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...
| Main Authors: | , , , , , , |
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| Format: | Journal Article |
| Published: |
Elsevier Science BV
2012
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| Online Access: | http://hdl.handle.net/20.500.11937/39892 |