1) salt diapir structure
盐底辟构造作用
2) salt diapirism
盐底辟作用
3) active salt dome
主动底辟盐构造
1.
Influence of rock strength on fault patterns above active salt domes:Insights from 2D discrete element simulations;
用离散元方法讨论岩石强度对主动底辟盐构造断层分布模式的影响
2.
Simulation of active salt domes using 2D discrete element method;
主动底辟盐构造的二维离散元模拟
4) diapir salt structure
底辟盐体构造
5) diapiric structure
底辟构造
1.
The diapiric structures display various types such as a turtleback-like arch, weak piercing, gas-chimney, fault (or crack) and seabed pit, originated in two huge mud-rich strata the Wenchan.
底辟构造包括龟背上拱、弱刺穿、气烟囱、底辟断层(或裂缝)、海底麻坑等类型,主要发源于断陷期深湖相的文昌组(始新统)—恩平组(上始新统-下渐新统),其次为坳陷期浅海-深海相沉积的珠江组(下中新统)—韩江组(中中新统)的两套巨厚富泥沉积层。
2.
Its particularstructural location and sedimentary environment brought various structural styles,including fault blocks, flowery structure, diapiric structure, inversion structure,buried hills and These geological structures occurred respectively in differentgeological ages and locations, forming superposition structures, so that they creat-ed favourable plac.
曾母盆地属周缘前陆盆地，发育于两个不同块体会聚带上，后期又经过走滑体系的作用，其特殊的构造部位和特定的沉积环境，造就了独特、丰富的构造样式，主要有断块构造、花状构造、底辟构造、反转构造、潜山构造等。
3.
The BF is a diapiric structure caused by basement .
依据底辟物质来源的深度，把底辟构造分为深源型和浅源型两大类。
6) diapir structure
底辟构造
1.
The relationships between diapir structure and gas hydrate mineralization;
底辟构造与天然气水合物的成矿关系
2.
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
3.
A fluid diapir model is proposed based on the features of diapir structures and their associated abnormal temperature and pressure data in Yinggehai basin, This paper also further discusses the significance of fluid diapirs to petroleum geology.
在总结莺歌海盆地底辟构造特征及其伴生的温度和压力异常资料的基础上,提出了流体底辟模式,并进一步讨论了流体底辟在石油地质中的意义。
补充资料：底辟构造
| 底辟构造 diapiric structure 密度较小的高塑性低粘度的岩石（如岩盐、石膏或泥岩等）向上流动，拱起甚至刺穿上覆岩层所形成的穹隆或蘑菇状构造。简称底辟。底辟的直径可从几米到几千米。盐丘是最常见的底辟构造，它由盐类岩石或石膏向上流动或挤入而使上覆岩层拱曲隆起所成。核部的盐体常成圆柱状，其内盐层变形复杂。盐核之上的上覆岩层往往形成穹隆或短轴背斜及伴生的放射状或环状断层。盐核周边与围岩常为陡倾的断层接触，围岩倾角也变陡。盐丘周围的岩层因盐丘上隆而相对下坳，形成周缘向斜，盐丘构造具有重要的经济价值，盐核常成重要的盐类或硫磺矿床，盐上的穹隆及周缘围岩中常富集石油和天然气。 以泥质为核的底辟称为泥质底辟，又称泥火山，泥质中的甲烷气体在泥火山形成中起了重要作用。由岩浆上拱并侵入围岩而形成的称岩浆底辟。 |
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条