ON THE DETECTION OF WEAK STRAIN PARALLEL TO THE BEDDING BY MAGNETIC-ANISOTROPY - A MATHEMATICAL-MODEL STUDY

被引：13

作者：

HROUDA, F

HRUSKOVA, L

机构：

[1] Geofyzika, N. C., Company Research Institute, Brno

来源：

STUDIA GEOPHYSICA ET GEODAETICA | 1990年 / 34卷 / 04期

关键词：

D O I：

10.1007/BF02316953

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：

Five mathematical models of the superposition of deformational magnetic fabric on sedimentary magnetic fabric are presented. These models are represented by various combinations of pure shear and simple shear. The diagrams of the variations in the main magnetic anisotropy parameters with strain can help in recognizing weak ductile deformation in sedimentary rocks. © 1990 Academia, Publishing House of the Czechoslovak Academy of Sciences.

引用

页码：327 / 341

页数：15

共 16 条

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[7] Ramberg H., Superposition of homogeneous strain and progressive deformation in rocks, Bull. Geol. Inst. Univ. Uppsala, 6, (1975)
[8] Sanderson D.J., Models of strain variation in nappes and thrust sheets: a review, Tectonophysics, 88, (1982)
[9] Elliott D., Determination of finite strain and initial shape from deformed elliptical objects, Geol. Soc. Amer. Bull., 81, (1970)
[10] Owens W.H., Strain modification of angular density distributions, Tectonophysics, 16, (1973)

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