高孔隙岩石中压实带的产生与演化

IMECH-IR > 力学所知识产出(1956-2008)

	高孔隙岩石中压实带的产生与演化
	鲁晓兵; 王淑云; 王义华; 崔鹏
Source Publication	第八次全国岩石力学与工程学术大会论文集.科学出版社,2008,p.132-135
	2008
Pages	132-135
Conference Name	第八次全国岩石力学与工程学术大会
Conference Date	2008
Conference Place	四川成都
Abstract	最近的现场调查和实验研究表明,薄的平直的纯压实变形区(压实带)会出现于岩石中。由于压实带内孔隙减小而成为水库、蓄水层或油田油气的渗流障碍,压实带有重要的应用价值。对岩石中压实带的产生和演化进行了研究。结果表明,热效应使得压实带扩张,应变硬化效应使压实带缩小。
Language	中文
Document Type	会议论文
Identifier	http://dspace.imech.ac.cn/handle/311007/34638
Collection	力学所知识产出(1956-2008)
Corresponding Author	鲁晓兵
Recommended Citation GB/T 7714	鲁晓兵,王淑云,王义华,等. 高孔隙岩石中压实带的产生与演化[C]第八次全国岩石力学与工程学术大会论文集.科学出版社,2008,p.132-135,2008:132-135.

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