Crustal Architecture Across Southern California and Its Implications on San Andreas Fault Development
被引:2
|
作者:
Sui, Siyuan
论文数: 0引用数: 0
h-index: 0
机构:
SUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USASUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USA
Sui, Siyuan
[1
]
Shen, Weisen
论文数: 0引用数: 0
h-index: 0
机构:
SUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USASUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USA
Shen, Weisen
[1
]
Holt, William
论文数: 0引用数: 0
h-index: 0
机构:
SUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USASUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USA
Holt, William
[1
]
Kim, Jeonghyeop
论文数: 0引用数: 0
h-index: 0
机构:
SUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USA
Univ Washington, Dept Earth & Space Sci, Seattle, WA USASUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USA
Kim, Jeonghyeop
[1
,2
]
机构:
[1] SUNY Stony Brook, Dept Geosci, Stony Brook, NY 11794 USA
[2] Univ Washington, Dept Earth & Space Sci, Seattle, WA USA
In this study, we perform a 2-frequency sequential receiver function stacking investigation in Southern California. The resulting Moho depths exhibit similar patterns to previous studies while the crystalline crustal Vp/Vs values show more regional variations. Most Vp/Vs variations can be explained by compositional differences. We observe a dichotomy in Moho depth, Vp/Vs, and crustal strain rates between the Peninsular Ranges and Southern San Andreas Fault system. Comparisons between strain rates, Vp/Vs, and temperature suggest that crustal compositional variations may have played a more critical role in influencing the crustal strain rate variations in the Peninsular Ranges and Southern San Andreas than temperature. The structural and compositional variations provide a new insight into the causes of the migration of the Southern San Andreas Fault system and the formation of the "Big Bend."