Maturing arc signatures monitored by trace element and Hf isotope systematics in the early Cretaceous Zacatecas volcanic field, Mexico
Mesozoic growth of continental crust along the southwestern margin of North America and its southern extension in Mexico has been partly explained by the accretion of terranes. These terranes have been considered to be fragments of exotic, intraoceanic island arcs that approached mainland Mexico after the Early Cretaceous. Trace elements and Lu-Hf isotopic systematics for primitive arc successions of the Zacatecas Volcanic Field indicate a close relationship with parts of the northern Guerrero...[Show more]
|Collections||ANU Research Publications|
|Source:||Journal of Geology|
|01_Escalona-Alcazar_Maturing_arc_signatures_2014.pdf||1.06 MB||Adobe PDF|
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