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京北云蒙山变质核杂岩南东侧剥离断层带的构造热演化
王巧云; 颜丹平; 苏本勋; 周密; 胡瑞忠
2006
Source Publication地质通报
Volume25Issue:4Pages:448-453
metadata_24其它
Abstract以云蒙山变质核杂岩东侧的河防口低角度正断层为研究对象,通过矿物(黑云母)的变形特征和形成环境分析,获得了该断层带上的构造热演化环境:温度为780~860℃,压力约为7.3×10^8-8.6×10^8pa。提出云蒙山变质核杂岩的成因机制是,在区域伸展背景下,处于半固结状态的云蒙山花岗岩在东南侧卷入河防口-水峪伸展型韧性剪切带,使花岗岩发生中高温条件的韧性变形;之后,该韧性剪切带在隆升过程中不断向浅层次过渡,形成了一些浅层次的脆性伸展变形构造。
Keyword云蒙山变质核杂岩
Subject Area中国典型特殊区带大规模成矿作用及其动力学
Funding Organization国家自然科学基金重点项目(编号40434011)、国家自然科学基金项目(编号40472106)资助.
Indexed ByCSCD
Language中文
CSCD IDCSCD:2358021
Citation statistics
Cited Times:9[CSCD]   [CSCD Record]
Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/406
Collection矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
矿床地球化学国家重点实验室
Corresponding Author胡瑞忠
Recommended Citation
GB/T 7714
王巧云,颜丹平,苏本勋,等. 京北云蒙山变质核杂岩南东侧剥离断层带的构造热演化[J]. 地质通报,2006,25(4):448-453.
APA 王巧云,颜丹平,苏本勋,周密,&胡瑞忠.(2006).京北云蒙山变质核杂岩南东侧剥离断层带的构造热演化.地质通报,25(4),448-453.
MLA 王巧云,et al."京北云蒙山变质核杂岩南东侧剥离断层带的构造热演化".地质通报 25.4(2006):448-453.
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