| 流体底辟构造及其成因探讨 |
| |
| 引用本文： | 张树林,黄耀琴,黄雄伟.流体底辟构造及其成因探讨[J].地质科技情报,1999,18(2):19-22. |
| |
| 作者姓名： | 张树林 黄耀琴 黄雄伟 |
| |
| 作者单位： | 中国地质大学资源学院,武汉,430074 |
| |
| 摘 要： | 以莺歌海和渤海盆地为例，总结了新的构造类型－流体底辟构造的特点；根据流体底辟破碎带中泥质混入程度，将它分为断裂破裂带、混杂破裂带、混合岩带和泥火山４种类型；并在综合分析国内外流力破裂研究成果的基础上，论述了流体底辟形成的和地质背景。
|
| 关 键 词： | 流力破裂 流体底辟 底辟构造 断裂 流体运移 |
FLUID DIAPIR STRUCTURE AND ITS GENESES |
| |
| Zhang Shulin,Huang Yaoqin,Huang Xiongwei.FLUID DIAPIR STRUCTURE AND ITS GENESES[J].Geological Science and Technology Information,1999,18(2):19-22. |
| |
| Authors: | Zhang Shulin Huang Yaoqin Huang Xiongwei |
| |
| Abstract: | The features and types of a new structure fluid diapir structure are discussed in this paper,taking those in Yinggehai and Bohai Bay basins as examples.According to mixed ratio of mudrock,fluid diapir structure can be divided into four types:fracture zone,chaotic fracture zone,mixed sandstone mudrock zone (or mudlump) and mud volcano.Besides,the mechanism and geologic setting of fluid diapir are analyzed,on the basis of the theory of fluid fracturing. |
| |
| Keywords: | fluid fracturing fluid diapir diapir structure fault fluid migration |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
|
