4d Strain Path Recorded In The Lower Crust During The Transition From Convergence To Continental Rifting, Doubtful Sound, Fiordland, New Zealand

4d Strain Path Recorded In The Lower Crust During The Transition From Convergence To Continental Rifting, Doubtful Sound, Fiordland, New Zealand

ABSTRACT Doubtful Sound, in SW New Zealand, exposes an exhumed section of lower crust that represents the root of an Early Cretaceous magmatic arc. Here, the lower crust underwent a change from contraction to extension and these tectonic cycles are fundamental to the growth of continental crust. Maf...

Full description

Bibliographic Details
Main Author: Ingram, Michael
Format: Others
Language:en
Published: ScholarWorks @ UVM 2017
Subjects:
convergence
Doubtful Sound
extension
lower crust
strain
Geology
Online Access:http://scholarworks.uvm.edu/graddis/683
http://scholarworks.uvm.edu/cgi/viewcontent.cgi?article=1682&context=graddis

Internet

http://scholarworks.uvm.edu/graddis/683
http://scholarworks.uvm.edu/cgi/viewcontent.cgi?article=1682&context=graddis

Similar Items