Cleavage fronts and fans as reflections of orogen stress and kinematics in Taiwan
- 1Department of Geosciences, Penn State University, University Park, Pennsylvania 16802, USA
- 2Department of Earth and Space Sciences, University of Washington, Seattle, Washington 98195, USA
- 3Geosciences Department, National Taiwan University, No. 1, Sec. 4, Roosevelt Road, Taipei 10617, Taiwan
- 4ExxonMobil Exploration Company, P.O. Box 4778, Houston, Texas 77210-4778, USA
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.
-
- Received 17 April 2006.
- Accepted 28 August 2006.
- Revision received 23 August 2006.
- Geological Society of America
