| 鄂州市莲花山地质特征 |
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| 引用本文： | 黄运开,吕新华,周高志,刘永耀,齐定清,刘玉珠.鄂州市莲花山地质特征[J].人天科学研究,1995(5). |
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| 作者姓名： | 黄运开 吕新华 周高志 刘永耀 齐定清 刘玉珠 |
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| 作者单位： | 武汉交通科技大学 副教授
(黄运开，吕新华)，湖北省区域地质矿产调查所 高级工程师
(周高志，刘永耀，齐定清)，中国元极学研究会 副研究员(刘玉珠) |
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| 摘 要： | 莲花山地处淮阳山字型前弧西翼,地壳组成主要是强烈钠长石化的中细粒闪长岩和斑状斜长花岗岩。由一系列断裂、节理(或劈理)组成、以格状构造为特征的现存构造格局显然是新华夏系构造迭加而造成的,力学结构面性质、特征显示它们形成于岩体冷却之后的脆性剪切应力作用。
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| 关 键 词： | 淮阳山字型前弧 新华夏系 闪长岩 斜长花岗岩 钠长石化 |
An analysis of geological structure of Mt. Lotus |
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| Authors: | Huang Yunkai |
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| Institution: | Wuhan Science and Technology University of Communication |
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| Abstract: | Located in the limbs of the forearch of Huaiyang epsilon - type structural system,the Mt. Lotus consisted mainly of medium and fine-grained diorite with intensenly albitization and porphyric plagiogranite. There are series of faults, joints (or cleavage) in it. The existing structural framework, being characterized by chessboard-like structures, was formed with superimposition of Neocathaysian structure. The nature and specialities of the mechanical textural planes indicate that they were formed by brittle shearing after the cooling of rock body. |
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| Keywords: | Forearch of Huaiyang epsilon - type structural system Neocathaysian structure Diorite Plagiogranite Albitization |
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