REPRINT: Late Cenozoic Structure of the Santa Susana Fault Zone (in Recent Reverse Faulting in the Transverse Ranges, California, USGS Professional Paper 1339, pp. 137-160)

Author(s):  
Robert S. Yeats
1976 ◽  
Vol 66 (6) ◽  
pp. 1931-1952
Author(s):  
Donald J. Stierman ◽  
William L. Ellsworth

abstract The ML 6.0 Point Mugu, California earthquake of February 21, 1973 and its aftershocks occurred within the complex fault system that bounds the southern front of the Transverse Ranges province of southern California. P-wave fault plane solutions for 51 events include reverse, strike slip and normal faulting mechanisms, indicating complex deformation within the 10-km broad fault zone. Hypocenters of 141 aftershocks fail to delineate any single fault plane clearly associated with the main shock rupture. Most aftershocks cluster in a region 5 km in diameter centered 5 km from the main shock hypocenter and well beyond the extent of fault rupture estimated from analysis of body-wave radiation. Strain release within the imbricate fault zone was controlled by slip on preexisting planes of weakness under the influence of a NE-SW compressive stress.


1999 ◽  
Vol 107 (6) ◽  
pp. 727-732 ◽  
Author(s):  
Carl R. Berquist, Jr., ◽  
Christopher M. Bailey

2013 ◽  
Vol 69 ◽  
pp. 11-30 ◽  
Author(s):  
Witold Zuchiewicz ◽  
Nguyễn Quốc Cu’ò’ng ◽  
Jerzy Zasadni ◽  
Nguyễn Trọng Yêm

Author(s):  
Alberto Gomes ◽  
Helder I. Chamin ◽  
Jos Teixeira ◽  
Paulo E. Fonseca ◽  
Lus C. Gama Pereira ◽  
...  

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