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安徽太湖、宿松一带白片岩的发现及其地质意义

THE DISCOVERY OF WHITESCHIST IN THE TAIHU-SUSONG AREA, ANHUI, AND ITS GEOLOGICAL SIGNIFICANCE

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【作者】 荆延仁张良田毕治国张树业乔兰勇梁万通

【Author】 Jing Yanren, Zhang Liangtian, Bi Zhiguo, Zhang Shuye, Qiao Lanyong snd Liang Wantong

【机构】 安徽区调队安徽区调队长春地质学院

【摘要】 笔者等在宿松、太湖一带首次发现了具有蓝晶石—滑石组合的白片岩。并对其岩性特征及地质意义进行了叙述。

【Abstract】 Early in the 1970’s schist made up of an association of tale+kyanite was named whiteschist by Schreyer (1973, 1974, 1977), who pointed out that the occurrence of whiteschist can be regarded as an indicator of high-pressure metamorphism. At present, whiteschist has been discovered only in a few areas of Asia and Africa, whereas in China there has been no report about its discovery. Recently the authors have found it during their work in the Taihu-Susong area, Anhui. Whiteschist is considered as one kind of high-pressure metamorphic rocks and a typical sign of intracontinental plate breakup-collision zone This discovery is of inportant significance to the study of the theory of plate tectoincs, mineralogy and petrology and the distribution of mineral resources related to high-pressure metamorphism.

  • 【文献出处】 中国区域地质 ,Regional Geology of China , 编辑部邮箱 ,1991年02期
  • 【被引频次】27
  • 【下载频次】89
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