Exhumation and continental strike-slip fault systems: Introduction

Geological Society of America Special Papers
By: , and 

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Abstract

Metamorphic rocks adjacent to and within strike-slip faultsystems occur in a wide range of tectonic settings. Detailed studies show that for a number of these locales a significant part of the exhumation occurred during strike-slip fault motion, but the specific processes involved are often cryptic. Although some sites share characteristic features, such as metamorphic rocks exhumed in extensional step-overs within overall transtensional systems, no one common theme emerges from all of the studies. Our understanding of the variables that control continental strike-slip faults' interaction with mid- to lower-crustal structures is still primitive.

Publication type Article
Publication Subtype Journal Article
Title Exhumation and continental strike-slip fault systems: Introduction
Series title Geological Society of America Special Papers
DOI 10.1130/978-0-8137-2434-8(2007)434[vii:I]2.0.CO;2
Issue 434
Year Published 2007
Language English
Publisher Geological Society of America
Contributing office(s) Alaska Science Center
Description 4 p.
First page vii
Last page x
Online Only (Y/N) N
Additional Online Files (Y/N) N
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