1) geopetal structure
示底构造
1.
Trace fossils:the importantgeopetal structure in flysch;
遗迹化石——复理石中重要的示底构造
2.
The geopetal structures of volcanic rocks in Beisantai field of Junggar basin are similar to those of carbonate rocks,which are mainly found in volcanic gas pores and autoclase fissures.
准噶尔盆地北三台火山岩中的示底构造类同于碳酸盐岩发育的示底构造,主要发育于火山岩的气孔和自碎缝中,其下部主要为渗滤泥沉积,上部常为结晶的钠沸石或其他自生矿物,二者之间界面平直。
2) geopetal structure
示顶底构造
3) 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。
4) basement structure
基底构造
1.
Gravity and magnetic anomaly profiles and characteristics of basement structure in the Qiangtang basin,Qinghai-Tibet Plateau;
青藏高原羌塘盆地重磁剖面异常与基底构造特征
2.
To discover the relationship between basement structure and evolution of Yingen basin,the basement structure is studied with methods combining gravity,magnetic,MT and seismic data,drilling data.
为了揭示基底构造与盆地形成演化的关系,从重力、磁力、大地电磁测深、地震、钻井资料入手,研究银根盆地的基底构造特征,并发现其成盆作用与基底构造之间的动力学关系。
3.
Based on 1∶50 000 high precision aeromagnetic data of 1996 and consulting other geophysical and geological data,this paper has analysed the framework of basement structure and fault structure and,in particular,probed into the relationships of aeromagnetic field characteristics,basement structure and fault structure to the distribution of underground thermal water.
以１９９６ 年１∶５ 万高精度航空磁测资料为基础，参考其它地球物理及地质资料，对山东黄河口地区基底构造、断裂构造格架进行了分析，尤其是探讨了航磁场特征、基底构造、断裂构造与地下热水分布的关系，在此基础上对本区的地热水远景进行了初步的分析。
5) 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。
6) basement tectonics
基底构造
1.
Influenced by the subsalt basement tectonics, differential loading and compressional stresses, the halite layers easily flowed from one place to another, and then formed numerous salt-related structures in the Qiulitag structural belt, which had important influences on the hydrocarbon migration and accumulation.
库车坳陷秋里塔格构造带沉积有较厚的古近系和新近系膏盐层,受盐下基底构造、沉积差异负载和构造挤压应力等因素影响,膏盐层发生了明显的塑性流动,影响了该地区的构造变形与演化过程,形成了丰富多样的盐相关构造样式,并对油气运聚成藏过程有重要的控制作用。
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