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首页> 外文期刊>Chinese science bulletin >The discovery of eclogite dikes in low-greenschist fades volcaniclastic rocks of the Dabie Mountains
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The discovery of eclogite dikes in low-greenschist fades volcaniclastic rocks of the Dabie Mountains

机译:低绿片岩中榴辉岩堤的发现使大别山的火山碎屑岩褪色

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摘要

ECLOGITE occurs in different metamorphic rocks in the Dabie Mountains. Some dike-like eclogite and garnet amphibolite were discovered when we investigated the newly founded low-greenschist facies volcaniclastic rocks in Changpu, Yuexi County and Siqian, Taihu County ( fig. 1). Coesite and quartz pseudomorphs exist in garnet and omphacite. By studying the occurrence and petrography-mineralogy characteristic, we believe that the eclogite is of igneous origin rather than tectonic melange or metamorphicorigin. The discovery is of geological significance for study of eclogitic origin, formation and ages.
机译:ECLOGITE发生在大别山的不同变质岩中。当我们在岳西县昌浦和太湖县四千新建的低绿片岩相火山碎屑岩中发现了一些类似堤防的榴辉岩和石榴石角闪石(图1)。石榴石和绿辉石中存在柯石英和石英假晶。通过研究其发生和岩石学-矿物学特征,我们认为该榴辉岩是火成岩而不是构造混杂岩或变质三聚体。该发现对于研究鳞状岩的成因,形成和年龄具有地质意义。

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