Skip to Main Content
Skip Nav Destination

Continental crust subjected to horizontal contraction in convergent settings deforms in a variety of styles. In many instances, it is useful to consider the deforming crustal sections in terms of crystalline basement rocks underlying incipiently undeformed sedimentary strata. Three deformation styles are commonly found in such settings. The structural style referred to as thin-skinned tectonics encompasses a stack of thrust sheets composed of non- or weakly metamorphic sedimentary rocks. The associated thrust faults usually level off in a mechanically weak décollement horizon along which a substantial amount of displacement occurs in the course of the formation of the fold-and-thrust belt....

You do not have access to this content, please speak to your institutional administrator if you feel you should have access.

Figures & Tables

Contents

References

Related

Citing Books via

Related Articles
Related Book Content
Close Modal

or Create an Account

Close Modal
Close Modal