RELATIONSHIP BETWEEN INSITU STRAIN RELAXATION AND OUTCROP FRACTURES IN POTSDAM SANDSTONE, ALEXANDRIA BAY, NEW-YORK

被引：27

作者：

ENGELDER, T ^{[1
]}

SBAR, ML ^{[1
]}

机构：

[1] LAMONT DOHERTY GEOL OBSERV,PALISADES,NY 10964

来源：

PURE AND APPLIED GEOPHYSICS | 1977年 / 115卷 / 1-2期

关键词：

D O I：

10.1007/BF01637096

中图分类号：

P3 [地球物理学]; P59 [地球化学];

学科分类号：

0708 ; 070902 ;

摘要：

引用

页码：41 / 55

页数：15

共 18 条

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[3]

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[5] EVIDENCE FOR UNIFORM STRAIN ORIENTATION IN POTSDAM SANDSTONE, NORTHERN NEW-YORK, FROM INSITU MEASUREMENTS [J].

ENGELDER, JT ;

SBAR, ML .

JOURNAL OF GEOPHYSICAL RESEARCH, 1976, 81 (17) :3013-3017

[6] MECHANISM FOR STRAIN RELAXATION OF BARRE GRANITE - OPENING OF MICROFRACTURES [J].

ENGELDER, T ;

SBAR, ML ;

KRANZ, R .

PURE AND APPLIED GEOPHYSICS, 1977, 115 (1-2) :27-40

[7] INFLUENCE OF RESIDUAL ELASTIC STRAIN ON ORIENTATION OF EXPERIMENTAL FRACTURES IN 3 QUARTZOSE SANDSTONES [J].

FRIEDMAN, M ;

LOGAN, JM .

JOURNAL OF GEOPHYSICAL RESEARCH, 1970, 75 (02) :387-+

[8] RESIDUAL ELASTIC STRAIN IN ROCKS [J].

FRIEDMAN, M .

TECTONOPHYSICS, 1972, 15 (04) :297-&

[9]

Herget G., 1974, Rock Mechanics, V6, P53, DOI 10.1007/BF01238053

[10]

LEE FT, 1972, 24TH IGC MONTR, P261

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