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   geothermal fields 在 石油天然气工业 分类中 的翻译结果: 查询用时:0.008秒
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geothermal fields
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  地温场
    Comparison of regional geothermal fields and analysis of organic geochemistry exhibited thermal evolution characteristics of organic matter in each fault depression, established hydrocarbon generation model, and summarized the extent of oil formation zone and hydrocarbon generation potential of source rock in three different fault depression of Erlian rift system. Furthermore, it is pointed out that Ⅰ type fault depression enriched in oil is the most favourable target for oil/gas exploration.
    通过区域地温场的对比和大量的有机地化资料分析研究,明确了各断陷有机质热演化特征,建立了断陷群烃源岩有机质的热演化生烃模式,总结归纳出二连裂谷系三种类型断陷烃源岩的成油带长度及生油气潜力,指出Ⅰ类断陷为含油断陷,是二连裂谷断陷群中最有勘探前景的断陷。
短句来源
    Such hydrocarbon dis- tribution pattern is clearly different from that generated slowly in normal geothermal fields,whieh shows symmetrical distribution with balanced light and heavy hydrocarbons.
    与正常地温场缓慢生成烃类的轻、重烃平衡、对称的分布模式明显不同。
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  “geothermal fields”译为未确定词的双语例句
    9)asymmetry in geothermal fields.
    9)地热场空间不均。
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  geothermal fields
The geothermal fields monitored in the study were, from west to east, Yalova, Efteni, Bolu, Mudurnu, Seben, Kur?unlu-?ank?r?, Hamam?zü, G?zlek and Re?adiye.
      
Such a mechanism is possibly significant under high-temperature conditions at geothermal fields because of temperature enhancement on chemical reactions for the sealing.
      
The locations of geothermal fields therefore appear to be influenced by plate geometry and correspond to lateral breaks in the continuity of the underthrusting plate.
      
A preliminary analysis, however, suggests that these geothermal fields are not situated along entire segments of plate boundaries but only at certain locations.
      
A number of geothermal fields explored so far in the circum-Pacific area occur along spreading ridges and subduction zones in areas of young tectonism and volcanism.
      
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The transition span is a special environment for forming oil-gas pools. The reason is that in a transition span there are abundant oil-gas-formig matter, a high geothermal field,appro-priate reservoir-cap rock asssociations,systematie networks for migration of oil and gas and multiple oil-gas-trap types.

过渡际是油气藏形成的特殊场所,原因在于过渡际中物质基础雄厚。地温场较高、储盖组合配置得当、有自成系统的油气运移通道网络以及存在多种圈闭类型。

Polygenetic compound oil-gas pools occupy an important position in the oil-gas domains of China.They occur principally in transition spans(including the transformation period between the stages of evolution of a crustobody and the transition zone between positive and negative tectonic units).There are four principal causes:(1)In transition spans.especially spatial ones,multichannel oil-gas sources may concentrate.(2)In transition spans is developed a systematic network of passages for migration of oil and gas,which...

Polygenetic compound oil-gas pools occupy an important position in the oil-gas domains of China.They occur principally in transition spans(including the transformation period between the stages of evolution of a crustobody and the transition zone between positive and negative tectonic units).There are four principal causes:(1)In transition spans.especially spatial ones,multichannel oil-gas sources may concentrate.(2)In transition spans is developed a systematic network of passages for migration of oil and gas,which can gather oil and gas from several sources into the same trap.(3)In transition spans there exist a variety of trap types.(4)in transition spans the association of reservoir with roof rock has many types.In addition,the high geothermal field in transition spans is also an important factor.It should be noted that transition spans of compressional regime differ from those of extensional regime and,therefore,differ from them also in trap-forming conditions,oil-gas pool types and distribution pattern of oil and gas accumulation zones.

在中国油气域中,多因复成油气藏占有相当重要的地位,它主要分布于过渡际(包括壳体演化阶段转换期及正负构造单元过渡带)中。主要原因有四个方面:①过渡际中具备集结多渠道油气源条件,空间过渡际者尤为突出,②过渡际中发育有自成系统的油气运移通道网络,可将多个油气源的油气汇聚于同一圈闭之中;③过渡际中存在形式多样的圈闭类型;④过渡际中具有多种类型的储盖组合。此外,空间过渡际中的地温场往往较高也是一个重要因素。值得指出的是,压性环境和张性环境的过渡际状况有所不同,因而,各自的成藏条件、油气藏类型和油气聚集带的展布方式亦有较大的差异。

The main natural gas-bearing basins in northern China are Huabei Basin,Ordos Basin,Qaidam Basin and Tarim Basin. Four tectonothermal evolution stages can be recognised in Huabei Basin,two stages including four periods inOrdos Basin, five stages in Qaidam Basin and four stages in Tarim Basin. The main natural gas-bearing basins in northern China are common in multiple stages and multiple cycles of tectonothermal evolution,in multiple tectonothermal layers,and in that the distribution of geothermal field...

The main natural gas-bearing basins in northern China are Huabei Basin,Ordos Basin,Qaidam Basin and Tarim Basin. Four tectonothermal evolution stages can be recognised in Huabei Basin,two stages including four periods inOrdos Basin, five stages in Qaidam Basin and four stages in Tarim Basin. The main natural gas-bearing basins in northern China are common in multiple stages and multiple cycles of tectonothermal evolution,in multiple tectonothermal layers,and in that the distribution of geothermal field is correspondent to the tectonic divisions.Since Archaean,there has been a complicated tectonothermal process in northern China,ie.the highly geothermal geodome stage→highly geothermal geosyncline stage→lowly geothermal platform stage→highly geothermal depression stage The geothermal field in the mantle ,mantle creep current and the thickness of the crust are three main factors controlling the tectonothermal evolution of the continental crust .

中国北方主要天然气盆地包括地洼型华北盆地、柴达木盆地、塔里木盆地和残留地台型鄂尔多斯盆地。华北盆地构造热演化史可以划分为四个阶段,鄂尔多斯盆地构造热演化史包括两个阶段四个发展期,柴达木盆地构造热演化过程分五个阶段,塔里木盆地则经历了四个阶段的构造热演化历程。中国北方主要天然气盆地的构造热演化具有如下共同特点:多阶段性,多旋回性,地热场结构多层性和地热场展布与构造分区一致性。自太古代至今,中国北方主要天然气盆地构造热演化的总体规律是:高(温)热(场)前地槽穹隆阶段→高热地槽阶段→低热地台阶段→高热地洼阶段。地幔热场、地幔蠕动流和地壳厚度是决定大陆地壳构造热演比性质的三大主体因素。

 
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