摘要
武功山岩浆热穹窿伸展滑覆构造是在加里东期褶皱基底上发育而成,其构造形迹在时空组合结构上规律有序,具垂向分层、横向分带的特点,是华南地区典型的岩浆热穹窿伸展滑覆构造。
The extensional gliding nappe structure of Wugongshan magmatic thermal dome was developed from a Calidonian folded basement.With its perfect structural features arranged regularly in space and time,dis-playing a layering pattern in cross section and a zoning form in plan view,it is a typical extensional gliding nappe structure of magmatic thermal dome in the South China area.
出处
《江西地质》
2001年第3期161-165,共5页
Jiangxi Geology
