李曙光, 刘德良, 陈移之, 葛宁洁, 张宗清, 叶笑江
Abstract
A large eclogite belt developed along the Dabie Mountains and Subei-Jiaonan Rise in central China is a result of collision between the North China and Yangtze blocks. Recently, coesite and coesite pseudomorphs are recognized as an inclusion in both garnet and
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A large eclogite belt developed along the Dabie Mountains and Subei-Jiaonan Rise in central China is a result of collision between the North China and Yangtze blocks. Recently, coesite and coesite pseudomorphs are recognized as an inclusion in both garnet and
Key concepts: Coesite, Eclogite, Pseudomorph, Geology, Geochemistry, Seismology, Paleontology, Quartz