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分布区带
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  “分布区带”译为未确定词的双语例句
     3. According to the vertical superposition of composed sandbody and horizonal heterogeneity of reservoir, there has been divide into 3 different sedimentary belts,that is major channel belt, channel margin and mouth bar belt and marginal sand bar-flooding fan -flooding plain belt, and discussed the different remaining oil distribution characteristic.
     3.从垂向叠置和平面组合上探讨了复合砂体的内部沉积构成和储层非均质特征,划分出主河道带、河道边缘—河口坝带、边缘砂坝—决口—越岸带等砂岩分布区带,指出各带的剩余油分布特征。
短句来源
     According to distribution of sandstone and types of reservoirs, predicatefavorable exploration belts.
     结合砂体分布和储层类型预测了有利的储层分布区带,指出了有利储盖组合分布区,为区内的勘探提供了参考。
短句来源
     Based on the studies of sedimentary systems, sandstone body types and regional structures, as well as the relation between the trap types and the favourable" source kitchens", the authors indicated that 3 major reservoir types can be classified, and 3 favourable belts can be circled in which various types of petroleum reservoir might be occured.
     本文论述松辽盆地三肇地区扶杨油层的沉积体系、储层砂体类型及其与区域构造的匹配关系,并论述其圈闭类型与有利油源区的配置及区内存在的3种主要油气藏类型,预测、划分出3个不同类型的油气藏分布区带
短句来源
     The sedimentary microfacies belt of gypsodolomite flat is the zone advantageous to the growth of reservoir bodies in this region,the palaeokarst slope is the zone where the effective denudation pores and cavities are mainly distributed,and the coincidence of the two in space can form the denudation pore and cavity reservoir body with a large area and stable distribution,so as to prepare the necessary reservoir spare for the formation of the gas reservoir.
     含膏云坪沉积微相带是本区有利储集体的发育区带,古岩溶斜坡区是有效溶蚀孔洞的主要分布区带,二者在空间上的吻合,形成了大面积稳定展布的溶蚀孔洞储集体,为气藏的形成准备了主要的储集空间;
短句来源
     Qinghai-Tibet plateau is one of the areas of the most concentrated and strong seismic activity in the global continent, and Qilian active mountain chain on the northeast margin of Qinghai-Tibet block is one of the most strong active tectonic zone in Qinghai-Tibet block.
     青藏高原是全球陆内地震活动最为集中而强烈的分布区带之一 ,位于高原块体东北缘的祁连山逆冲推覆型活动山链又是其中最强烈的现代活动构造带之一。
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     a. zone, E.
     C,E.
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     sakmaricus zone and C.
     centrifugus—C.
短句来源
     For species belonging to the same family, the distributions of isozyme bands were similar.
     属于同一科的种类的酶分布区较接近.
短句来源
     Predicting the potential geographical distribution of flavescence dorée and its vector Scaphoideus titanus Ball in China using DIVA-GIS
     葡萄金黄化病和葡萄叶蝉在中国的潜在分布区
短句来源
     THE REGIONARIZATION OF THE BRYOPHYTES IN CHINA
     中国苔藓植物的分布区
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  range zone
Position of the Blyb Complex in the pre-Mesozoic crustal structure of the Front Range Zone in the Northern Caucasus
      
A number of Variscan nappe complexes were recognized in the Late Mesozoic structure of the Front Range Zone of the Greater Caucasus in the 1970s.
      
The hanging wall of the Blyb Thrust Fault may be traced farther southward into the Main Range Zone, where it most likely consists of the Laba Group and other rocks.
      
These relationships suggest that the rock complexes of the Front Range Zone could have undergone repeated displacements due to post-Variscan (Indosinian) tectonic events and overrode crystalline rocks in the Main Range Zone and more easterly areas.
      
Paleozoic rocks in infrastructure of the metamorphic core, the Greater Caucasus Main Range zone
      
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Based on the studies of sedimentary systems, sandstone body types and regional structures, as well as the relation between the trap types and the favourable" source kitchens", the authors indicated that 3 major reservoir types can be classified, and 3 favourable belts can be circled in which various types of petroleum reservoir might be occured. Fortunately, the suggestions proposed by the authors have been confirmed by the latest exploration activities.

本文论述松辽盆地三肇地区扶杨油层的沉积体系、储层砂体类型及其与区域构造的匹配关系,并论述其圈闭类型与有利油源区的配置及区内存在的3种主要油气藏类型,预测、划分出3个不同类型的油气藏分布区带。本文提出的油气藏分布规律已被勘探成果证实。

The Ordovician fossil weathered residuum gas reservoir in the centre of Eerduosi Basin has a specific assemblage of forming reservoir.Two sets of hydrocarbon source rocks of the Upper and Lower Paleozoic supplied it with abundant mixing source gas and the natural gas supplied by the Upper Paleozoic sourrce rocks is more than the Lower Paleozoic ones.The sedimentary microfacies belt of gypsodolomite flat is the zone advantageous to the growth of reservoir bodies in this region,the palaeokarst slope is the zone...

The Ordovician fossil weathered residuum gas reservoir in the centre of Eerduosi Basin has a specific assemblage of forming reservoir.Two sets of hydrocarbon source rocks of the Upper and Lower Paleozoic supplied it with abundant mixing source gas and the natural gas supplied by the Upper Paleozoic sourrce rocks is more than the Lower Paleozoic ones.The sedimentary microfacies belt of gypsodolomite flat is the zone advantageous to the growth of reservoir bodies in this region,the palaeokarst slope is the zone where the effective denudation pores and cavities are mainly distributed,and the coincidence of the two in space can form the denudation pore and cavity reservoir body with a large area and stable distribution,so as to prepare the necessary reservoir spare for the formation of the gas reservoir.A reasonable disposition of the multiple set cap rocks including the direct cap rocks(Benxi Formation of Carboniferous)and indirect cap rocks(Upper Paleozoic)is the sufficient condition of forming an ideal source reservoir seal assemblage for the Ordovician fossil weathered residuum gas reservoir.The ancient erosion groove and diagenesis compact belt constitute a regional large sized palaeogeomorphologic lithologic trap.And the large ancient buried platform is the beneficial zone for the migration and accumulation of natural gas,controlling the shape and scope of the gas reservoir.

鄂尔多斯盆地中部奥陶系古风化壳气藏有其特定的成藏组合。上、下古生界两套烃源岩提供了丰富的混源气,其上古生界烃源岩提供的气源较下古生界丰富;含膏云坪沉积微相带是本区有利储集体的发育区带,古岩溶斜坡区是有效溶蚀孔洞的主要分布区带,二者在空间上的吻合,形成了大面积稳定展布的溶蚀孔洞储集体,为气藏的形成准备了主要的储集空间;直接盖层石炭系本溪组和间接盖层上古生界发育的多套封盖层的合理配置,是形成奥陶系古风化壳气藏较理想生储盖组合的充分条件;古侵蚀沟槽与成岩作用致密带组成区域性大型古地貌—岩性圈闭;大型古潜台是天然气运聚的有利区带,它控制了气藏的形态和分布范围。

Qinghai-Tibet plateau is one of the areas of the most concentrated and strong seismic activity in the global continent, and Qilian active mountain chain on the northeast margin of Qinghai-Tibet block is one of the most strong active tectonic zone in Qinghai-Tibet block. Daliushu damsite district is situated in the secondary fault zone of the MBT(main boundary thrust) of North-Qilian Mountain front named as Xiangshan-Tianjinshan thrust nappe zone in Gulang-Zhongwei-Tongxin arc thrust-strike-slip active zone....

Qinghai-Tibet plateau is one of the areas of the most concentrated and strong seismic activity in the global continent, and Qilian active mountain chain on the northeast margin of Qinghai-Tibet block is one of the most strong active tectonic zone in Qinghai-Tibet block. Daliushu damsite district is situated in the secondary fault zone of the MBT(main boundary thrust) of North-Qilian Mountain front named as Xiangshan-Tianjinshan thrust nappe zone in Gulang-Zhongwei-Tongxin arc thrust-strike-slip active zone. In the thrust nappe zone, the size of the trunk fault F 201 and its active intensity both mainly affect the stability of the dam being built. this paper also expounds fault F 201 controlling on its secondary faults and F 7(8) , another major fault, by analyzing basic framework of the fracture in the district and activity of the secondary fault F 39 and F 40 is quantitatively simulated by finite element method.

青藏高原是全球陆内地震活动最为集中而强烈的分布区带之一 ,位于高原块体东北缘的祁连山逆冲推覆型活动山链又是其中最强烈的现代活动构造带之一。大柳树坝址区即位于该活动山链的北祁连山前主边界逆冲断裂活动带向东延伸的分支断裂 ,即古浪 -中卫 -同心弧形逆冲走滑活动断裂带内的东段 ,中卫 -同心弧形逆冲走滑活动断裂带的香山—天景山逆冲推覆构造带内。逆冲带内的主干活动断裂 F2 0 1 的规模及活动强度是影响坝址稳定的主要因素。本文通过分析大柳树坝址区基本断裂构造格局 ,阐述了 F2 0 1 断层活动对坝区内另一条主干断层 F7( 8) 以及位于坝址上分支断层 F39、F40 的控制牵动效应。通过室内有限元数值模拟 ,定量分析了断层 F2 0 1 的活动对分支断层 F39、F40 的牵动程度。

 
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