摘要
】通过对菖蒲地区１∶１００００区域地质调查，基本查明了大别山超高压变质带的岩石组成、产出状态及分布规律。探讨了榴辉岩形成的多样性，指出碧溪岭榴辉岩体的“Ｓ型”构造形态，并确定了港河浅变质火山碎屑岩系的层序。
This paper,based on the 1:10000 scale regional geological survey in Changpu that has basically disclosed the composition, occurrences and distribution law of the ultra-high pressure metamorphic rocks in the Dabie Mt s deals with the diversification of the formation of eclogite, the s-type strucrure of eclogite 'bodies' in Bixiling and the stratigraphic order of epimetamorphic pyroclastic rock series in Ganghe
出处
《安徽地质》
1998年第1期19-27,共9页
Geology of Anhui
关键词
超高压变质带
榴辉岩
浅变质岩系
构造变形
岳西菖蒲地区
ultra-high pressure metamorphic rock, eclpgote, epimetamorphic rock series,structural deformation,Changpu
