Detrital zircon (U–Th)/He thermochronometry of the Mesozoic Daba Shan Foreland Basin, central China: Evidence for timing of post-orogenic denudation

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Detrital zircon (U–Th)/He thermochronometry of the Mesozoic Daba Shan Foreland Basin, central China: Evidence for timing of post-orogenic denudation

The timing of the transition of a peripheral foreland basin from underfilled to overfilled provides important insights into the post-orogenic dynamics of its coupled orogenic wedge. Such information is lacking in the Mesozoic foreland basins surrounding the Qinling Orogen, central China, such as the...

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Bibliographic Details
Main Authors:	Tian, Y., Qiu, N., Kohn, B., Zhu, C., Hu, S., Gleadow, A., McInnes, Brent
Format:	Journal Article
Published:	Elsevier Science BV 2012
Online Access:	http://hdl.handle.net/20.500.11937/39892

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