Incorporation of incomplete fault-slip data into stress tensor inversion

被引:21
作者
Sato, Katsushi [1 ]
机构
[1] Kyoto Univ, Grad Sch Sci, Div Earth & Planetary Sci, Kyoto 6068502, Japan
关键词
fault-slip analysis; stress tensor inversion; incomplete data; sigma-space;
D O I
10.1016/j.tecto.2006.05.004
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
A fault-slip datum used in the stress tensor inversion techniques is composed of fault orientation, slip orientation and the sense of slip. Sometimes the latter two items are not available. This paper proposes a method to deal with such incomplete fault-slip data. Firstly, the constraints on stress state from full and incomplete data are theoretically specified. The admissible stresses are expressed by the probability distributions in the parameter space. The objective function of inversion is given by superposing the probability distributions for all data including full and incomplete ones. Finally, the peaks of the objective function are detected to enumerate possible solutions. The validity of the present method is tested by simulated data. The incorporation of incomplete data can enhance the detectability of stress states and expands the applicability of stress tensor inversion. (c) 2006 Elsevier B.V. All rights reserved.
引用
收藏
页码:319 / 330
页数:12
相关论文
共 20 条
[1]  
Anderson E.M., 1951, DYNAMICS FAULTING
[2]   TECTONIC ANALYSIS OF FAULT SLIP DATA SETS [J].
ANGELIER, J .
JOURNAL OF GEOPHYSICAL RESEARCH, 1984, 89 (NB7) :5835-5848
[3]  
Angelier J., 1994, Continental Deformation, P53, DOI DOI 10.1017/S001675680001160
[4]  
[Anonymous], TECTONOPHYSICS
[5]  
Bott M., 1959, Geological Magazine, V96, P109, DOI DOI 10.1017/S0016756800059987
[6]   Stress space: striated faults, deformation twins, and their constraints on paleostress [J].
Fry, N .
JOURNAL OF STRUCTURAL GEOLOGY, 2001, 23 (01) :1-9
[7]   Striated faults: visual appreciation of their constraint on possible paleostress tensors [J].
Fry, N .
JOURNAL OF STRUCTURAL GEOLOGY, 1999, 21 (01) :7-21
[8]   Determination of slip sense along a fault in an unlithified sediment [J].
Hirono, T .
JOURNAL OF STRUCTURAL GEOLOGY, 2000, 22 (05) :537-541
[9]  
Kaymakçi N, 2000, GEOL SOC SPEC PUBL, V173, P295, DOI 10.1144/GSL.SP.2000.173.01.15
[10]   A stress inversion method requiring only fault slip sense [J].
Lisle, R ;
Orife, T ;
Arlegui, L .
JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH, 2001, 106 (B2) :2281-2289