Diapir
英音[ ˈdaɪəpɪə(r) ] 美音[ ˈdaɪəˌpɪr ]

[地质] 底辟

常用释义

词性释义

n.

[地质] 底辟;挤入构造
例句
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岩盐造成的蘑菇状或柱塞状的刺穿构造。一般有上覆盖岩。
Besides, the mechanism and geologic setting of fluid diapir are analyzed, on the basis of the theory of fluid fracturing.
并在综合分析国内外流力破裂研究成果的基础上,论述了流体底辟形成的机制和地质背景。
Magmatic Diapir of Fangshan Pluton in the Western Hills, Beijing and Its Geological Significance
北京西山房山岩体岩浆底辟构造及其地质意义
底辟构造与天然气水合物的成矿关系
The thrust faults, folds, strike-slip faults and magmatic diapir structures were formed in the lower layer;
下构造层发育逆冲断层、褶皱、走滑构造和岩浆底辟构造;
The Elementary Research of Gas Hydrate Associated with Mud Diapir Structure in the East China Sea
东海与泥底辟构造有关的天然气水合物初探