| 准确鉴别武当山群面理及其意义 |
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| 引用本文： | 罗洪. 准确鉴别武当山群面理及其意义[J]. 资源环境与工程, 1995, 0(2) |
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| 作者姓名： | 罗洪 |
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| 作者单位： | 湖北省鄂西北地质矿产调查所 |
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| 摘 要： | 求文以１：５万凉水河镇幅、浪河镇幅区调资料为基础，阐述了武当山群的原生层理（Ｓｏ）、板劈理（Ｓ１Ｂ）、分异层理（Ｓ２Ｃ）和折劈理（Ｓ３Ｚ）等面理的宏观及微观特征，探讨了其成生及演化关系，意义在于：客观地进行地质境图，合理地划分线状的强应变带与弱应变城，以揭示武当山群的变形变质及演化史。
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| 关 键 词： | 武当山群，面理，强应变带，弱应变域，变形，演化史 |
THE IDENTIFICATION OF FOLIATION IN WUDANG GROUP AND ITS IMPLICATION |
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| Luo Hong. THE IDENTIFICATION OF FOLIATION IN WUDANG GROUP AND ITS IMPLICATION[J]. Resources Environment & Engineering, 1995, 0(2) |
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| Authors: | Luo Hong |
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| Abstract: | Based on 1: 5000 scale's mapping of Liangshuihe Town, the author discusses the macroscopic and microscopic characteristics, geneses and the relations each other of different types of folliations such as primary beddings (S0), slaty cleavages (S1B), segregation beddings and crenulation cleavages (S32) in Wudang Gr. It is helpful for our mapping objectively,dineating reasonablly the linear strong strain zone and weak strain domain, and revealing thd deformational and metamorphic history of Wudang Gr. |
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| Keywords: | Wudang Gr. foliation strong strain zone weak strain domain deformation evolution |
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