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现代地质 ›› 2004, Vol. 18 ›› Issue (2): 229-236.

• 岩石 • 上一篇    下一篇

湘东北文家市蛇绿混杂岩带的发现及意义

贾宝华1,2. 彭和求2,3. 唐晓珊2. 何江南2. 郭乐群2.   

  1. 1.中国地质大学“岩石圈构造、深部过程及探测技术”教育部重点实验室,北京100083;2 湖南地质调查研究院,湖南 湘潭 411100;3中国地质大学地球科学学院,湖北武汉 430074
  • 出版日期:2004-02-20 发布日期:2004-02-20

DISCOVERY OF THE WENJIASHI OPHIOLITIC MELANGE BELT IN NORTHEASTERN HUNAN AND ITS IMPLICATIONS

JIA Bao-hua1,2,PENG He-qiu2,3,TANG xiao-shan2,HE Jiang-nan2,Guo Le-qun2   

  1. 1 China University of Geosciences, Beijing 10083,China;2 Hunan Institute of Geological Survey, Xiangtan, Hunan  411100;3 China University of Geosciences, Wuhan, Hubei  430074, China

  • Online:2004-02-20 Published:2004-02-20

摘要:

在湘东北文家市首次识别出蛇绿岩套残片,它由变沉积岩、变玄武岩、变辉绿岩、变辉长岩、变辉石岩类及变硅质岩组成。综台其地质学、岩石学、地球化学和同位素年代学的资料,提出文家市蛇绿岩可能形成于有限小洋盆的构造环境。文家市蛇绿混杂岩带、前陆盆地、磨拉石建造和"s"型花岗岩等构造岩石组合记录了碰撞造山的全过程,证实了江南雪峰古陆属元古宙造山带。这一发现为华南前寒武纪的大地构造格架和地壳演化提供了依据.同时该地区也将成为研究早期华南大陆地壳演化——武陵运动的关键地带。

关键词: 湘东北, 文家市, 蛇绿岩套, 江南雪峰古陆, 武陵运动

Abstract:

This is the first report on the ophiolite suite,which consists of metasediment,meta-basalt,metadiabase,metagabbro,metapyroxene and metasilicith,in the Wenjiashi area, northeastern Hunan.Based on geology,petrology,geochemistry and isotope chronologic data issued in this work,it is suggested that the Wenjiashi ophiolite be developed under the tectonic setting of a restricted small ocean basin.Tectono -rock assemblages such as ophiolite melange belt,foreland basin,molasse formation and“S—type”granitoid recorded the whole process of collisinal orogenesis of Wuling epoch and confirm that the
Jiangnan—Xuefeng Block should belong to Protemzoic orogens.The discovery of the ophiolitic melange belt in the Wenjiashi area provides information about the Precambrian geotectonic framework and crust evolution of South China,and therefore,this area would become one of key areas to study the early evolution(the Wuling Movement)of South China continental crust.

Key words: northeastern Hunan, Wenjiashi, ophiolite suite, the Jiangnan-Xuefeng Block, the Wuling Movement

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