(1991-),男,硕士,主要从事变质岩石学方面的研究,E-mail:shilei16@mails.jlu.edu.cn
基金资助:
国家自然科学基金项目（41472164，41872192）；中国地质调查局地质调查项目（121201102000150020-06）

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

Shi Lei^1,2, Zhou Xiwen³, Zheng Changqing^1,2, Dong Yunfeng^1,2, Zhou Xiao^1,2, Guo Tengda^1,2

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)

摘要/Abstract

摘要： 浙西南遂昌-大柘地区八都岩群在印支期变质事件影响下发生变质变形，通过详细野外调查和岩相学研究，可将其划分为3期变质变形序列：S₁变形期，NW向片麻理记录的残留紧闭褶皱，共生矿物组合为石榴子石变斑晶及其内部定向分布的包裹体矿物，石榴子石+黑云母+石英（泥质）和石榴子石+角闪石+斜长石+石英（长英质）；S₂变形期，区域性宽缓褶皱及NE向缓倾透入性片麻理，共生矿物组合为石榴子石变斑晶及定向分布的基质矿物，矽线石+石榴子石+黑云母+石英+斜长石±钾长石（泥质）和石榴子石+钾长石+斜长石+黑云母+石英（长英质）；S₃变形期，NE向陡倾透入性片麻理及韧脆性断裂大部分被花岗斑岩脉填充，共生矿物组合为石榴子石变斑晶及其周围退变矿物，石榴子石+矽线石+堇青石+斜长石+黑云母+石英±钾长石（泥质）和角闪石+斜长石+黑云母+钛铁矿（长英质）。结合前人研究成果，八都岩群印支期变质事件峰期变质程度达到麻粒岩相，显示顺时针近等温降压（ITD）型的p-T演化轨迹，S₁-S₃变质变形反映出从俯冲碰撞到快速折返冷却的演化过程，伴随S₃同期侵位的花岗斑岩锆石U-Pb定年结果，将该演化过程完成时间约束在229.7 Ma，可能是浙西南地区对印支期古特提斯洋域内印支-华南-华北板块之间俯冲-碰撞过程的响应。

关键词: 八都岩群, 变质变形序列, 共生矿物组合, 锆石U-Pb定年, 浙西南

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

中图分类号:

P588.34

石磊, 周喜文, 郑常青, 董云峰, 周枭, 郭腾达. 浙西南遂昌—大柘地区八都岩群印支期变质变形序列[J]. 吉林大学学报(地球科学版), 2019, 49(6): 1658-1671.

Shi Lei, Zhou Xiwen, Zheng Changqing, Dong Yunfeng, Zhou Xiao, Guo Tengda. Indosinian Metamorphic Deformation Sequence of Badu Group in Suichang-Dazhe Region,Southwestern Zhejiang[J]. Journal of Jilin University(Earth Science Edition), 2019, 49(6): 1658-1671.

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浙西南遂昌—大柘地区八都岩群印支期变质变形序列

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

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