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   水文地质旋回 的翻译结果: 查询用时:0.206秒
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水文地质旋回
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  “水文地质旋回”译为未确定词的双语例句
     the second one(J 1b -J 2x )is a mid-depth,weakly opened compacting drive hydrodynamic system;
     第二水文地质旋回J1b-J2x,属于中层弱开放的压实驱动型水动力系统。
短句来源
     the third one(J 2t -K)be-longs to shallow,strongly opened gravity drive hydrodynamic one.
     第三水文地质旋回J2t~K(J2t可属于过渡带),属于浅层强开放的重力驱动型水动力系统;
短句来源
     6 hydrogeologic circles after the deposition of the Yangxin Limestone are recognized.
     研究区自阳新统沉积后,经历了6个水文地质旋回
短句来源
     For the first time, the hydrogeological development history of deep groundwater has been introduced and the reconstruction of palaeo hydrogeology has been comducted and the new concept, i.e., the palaeohydrogeological cycle, has been put forward.
     而且首次探讨了深层地下水的水文地质发育史 ,进行了古水文地质再造 ,提出了古水文地质旋回的新概念。
短句来源
     According to the depositional, structural and hydrochemical features in Gunan sub-sag, the hydrogeological process is divided into 3 cycles of hydrogeology of Middle-Upper Eocene to Lower Oligocene in abnormal pressure, Middle-Upper Oligocene in transitional pressure and Miocene to Quaternary.
     根据孤南洼陷的沉积、构造和水化学特征,将其水文地质作用划分为3个水文地质旋回:异常压力的中上始新统-下渐新统旋回、压力过渡状态的中上渐新统旋回和正常压力的中新统-第四系旋回。
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  相似匹配句对
     GLOBAL CYCLOSTRATIGRAPHY
     全球旋回地层学
短句来源
     Hydrogeologic Management Information System
     水文地质管理信息系统HMIS
短句来源
     6 hydrogeologic circles after the deposition of the Yangxin Limestone are recognized.
     研究区自阳新统沉积后,经历了6个水文地质旋回
短句来源
     A Stady on Hydrogeological Model
     水文地质模型的研究
短句来源
     Metallogeny in Relation to Supercontinent
     超大陆旋回和成矿作用
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The paleo-hydrogeological condition of Dongying depression and its relation with oil and gas have been studied. The Cenozoic (Kz) in this area is divided into three hydrogeological cycles of Eocene (E2), Oligocene (E3) and Neogene (N)-Quaternary (Q) . Each cycle is in turn divided into two hydrogeological stages of deposition and seeping. The first two cycles brought about accumu-lation and burial of a great quantity of organic matter. The last one was the most important period of generation, migration and accumulation...

The paleo-hydrogeological condition of Dongying depression and its relation with oil and gas have been studied. The Cenozoic (Kz) in this area is divided into three hydrogeological cycles of Eocene (E2), Oligocene (E3) and Neogene (N)-Quaternary (Q) . Each cycle is in turn divided into two hydrogeological stages of deposition and seeping. The first two cycles brought about accumu-lation and burial of a great quantity of organic matter. The last one was the most important period of generation, migration and accumulation of oil and gas in this area. It was also the formation period of a large number of oil and gas pools. The general direction of s tratigraphic water in this area was from the center of the depression to the periphery. The seeping of the peri-pheral surface water was secondary. An estimation of the number of water-displacement in deposition and seeping stages show that the activity of depo-sition water far exceeds that of seeping water. This is quite favourable to the migration, accumulation and preservation of oil and gas.

本文探讨了东营凹陷的古水文地质条件反其与油气的关系。文中将本区新生代划分为始新世、渐新世、中上新世—第四纪三个水文地质旋回,各旋回又进一步划分为沉积和渗入两个水文地质阶段。前两个旋回导致了本区有机质的大量堆积和埋藏,后一个旋回则是本区油气生成、运移、聚集的主要时期,亦是油气藏大量形成的时期。本区古地层水的主要流向是由凹陷内部指向边缘,而边缘地表水的渗入是次要的。估算的水交替次数表明沉积水的活动程度远超过渗入水,这对油气的移聚和保存十分有利。

6 hydrogeologic circles after the deposition of the Yangxin Limestone are recognized. According to data of area integration from the compaction curve, among waters entering into the Yangxin Limestone, Silurian squeezed water is predominant. Water from Longtan Formation and Silurian System are 0.4 trillion cubic metres (26.68 percent of the total Longtan squeezed water) and 7.5 trillion cubic metres (68.34 percent of the total Silurian squeezed water) respectively. The latter gives more influence upon the fluids...

6 hydrogeologic circles after the deposition of the Yangxin Limestone are recognized. According to data of area integration from the compaction curve, among waters entering into the Yangxin Limestone, Silurian squeezed water is predominant. Water from Longtan Formation and Silurian System are 0.4 trillion cubic metres (26.68 percent of the total Longtan squeezed water) and 7.5 trillion cubic metres (68.34 percent of the total Silurian squeezed water) respectively. The latter gives more influence upon the fluids in Yangxin Limestone. Squeezed water for each well in different geologic period is calculated quantitatively. On the palaeohydrodynamic maps, it is clearly observed that the occurrence of high-pressure area is inheritable, that explains why the natural gas is accumulated mainly on the ancient Luzhou uplift and in the western part of the researched region.As the squeezed water entered into Yangxin Limestone, the gas produced from coal in Longtan and the natural gas in Silurian might have also moved into the same stratum. In addition, Yangxin Limestone itself is also a productive source bed. Thus the natural gas in Yangxin Limestone is a mixture of gases originated from several strats.

研究区自阳新统沉积后,经历了6个水文地质旋回。按压实曲线用积分求面积的方法计算结果,自志留系进入阳新统的水量最多,对阳新统的影响较大,并已为若干地球化学资料所证实。从古水动力图上看,高压区的分布是继承性的,因而解释了研究区西部和泸州古隆起上天然气富集的原因。阳新统中的天然气是志留系中生成的天然气、龙潭组中的煤成气以及阳新统本身所生天然气的混合物。

From the cyclic points of view, the present paper deals with the relationship between the underground water flow and hydrocarbons in Jiuxi basin.

酒西盆地可分为二大水文地质旋回,即白垩纪水文地质旋回和新生代水文地质旋回.每个旋回分为二个阶段,即沉积压实水流阶段和重力渗入水流阶段.水动力场、水化学场表明盆地南部油气富集带处于新生代水文地质旋回沉积压实水流的停滞泄水区,而北部单斜带处于重力渗入水流阶段.为了定量分析沉积压实水动力状况,本文提出了一种简便方法,即求解地上水均衡方程,可得出不同时期沉积水动力场特征.计算结果表明,白垩系原生油藏位于水动力场特定部位:高水头区中的低水头区、水头陡急变化带即停滞泄水区.

 
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