Both shallow and deep gas plays are present in the mud diapir belt.

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。

Diapir was mainly composed of some salts, and minor soft mudstone or other plaster sediments.

底辟物质由盐岩为主的塑性层组成。

The high geotherm the upper mantle diapir and the corresponding lithosphere thinning regions.

这种高地温线与该区上地幔的底辟上涌和岩石圈的相应减薄有关.

Mud diapir is an important geologic phenomenon related to gas accumulation in Yinggehai Basin.

泥拱是莺歌海盆地的重要地质现象，它与油气聚集有密切关系。

Negative coefficients occur where there is a downward decrease in velocity and density: for example, at the top of an over pressured shale diapir.

只有当速度和密度向下减少时，例如在超压页岩穿刺体的顶部，反射系数才会出现负值。