摘要
Ultrahigh-pressure metamorphic (UHPM) rocks in Shuanghe was recognized as a slab emplaced into the lower-pressure (LP) country gneisses, while within the UHPM slab the coesite-bearing eclogites, jadeite quartzite, eclogite-bearing marble are structurally concordant with "in situ" schists and gneisses.
Ultrahigh-pressure metamorphic (UHPM) rocks in Shuanghe was recognized as a slab emplaced into the lower-pressure (LP) country gneisses, while within the UHPM slab the coesite-bearing eclogites, jadeite quartzite, eclogite-bearing marble are structurally concordant with 'in situ' schists and gneisses.
基金
Project supported by the National Natural Science Foundation of China.
