Formation of segmented normal faults: a 3-D perspective

被引:325
作者
Walsh, JJ
Bailey, WR
Childs, C [1 ]
Nicol, A
Bonson, CG
机构
[1] Univ Coll Dublin, Dept Geol, Fault Anal Grp, Dublin 4, Ireland
[2] Inst Geol & Nucl Sci Ltd, Lower Hutt, New Zealand
[3] CSIRO, Petr, ARRC, Kensington, WA 6151, Australia
关键词
segmented normal fault; fault propagation; fault growth;
D O I
10.1016/S0191-8141(02)00161-X
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
The interpretation of fault kinematics from geometric data is an essential step in developing an understanding of the growth of fault systems. Constraints on fault geometry are, however, often restricted to 2-D maps or cross-sections. In this article we consider the extent to which kinematic interpretations of faulting benefit from a 3-D, rather than 2-D geometrical perspective. Concentrating on relay zones and segmented normal fault arrays, we suggest that very different interpretations of their evolution arise from the recognition that the propagation directions of faults. and fault segments, will rarely be contained within the inspection plane of 2-D data. A 3-D perspective favours an interpretation in which the segments of a fault array are kinematically interrelated from their initiation. Individual segments in such systems may link into a single fault surface out of the plane of inspection or may be unconnected in 3-D. We argue that this interpretation, which conflicts with the often suggested model of incidental overlap of originally isolated faults, should be the preferred model for the generation and Growth of segmented normal fault arrays. (C) 2002 Published by Elsevier Science Ltd.
引用
收藏
页码:1251 / 1262
页数:12
相关论文
共 64 条
[1]   OVERLAPPING FAULTS, INTRABASIN HIGHS, AND THE GROWTH OF NORMAL FAULTS [J].
ANDERS, MH ;
SCHLISCHE, RW .
JOURNAL OF GEOLOGY, 1994, 102 (02) :165-180
[2]  
[Anonymous], 2001, GEOL S AMER
[3]  
BARNETT JAM, 1987, AAPG BULL, V71, P925
[4]  
Cartwright J.A., 1996, MODERN DEV STRUCTURA, V99, P163, DOI DOI 10.1144/GSL.SP.1996.099.01.13
[5]   FAULT GROWTH BY SEGMENT LINKAGE - AN EXPLANATION FOR SCATTER IN MAXIMUM DISPLACEMENT AND TRACE LENGTH DATA FROM THE CANYONLANDS GRABENS OF SE UTAH [J].
CARTWRIGHT, JA ;
TRUDGILL, BD ;
MANSFIELD, CS .
JOURNAL OF STRUCTURAL GEOLOGY, 1995, 17 (09) :1319-1326
[6]  
Chapman T., 1991, Geol. Soc. Lond. Spec. Publ., V56, P183
[7]   FAULT OVERLAP ZONES WITHIN DEVELOPING NORMAL-FAULT SYSTEMS [J].
CHILDS, C ;
WATTERSON, J ;
WALSH, JJ .
JOURNAL OF THE GEOLOGICAL SOCIETY, 1995, 152 :535-549
[8]   Growth of vertically segmented normal faults [J].
Childs, C ;
Nicol, A ;
Walsh, JJ ;
Watterson, J .
JOURNAL OF STRUCTURAL GEOLOGY, 1996, 18 (12) :1389-1397
[9]   KINEMATIC ANALYSIS OF FAULTS IN A PHYSICAL MODEL OF GROWTH FAULTING ABOVE A VISCOUS SALT ANALOG [J].
CHILDS, C ;
EASTON, SJ ;
VENDEVILLE, BC ;
JACKSON, MPA ;
LIN, ST ;
WALSH, JJ ;
WATTERSON, J .
TECTONOPHYSICS, 1993, 228 (3-4) :313-329
[10]   A model for the structure and development of fault zones [J].
Childs, C ;
Watterson, J ;
Walsh, JJ .
JOURNAL OF THE GEOLOGICAL SOCIETY, 1996, 153 :337-340