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1)  fluid diapir
流体底辟
1.
The features and types of a new structure fluid diapir structure are discussed in this paper,taking those in Yinggehai and Bohai Bay basins as examples.
以莺歌海和渤海湾盆地为例,总结了一种新的构造类型——流体底辟构造的特点;根据流体底辟破碎带中泥质混入程度,将它分为断裂破裂带、混杂破裂带、混合岩带和泥火山4种类型;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
2)  heat flow diapris
热流底辟体
1.
Through the channel way of the connnection of the base of Xujiaweizi linked system of faults with partial chamber,the carbonate dioxide gas in the mantle\|derived heat flow diapris move up into appropriate volcanic rock encirclement along the faults, and form gas pool.
对芳深 9、芳深 7、芳深 6井的天然气组成及甲烷同位素分析表明 ,松辽盆地北部昌德CO2 气为幔源无机气 ,该CO2 气是以由徐家围子连锁断层系下延与局部岩浆房相接作为通道 ,幔源热流底辟体中的CO2 气顺断层上移至合适的火山岩圈闭中而成藏
3)  mud-fluid diapir
泥-流体底辟
4)  heat flow in the diapir belt
泥底辟热流体
1.
The high geotemperature and superpressure system is mainly located in the diapir belt of the Yinggehai depression in the middle of the basin,so the intrusion of heat flow in the diapir belt, especially the movement of heat fluids of the late Pliocene and the distribution of abnormal high geotemperature and superpressure contro.
莺歌海盆地属南海北部被动大陆边缘新生代异常高温高压盆地,其异常高温高压地层系统主要展布于盆地中部莺歌海坳陷区泥底辟构造带,因此,泥底辟热流体上侵活动,尤其是上新世后期的热流体活动与异常高压区带的展布,控制了天然气及CO2的运聚富集特征。
5)  diapir of asthenosphere
软流圈底辟体
6)  diapris
底辟体
补充资料:贤辟
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