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《地球科学与环境学报》[ISSN:1672-6561/CN:61-1423/P]

卷:

第41卷

期数:

2019年第04期

页码:

379-395

栏目:

基础地质与矿产地质

出版日期:

2019-07-15

文章信息/Info

Title:

Metamorphism of Rocks in Shiyan-Wudang Area of South Qinling Tectonic Belt, China

文章编号:

1672-6561(2019)04-0379-17

作者:

王东升; 王宗起^*; 王刚; 武昱东; 杨皓

(中国地质科学院矿产资源研究所 自然资源部成矿作用与资源评价重点实验室,北京 100037)

Author(s):

WANG Dong-sheng;  WANG Zong-qi^*;  WANG Gang;  WU Yu-dong;  YANG Hao

(MNR Key Laboratory of Metallogeny and Mineral Assessment, Institute of Mineral Resources, Chinese Academy of Geological Sciences, Beijing 100037, China)

关键词:

变质作用;  印支期;  片岩;  绿片岩相;  中低级变质岩;  俯冲-增生;  十堰—武当地区;  南秦岭

Keywords:

metamorphism;  Indosinian;  schist;  greenschist facies;  middle- and low-grade metamorphic rocks;  subduction-accretion;  Shiyan-Wudang area;  South Qinling

分类号:

P588.34

DOI:

-

文献标志码:

A

摘要:

十堰—武当地区位于南秦岭构造带和扬子板块的结合部位,内部发育的变质岩可为秦岭造山带印支期造山过程提供重要信息。在该地区含石榴子石片岩的岩石学、矿物学研究基础上,利用石榴子石-黑云母地质温度计和石榴子石-白云母地质温度计计算变质作用条件。结果表明:石榴子石-黑云母地质温度计计算得到方滩—王家山剖面南、北两侧变质岩的主期变质温度分别为344 ℃～410 ℃和368 ℃～431 ℃,属于低绿片岩相; 由石榴子石-白云母地质温度计计算得到十堰—大木剖面南、北两侧变质岩主期变质温度分别为322 ℃～440 ℃和535 ℃～540 ℃,属于低—高绿片岩相。结合区域变质变形研究成果,认为十堰—武当地区中低级变质岩的变质作用演化与南秦岭构造带印支期洋盆闭合伴生的俯冲-增生过程有关,它使得不同变质级别的岩石发生并置然后一起抬升。

Abstract:

Shiyan-Wudang area is located at the junction of South Qinling tectonic belt and Yangtze plate. Its metamorphism can provide important information for Indosinian orogenic process of Qinling orogenic belt. Based on the study of petrology and mineralogy of garnet-bearing schist in Shiyan-Wudang area, the metamorphic conditions were calculated by using garnet-biotite geothermometer and garnet-muscovite geothermometer. The results show that main metamorphism temperatures of metamorphic rocks from south and north parts of Fangtan-Wangjiashan section calculated by garnet-biotite geothermometer are 344 ℃-410 ℃ and 368 ℃-431 ℃, which are in agreement with lower greenschist facies; meanwhile, main metamorphism temperatures of metamorphic rocks from south and north parts of Shiyan-Damu section calculated by garnet-muscovite geothermometer are 322 ℃-440 ℃ and 535 ℃-540 ℃, agreeing with lower to higher greenschist facies condition. Combining with regional metamorphism and deformation data, it is suggested that metamorphic evolution of middle- and low-grade metamorphic rocks in Shiyan-Wudang area is related to the subduction-accretion process caused by the closure of ocean in South Qinling tectonic belt during Indosinian, which juxtaposes different grades of metamorphic rocks and makes them uplift together.

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备注/Memo

备注/Memo:

收稿日期:2019-03-04; 修回日期:2019-05-20投稿网址:http://jese.chd.edu.cn/
基金项目:国家重点研发计划项目(2016YFC0600202); 国家自然科学基金项目(41702213,41702076); 中国地质科学院基本科研业务费专项资金项目(K1614)
作者简介:王东升(1988-),男,河南濮阳人,助理研究员,理学博士,E-mail:wangdsyzy@126.com。
*通讯作者:王宗起(1960-),男,天津市人,研究员,博士研究生导师,理学博士,E-mail:wzq@ccsd.org.cn。

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