COMPRESSIONAL UPLIFT IN THE CENTRAL CALIFORNIA COAST RANGES

被引：0

作者：

MONTGOMERY, DR ^{[1
]}

机构：

[1] UNIV WASHINGTON, QUATERNARY RES CTR, SEATTLE, WA 98195 USA

来源：

GEOLOGY | 1993年 / 21卷 / 06期

关键词：

D O I：

10.1130/0091-7613(1993)021<0543:CUITCC>2.3.CO;2

中图分类号：

P5 [地质学];

学科分类号：

0709 ; 081803 ;

摘要：

Controversy over the relative importance of transverse and compressional deformation surrounds continuing debate over uplift in the California Coast Ranges. A simple model for compressional deformation in the central California Coast Ranges predicts a significant part of reconstructed post-3 Ma surface uplift. This result suggests that, in addition to passage of the Mendocino triple junction and fault interactions in a dominantly strike-slip setting, late Cenozoic surface uplift in the California Coast Ranges reflects a small compressive component of deformation across the Pacific-North American plate boundary.

引用

页码：543 / 546

页数：4

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