CENOZOIC NORMAL FAULTING AND THE SHALLOW STRUCTURE OF THE RIO-GRANDE RIFT NEAR SOCORRO, NEW-MEXICO

被引：0

作者：

CAPE, CD ^{[1
]}

MCGEARY, S ^{[1
]}

THOMPSON, GA ^{[1
]}

机构：

[1] STANFORD UNIV,DEPT GEOPHYS,STANFORD,CA 94305

来源：

GEOLOGICAL SOCIETY OF AMERICA BULLETIN | 1983年 / 94卷 / 01期

关键词：

D O I：

10.1130/0016-7606(1983)94<3:CNFATS>2.0.CO;2

中图分类号：

P [天文学、地球科学];

学科分类号：

07 ;

摘要：

引用

页码：3 / 14

页数：12

共 50 条

[1] SHALLOW VELOCITY MODEL OF THE RIO-GRANDE RIFT NEAR SOCORRO, NEW-MEXICO
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[2] SHALLOW VELOCITY STRUCTURE OF THE RIO-GRANDE RIFT NORTH OF SOCORRO, NEW-MEXICO - A REINTERPRETATION
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[8] UPPER CRUSTAL STRUCTURE OF THE RIO-GRANDE RIFT NEAR SOCORRO, NEW-MEXICO, FROM INVERSION OF MICRO-EARTHQUAKE S-WAVE REFLECTIONS
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[9] LATE OLIGOCENE AND MIOCENE FAULTING AND SEDIMENTATION, AND EVOLUTION OF THE SOUTHERN RIO-GRANDE RIFT, NEW-MEXICO, USA
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[10] SEISMIC REFRACTION STUDY OF CRUSTAL STRUCTURE IN CENTRAL RIO-GRANDE RIFT, NEW-MEXICO
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