SHRIMP U-Pb zircon geochronological and geochemical evidence for Neoproterozoic arc-magmatism along the western margin of the Yangtze Block, South China.

SHRIMP U-Pb zircon geochronological and geochemical evidence for Neoproterozoic arc-magmatism along the western margin of the Yangtze Block, South China.

The magmatic and tectonic history of the Yangtze Block and its possible affinity with other Neoproterozoic arc terranes are important in the reconstruction of Neoproterozoic plate tectonics. In the Panxi Belt, adjacent to the eastern margin of the Tibetan Plateau, there are many metamorphic complexe...

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Bibliographic Details
Main Authors: Zhou, M., Yan, D., Kennedy, Allen, Li, Y., Ding, J.
Format: Journal Article
Published: Elsevier Science BV 2002
Subjects:
metamorphic belts
subduction
geochronology
SHRIMP data
Rodinia
South China Block
Neoproterozoic
granite
Online Access:http://hdl.handle.net/20.500.11937/9442

Internet

http://hdl.handle.net/20.500.11937/9442

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