Cleavage fronts and fans as reflections of orogen stress and kinematics in Taiwan

Donald M. Fisher, Sean Willet, Yeh En-Chao, M. Brooks Clark

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25 Citations (Scopus)

Abstract

Recent observations of cleavage patterns, strain histories, and kinematics across the Taiwan mountain belt depict systematic orogen-scale variations with respect to the synorogenic divide and suggest that the pattern of cleavage development is a predictable consequence of orogen stresses and kinematics. In Taiwan, continental crust within the collision is accreted in the prowedge facing Asia, but is advected eastward into the east-verging retrowedge, where the most deeply exhumed rocks are exposed. Wedge mechanics predict a reversal in the direction of plunge of the principal compressive stress at the topographic divide between the opposing wedges. The observation of a single cleavage in western Taiwan suggests that the cleavage in the prowedge remains stable with respect to the stress orientation. In contrast, the existence of a second crenulation cleavage in the retrowedge is evidence for an abrupt change in stress orientation and unstable buckling of preexisting prowedge fabrics. Advection of a fabric across a topographic divide in a doubly vergent wedge provides an explanation for the occurrence of cleavage fronts and fans in natural systems such as Taiwan.

Original languageEnglish
Pages (from-to)65-68
Number of pages4
JournalGeology
Volume35
Issue number1
DOIs
Publication statusPublished - 2007 Jan 1

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Keywords

  • Cleavage fan
  • Cleavage front
  • Incremental strain
  • Slaty cleavage
  • Taiwan

ASJC Scopus subject areas

  • Geology

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