| 湖北房县青峰断裂带的变形与变质作用研究 |
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| 引用本文： | 李树钧,王国芝. 湖北房县青峰断裂带的变形与变质作用研究[J]. 成都理工大学学报(自然科学版), 1993, 0(4) |
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| 作者姓名： | 李树钧 王国芝 |
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| 作者单位： | 成都理工学院地质学系(李树钧)，成都理工学院地质学系(王国芝) |
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| 摘 要： | 在武当山地区的青峰断裂带上,由推覆构造引起了岩石的多期变形,并发现有与之相应的共生矿物组合。据此,绘制了以温度和压力为变量的施莱纳玛克斯束图解,进而推测了在多期变质作用过程中的温、压变化。
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| 关 键 词： | 多期变形 共生矿物组合 施莱纳玛克斯束 |
A RESEARCH ON DEFORMATION AND METAMORPHISM OF QINGFENG FAULT ZONE IN FANG COUNTY, HUBEI PROVINCE |
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| Li Shujun Wang Guozhi. A RESEARCH ON DEFORMATION AND METAMORPHISM OF QINGFENG FAULT ZONE IN FANG COUNTY, HUBEI PROVINCE[J]. Journal of Chengdu University of Technology: Sci & Technol Ed, 1993, 0(4) |
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| Authors: | Li Shujun Wang Guozhi |
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| Affiliation: | Li Shujun Wang Guozhi |
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| Abstract: | In the Qingfeng fault zone of Mt. Wudang area,the polydeformation of roks was caused by nappe movement,and the paragenetic mineral assemblages corresponding to the polydeformation could be found. According to this,the diagram of Schreinmakers bundle in which temperature and pressure are regarded as two forcible variants, can be drawn. Therefore, we can suppose the changes of temperature and pressure during the process of the polymetamorphism. |
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| Keywords: | polydeformation paragenetic mineral assemblage Schreinmakers bundle |
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