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...
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| Format: | Others |
| Language: | en |
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ScholarWorks @ UVM
2017
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| Online Access: | http://scholarworks.uvm.edu/graddis/683 http://scholarworks.uvm.edu/cgi/viewcontent.cgi?article=1682&context=graddis |