Metamorphic P–T path and tectonic implications of pelitic granulites from the Daqingshan Complex of the Khondalite Belt, North China Craton.

Highlights: [•] Four metamorphic stages have been identified within the Daqingshan pelitic granulites. [•] Phase equilibria modeling has constrained a clockwise P–T path. [•] The Daqingshan Complex was involved in collisional orogen between the Yinshan and the Ordos Blocks. [Copyright &y& Elsevier]