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Palaeogene相关的网络例句

查询词典 Palaeogene

与 Palaeogene 相关的网络例句 [注:此内容来源于网络,仅供参考]

The basin evolution from the Cretaceous to the Palaeogene shows a complete process of rifting development, in which the Lower Cretaceous is theproduct of early rifting and the Upper Cretaceous and the Eogene represent the sediments of thermal subsidence in late rifting stage.

白垩纪—早第三纪盆地演化为一个完整的裂谷发育过程,下白垩统是裂谷早期断陷作用的产物,而上白垩统和下第三系则代表裂谷后期热沉降沉积。

Two sets of oil-bearing series,the upper E_2s_4 and E_2s_3 of Palaeogene in Boxing subsag,were studied by adopting organic geochemistry,high-resolution sequence stratigraphy and pool-forming dynamics.

应用有机地球化学、高分辨率层序地层学和成藏动力学等研究方法,对博兴洼陷古近系沙四上亚段和沙三段两套烃源岩的油气成藏的差异性进行了研究。

In the Shasan (the third member of Shahejie Formation of the Palaeogene) age, huge deep water mudstone and multiple low angle sloped lake floor fan sediments were deposited as a result of active faulting and subsiding.

本区在老第三纪沙河街组第三段即沙三段沉积时期断陷活动强烈,发育了巨厚的深水泥岩和多期次缓坡型湖底扇沉积,为油气聚集成藏提供了丰富的油气源条件和储集条件。

The crust-mantle background and space distribution of palaeogene source rock in the east of China,the tectonic background,sediment and basin environment,state of organic matter,abundance of organic matter and type of organic matter in source rocks and geothermal field characters are analyzed.

对我国东部下第三系源岩发育的壳幔背景及空间展布、源岩发育的构造背景、沉积和盆地环境、有机质赋存状态、有机质丰度、类型及地温场特征等方面的研究表明,秦岭-大别和郯庐断裂的生成演化是区内下第三系盆地发育的主要构造控制因素,渤海湾北东向裂谷型盆地规模大、切割深,有效烃源岩最为发育;南华北近东西向-北西西向断陷型盆地规模小、切割浅,有效烃源岩相对最不发育;而立交桥型的南襄盆地有效烃源岩发育程度介于两者之间。

The analysis of group component, stable carbon isotopic compositions and biomarker, and the geochemical characteristics of the oil and gas show that the oil comes from the Palaeogene and the oil reservoir is new bed-generating and old bed-storing; the gas comes from Carboniferous-Permian and the gas reservoir is old bed-generating and new bed-storing.

通过对油气族组成、稳定碳同位素组成及生物标志化合物进行油气地球化学研究,认为东濮凹陷三叠系砂岩裂缝性油藏原油来源于古近系,油藏类型为新生古储式;天然气来源于石炭-二叠系,气藏类型为古生新储式。

In order to identify the disputed oil source in Suaiqo-Wen'an region, Baxian sag, Jizhong depression, on the basis of source rock evaluation and oil-to-source correlation in this region, we recognized the typical Palaeogene oil and Carboniferous-Permian oil viz. two-ends oil, and established effective identification index from detailed analysis of biological marker, separation of nitrogen containing compound, stable carbon isotope and also make reference to the foreign studies on coal derived oil.

针对长期以来冀中坳陷坝县凹陷苏桥-文安地区存在的原油来源争议的问题,在对本区烃源层评价认识和油源对比的基础上,运用生物标志物精细检定、含氮化合物的分离检定、稳定碳同位素分析等技术手段,并结合国内外煤成油的研究成果,划分出了坝县凹陷典型的下第三系原油和石炭-二叠系原油,即两类端元油,并提出了有效的判识指标。

The forming of lithologic reservoirs in the Palaeogene of Boxing Sag is generally characterized by multiple hydrocarbon expulsion,expulsion and accumulation coupling,and fourfold genesis controlling reservoir-forming.

博兴洼陷下第三系岩性油藏的形成具有&复式排烃、排聚耦合和四元控藏&的总体特征,而其独特的烃源岩结构和地层压力系统决定了沙四上亚段和沙三段烃源岩在排烃方式、排烃机制以及岩性油藏成藏特点上的不同。

Based on the identification of the sequence boundry with the comprehensive analyses of the seismic, well logging and well drilling data, the palaeogene in Jiyang depression can be divided into one lst-order and three 2nd-order sequences, of which six 3rd-order sequences can be subdivided from the third stage of Shahejie formation to Dongying formation.

本文在综合利用地震、声波时差测井、地层倾角测井、电阻率测井、岩心、地球化学等方法进行层序地层界面识别的基础上,将济阳坳陷古近系划分出1个一级层序,3个二级层序,其中沙三段-东营组分出6个三级层序。

In the temproal-spatial′distribution, its source rocks is mainly Palaeogene, secondly Cretaceous and Jurassic of Mesozoic, Triassic, having mudy rocks and coal-rich, their organic carbon being 0.2% and 0.4% respectively.

提出了过渡带气综合判识标志:时空分布上,其源岩主要为下第三系,其次为中生界白垩系和朱罗系、三叠系,以泥质和煤系有机质最丰富,有机碳丰度为0.2%、后者为0.4%。

It stably subsided after its formation. During Palaeogene ang Neogene salt-forming, Kuqa basin experienced strong-weak-strong tectonic stages, and its center of subsidence moved gradually from north to south and depocenter from northwest to east and southeast. Because of tectonic differentiation, series of second depression formed in Kuqa basin.

盆地自形成以来一直处于稳定的沉降状态,在古近纪和新近纪成盐期,盆地经历了强-弱-强3个构造演化阶段,其沉降中心由北而南逐渐迁移,沉积中心由北西逐渐向东、南东方向迁移,盆地内的构造分异渐趋明显,形成了一系列次级凹陷。

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