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basins相关的网络例句

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与 basins 相关的网络例句 [注:此内容来源于网络,仅供参考]

In a view of the theory of the traditional oil and gas formation it is considered that the oil and gas resources buried in sedimentary basins are generated by OM in source rocks during thermal evolution and marine, lacustrine sapropel and humic-sapropel OM is the mater of the formation of considerable oil and gas but coal-measure strata is relatively bad source rocks, being considered that they can not generate significant amounts of oil and gas.

传统的石油天然气成因理论认为蕴藏于沉积盆地的油气资源是由烃源岩中的有机母质在热演化过程中形成的,而且是海相或者湖相腐泥型和腐泥-腐殖混合型的有机质有利于形成大量的石油和天然气,而煤系地层相对是较差的烃源,认为这种烃源岩不能形成大量的油气。

From the research of the kerogen carbon isotopes of the coal-measure strata in some basins of China (the Carbo-Permian in the Ordos basin, the Triassic in the Sichuan basin, the Jurassic in the Jungar basin and Turpan-Hami basin, the Tertiary in the Yingqong basin) it can be indicated that the Type Ⅲ kerogen has a wide δ〓C range from -21. 2‰ to -27. 6‰, averaging -25‰, which is more enriched in 〓C than sapropel and mixed kerogens.

对我国一些含煤盆地(陕甘宁石碳-二叠、四川三叠系、准噶尔侏罗系、吐哈侏罗系、莺琼盆地第三系)的煤系地层干酪根碳同位素研究表明,煤系地层的干酪根碳同位素组成δ〓C值分布范围为-21.2~-27.6‰,说明其变化范围较宽,平均值为-25‰左右,相对腐泥型干酪根和混合型干酪根较明显地富重碳同位素。

Based on the previous researches, combined with the further understanding of the present oil\|gas exploration, the exploitation of the Junggar basin, the analysis of the sedimental strata characteristics in different stages and the mountains profiles on the margin of the Junngar basin, it is considered that there are three\|period foreland basins formed since the Permain in Junggar basin.

基于前人的研究成果,结合在准噶尔盆地油气勘探开发实践中取得的新认识和对准噶尔盆地周缘盆—山耦合区带地质剖面及盆地不同时期沉积地层特征的分析,认为该盆地自二叠纪以来发育了3期前陆盆地,这3期前陆盆地及与其相关坳陷的组合和叠加是形成准噶尔盆地丰富油气资源和多样化成藏模式的主要原因。

Because of the stratigraphic conditions of multi-lithologies and thin-bed association, unstability of lithofacies in the vertical and lateral direction, and the particalar conditions of seissmic geology in Inland Basins, Western China, a stratigraphic model of sedimentary facies in which there are many theoretical reflecting seismic interface does not completely display on the seismic section, especially the some the most important stratigraphic information such as toplap, onlap, progradation, erosional truncation and fill of channal, divergent, shingled, ect.

本文在研究了9类沉积相及相组合地层模型的地震模拟记录后证明:现今流行的在地震剖面上划分地震相进而应用国外海相地层反射模式再转换为沉积相这一所谓&相面&方法完全不适用于西部陆相盆地沉积相地层模型的特点,作者首次开辟了用速度参数,合成地震记录、二维地层模型技术研究西部盆地地下沉积相的新途经。

Prisonrs in older gaols have to take their basins and buckets to the latrine for slopping out .

老监狱的因犯清早要把他们的便盆,拿到厕所里去倒。

In the morning, prisonrs in older gaols have to take their basins and buckets to the latrine for slopping out.

老监狱的因犯清早要把他们的便盆、便桶拿到厕所里去倒。拖洗室内地面。

In this article, I share several tested, practical design concepts for spillways and stilling basins.

在此,我做了很多测试,为泄洪和st固定基础理论概念。

The geological and geophysical data show that in the lower crust of young continental tectonic units may occur pervasive, non-seismic, subhorizontal and ductile flow related to thermal softening. The laminar flow drives fault-block movement of the upper crust, results in the formation of orogenic belts and sedimentary basins, and causes coupling between ductile lower crust and brittle upper crust/mantle.

大量的地质和地球物理资料表明,年轻的大陆构造活动区的下地壳可能因热软化而出现透入性非地震式顺层韧性流动,这种下地壳层流作用驱动大陆上地壳发生地震式脆性断块运动,形成盆山格局,发生圈层耦合。

This belt was formed during the Indo-China Stage of intracontinental collision of East Qinling Orogen Belt; 9. Many structural features imply the existence of Wudangshan nappe, which was formed by intracontinental subduction during Indo-China stage; and 10. The evidences of stratigraphy, petrology and structure imply that the collision of the two Paleoplate took place during the last stage of Caledonian, while the intracontinental subduction and the nappe took place during Indo-China stage, and the transcurrent basins took place during Yenshan stage. In the last part of this article, all kinds of favourable mineral forming conditions were analysed.

这条高压变质带是印支期东秦岭造山带陆间碰撞阶段产生的;9、各种构造迹象表明武当山推覆体的存在,它是印支期因陆间俯冲造成的准原地推覆体;10、地层、岩石、构造等各方面的证据表明南北板块的碰撞发生于加里东末期,而海西期至印支期为陆间俯冲和推覆作用阶段,燕山期则是应力松驰和断陷盆地发育的阶段,本文最后对区内各种有利的成矿地质条件作了扼要的分析。

The modern structural pattern ofthe area consists of three synclines and three anticlines, a group of strike faults and a group of transcurrent faults, as well as some downfaulted basins; 8. The blue schist belt, which distributs at the northern part of the area, has a genetic relationship with the decollement plane between Yaolinghe Group and Doushantuo Formation.

晚元古代扬子板块北缘由被动大陆边缘转化为主动陆缘;7、本区的现存构造格局,由近东西向的三个复式向斜加三个复式背斜,一组走向断裂加一组横向断裂以及若干断陷盆地构成;8、本区北部的蓝闪石类矿物成带分布与耀岭河群与陡山沱组之间的层间滑脱面有关;一百五十多个白云母b。

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Since this year, in a lot of villages of Beijing, TV of elevator liquid crystal was removed.

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