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Destruction of the North China Craton in the Mesozoic

Annual Review of Earth and Planetary Sciences, 2019
The North China Craton (NCC) was originally formed by the amalgamation of the eastern and western blocks along an orogenic belt at ∼1.9 Ga. After cratonization, the NCC was essentially stable until the Mesozoic, when intense felsic magmatism and related ...
Jin-Hui Yang, Yi-Gang Xu, Simon A Wilde
exaly   +2 more sources

Mesozoic–Cenozoic geological evolution of the Himalayan-Tibetan orogen and working tectonic hypotheses

American Journal of Science, 2019
The Himalayan-Tibetan orogen culminated during the Cenozoic India – Asia collision, but its geological framework and initial growth were fundamentally the result of multiple, previous ocean closure and intercontinental suturing events.
P. Kapp, P. DeCelles
semanticscholar   +1 more source

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