Article ID Journal Published Year Pages File Type
6444399 Journal of Asian Earth Sciences 2015 22 Pages PDF
Abstract
In conjunction with regional data within the SCB, it is most likely that the magmatism younger than 435 Ma was generated in a post-collisional extensional regime related to the partial delamination of an overthickened lithospheric mantle root without lower crust.
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Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Geology
Preview
Petrogenesis of the early Paleozoic strongly peraluminous granites in the Western South China Block and its tectonic implications
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