Nittrouer and Hallet Glacial-Marine Sedimentation as a Recorder of Tectonic, Climatic and Sea-Level Dynamics on Active Continental Margins
a) Overview Statement Glacial-marine sedimentation responds to and provides sedimentary archives for a diversity of important processes associated with continental-margin dynamics. Tectonic convergence and subduction on active margins lead to uplift and volcanism that commonly (in temperate and high...
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Language: | English |
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Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.625.4335 http://www.nsf-margins.org/Planning_and_review/White_Papers/Nittrouer_and_Hallet.pdf |