Kun-Feng Qiu

The Cambrian Magmatic Evolution in the Damara Belt, Namibia: Constraints from Garnet-Bearing Granites

Abstract Garnet is a petrogenetic key indicator, common in igneous and medium- to high-pressure metamorphic rocks. It provides valuable constraints for pressure–temperature–time paths in orogenic belts and offers insight into magma generation, evolution, and crystallization. To i...