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1)  diapir [英]['daɪə,pɪə]  [美]['daɪə,pɪr]
泥底辟
1.
For the exploration of gas hydrates,it is of great significance to study such geological structures as mud diapir and mud volcano.
在天然气水合物勘探中,海底的泥底辟和泥火山构造是重要的研究对象。
2)  Mud Diapir
泥底辟
1.
Based on the seismic data,the salt and mud diapirs in the offshore Bohai Bay Basin are analyzed,and the result shows that the salt and mud diapirs have various geometries and formation mechanisms,and have also exerted important influences on hydrocarbon accumulation.
渤海地区主要发育盐底辟和泥底辟,根据地震资料解释成果,对渤海地区的底辟构造及其伴生构造的几何形态特征与形成机制进行了分析,同时探讨了底辟构造与油气聚集成藏的关系。
3)  mud diapir belt
泥底辟带
1.
Both shallow and deep gas plays are present in the mud diapir belt.
莺歌海盆地泥底辟带存在浅层和中深层2套含气组合。
4)  mud diapiric type
泥底辟类型
5)  mud diapir structure
泥底辟构造
1.
According to the analysis of seismic profile and bathymetry,some mud volcanoes or mud diapir structures were found in the west slope of the south Okinawa Trough.
根据所获得的高分辨率地震资料分析,发现冲绳海槽南部西侧槽坡附近以及海槽内部发育有一系列泥火山(底辟)构造,在地形上表现为泥火山地貌,在穿过泥火山的地震剖面上,表现出典型的泥底辟构造。
2.
Mud diapir structures in Yingehai Basin, South Chia Sea provided better channels for gas migration, so that gas at 3000-6000m depth were migrated to <3000m shallow reservoirs throught mud diapir structures and traped in favourable structures.
莺歌海盆地泥底辟构造为天然气运移提供了良好通道,3000~6000m深处的天然气通过泥底辟构造运移到浅部,并在有利构造部位成藏。
3.
The mud diapir structure in Yinggehai Basin,South Chian Sea,was been formed and evoluted mainly by thermodynamic actions.
莺歌海盆地泥底辟构造主要是在热动力作用下形成和演化的,包括热传导和热对流作用。
6)  mud-fluid diapir
泥-流体底辟
补充资料:泥底
【泥底】
 (界名)与泥梨同。
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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