P-T-t evolution of pelitic gneiss from the basement underlying the Northwestern Ordos Basin, North China Craton, and the tectonic implications
© 2016 Elsevier B.V.. Using petrography, phase equilibria modeling and in situ (U-Th)-Pb monazite geochronology, we show that pelitic gneiss from close to the bottom of the Qitan1 borehole in the northwest of the Ordos Basin records a four stage metamorphic evolution. The M1-M3 stages, which were su...
Main Authors: | , , , , , |
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Format: | Journal Article |
Published: |
Elsevier BV
2016
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Online Access: | http://hdl.handle.net/20.500.11937/46713 |