Abstract:The Cenozoic evolution of SE Asia is marked by thousands of kilometres extension on the continental margin, including normal faults, half-grabens, and volcanic rocks, but dating of brittle faults in the shallow crust is difficult because of a lack of synkinematic minerals. The Cenozoic extension in the Youjiang fold-thrust belt in southwest China is marked by brittle normal faults and half-grabens filled with Paleogene sediments in the region. Here, we identified a strongly weathered mafic sill that was trunca… Show more
Set email alert for when this publication receives citations?
scite is a Brooklyn-based organization that helps researchers better discover and understand research articles through Smart Citations–citations that display the context of the citation and describe whether the article provides supporting or contrasting evidence. scite is used by students and researchers from around the world and is funded in part by the National Science Foundation and the National Institute on Drug Abuse of the National Institutes of Health.