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顶部不整合
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  top unconformity
     The key surfaces,which reflect the tectonic evolutionary stages,are pre rift unconformity surface,transgressive surface,maximum flooding surface,and top unconformity surface of immediate post rift sediments.
     反映构造阶段演化的关键界面为前裂谷期不整合面、水进面、最大洪泛面和后裂谷早期沉积顶部不整合面。
短句来源
     The top unconformity of lower Paleozoic and dolomite rock of Yeli-Liangjiashan group are two very important reservoir strata.
     下古生界顶部不整合面附近及冶里-亮甲山组白云岩是2套重要的储集层段.
短句来源
  “顶部不整合”译为未确定词的双语例句
     CHARACTERISTICS AND OIL-CONTROLLING SIGNIFICANCE OF UNCONFORMITY STRUCTURE LAYER ON TOP OF CARBONATE ROCK
     碳酸盐岩顶部不整合面结构层及控油意义
短句来源
     Directed by theresults of foreward modeling, to analyze the wave form charateristic ofburied grooves on the Majiagou formation unconformity of the Paleozoicperiod, to analyze seismic attributions of the sand body in the pre –Paleozoic period and Mesozoic.
     本文以大量的正演模型结果为指导,分析下古生界马家沟组顶部不整合面潜沟、上古生界和中生界砂体在地震剖面上的波形及属性特征;
短句来源
     Surface of unconformity and ancient stream channel sandbody of Jurassic constitute the major migration pathway of the Jurassic,the oil reservoir accumulated primarily in the ancient stream channel and places near the surface of unconformity.
     三叠系顶部不整合面和侏罗系古河道砂体共同构成了侏罗系油藏的油气主要运移通道,其油气主要分布在侏罗系古河道内及其不整合面附近。
短句来源
     The subtle reservoir of carbonate rock in Lunguxi buried hill is a dissolution fissure-cave reservoir distributed along the top of Ordovician unconformity where oil-gas distribution is uncontrolled by local structural high.
     轮古西潜山油藏是沿奥陶系顶部不整合构造分布的碳酸盐岩古岩溶缝洞型隐蔽油藏,油气分布不受现今局部构造高点控制。
短句来源
  相似匹配句对
     CHARACTERISTICS AND OIL-CONTROLLING SIGNIFICANCE OF UNCONFORMITY STRUCTURE LAYER ON TOP OF CARBONATE ROCK
     碳酸盐岩顶部不整合面结构层及控油意义
短句来源
     (9) the large-scaled unconformity strata;
     (9)大型不整合;
短句来源
     DISCOVERY OF PALEOKARST UNCONFORMITY ON TOP OF THE LOUSHANGUAN FORMATION,WESTERN HUBEI,AND ITS SIGNIFICANCE FOR SEQUENCE STRATIGRAPHY
     鄂西娄山关组顶部古岩溶不整合面的发现及层序地层学意义
短句来源
     THE DETACHMENT ON THE UNCONFORMABLE SURFACE
     不整合面上的滑脱构造
短句来源
     Top drive drilling system(一)
     顶部驱动钻井装置(一)
短句来源
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Above and under the unconformity at the top of carbonate rocks in North Tarim (Tabei) uplift show that three structural layers were developed widely They are sedentary deposit layer, seepage flow layer, and under flow layer. Related studies of distribution and oil-controlling factors indicate: sedentary deposit layer occurs widely in both above and under the unconformity. It is the best path to regional oil and gas migration; the seepage layer mainly distributes on high part of palaeoarch, it is a potential...

Above and under the unconformity at the top of carbonate rocks in North Tarim (Tabei) uplift show that three structural layers were developed widely They are sedentary deposit layer, seepage flow layer, and under flow layer. Related studies of distribution and oil-controlling factors indicate: sedentary deposit layer occurs widely in both above and under the unconformity. It is the best path to regional oil and gas migration; the seepage layer mainly distributes on high part of palaeoarch, it is a potential place to seek large cave-fissure oil and gas fields; the underflow layer mainly distributes in the slope of uplift-sag transition, it is another possible place to seek "inside" oil and gas pools.

塔北隆起碳酸盐岩顶部不整合面的上、下普遍发育残积层、渗流层和潜流层。残积层广泛分布于不整合面上、下,是区域性油气运移的良好通道;渗流层主要分布于古隆起高部位,有利于形成溶蚀性大油气田;潜流层主要分布于隆坳过渡斜坡区,有利于内幕油气藏的发育。

Evolution of rift basins is divided into rift initiation,rift climax,immediate post rift,and late post rift stages.The key surfaces,which reflect the tectonic evolutionary stages,are pre rift unconformity surface,transgressive surface,maximum flooding surface,and top unconformity surface of immediate post rift sediments.Maximum flooding deposits are most developed intervals of possible source rocks.Mapping of the key surfaces and defining of source rocks are important for hydrocarbon exploration of rift...

Evolution of rift basins is divided into rift initiation,rift climax,immediate post rift,and late post rift stages.The key surfaces,which reflect the tectonic evolutionary stages,are pre rift unconformity surface,transgressive surface,maximum flooding surface,and top unconformity surface of immediate post rift sediments.Maximum flooding deposits are most developed intervals of possible source rocks.Mapping of the key surfaces and defining of source rocks are important for hydrocarbon exploration of rift basins.Play types of rift basins are:(1)buried hill pools of pre rift stage; (2)fluvial,delta,and subaqueous fan sandstone and conglomerate pools of lowstand systems tract deposited during rift initiation stage; (3)gravity flow channel sandstone and turbidite fan pools of rift climax transgressive systems tract;and (4)fan delta,braid delta,delta and fluvial sand stone pools of immediate post rift highstand systems tract.Play types of depression stage of faulted depression stacked basins are incised valley,fluvial delta,and shoreface sandstone pools.Sequence stratigraphic study of petroliferous provinces,genesis of nonmarine sequences,and high-resolution sequence stratigraphic study should be enhanced in hydrocarbon exploration practices of China in the 21st century,in order to serve for discovering new petroliferous sags and strata and finding subtle traps and new reserves in “matured” exploration regions

裂谷盆地演化可分为裂谷初始期、深陷期、后裂谷早期和后裂谷晚期阶段。反映构造阶段演化的关键界面为前裂谷期不整合面、水进面、最大洪泛面和后裂谷早期沉积顶部不整合面。最大洪泛期的沉积物可能是烃源岩最发育的层段。关键界面作图与烃源岩的确定对裂谷盆地的油气勘探有着重要意义。裂谷盆地的成藏组合类型为前裂谷期潜山油气藏 ;裂谷初始期低水位体系域河流、三角洲和水下扇砂砾岩体油气藏 ;裂谷深陷期水进体系域重力流水道砂体和浊积扇体油气藏 ;后裂谷早期高水位体系域扇三角洲、辫状河三角洲、三角洲和河流砂体油气藏 ;具断—坳叠合结构盆地的坳陷阶段发育下切谷、河流—三角洲和滨岸砂岩油气藏。在 2 1世纪我国油气勘探实践中 ,应加强含油气大区层序地层学、陆相层序成因与高分辨率层序地层学研究 ,为寻找新的含油气凹陷与含油气层系、寻找隐蔽圈闭与老区挖潜服务。

Palaeogeomorphology is one of the main factors. It controls not only the development and distribution of the late sedimentary facies but also the assemblage of reservoirs and capping formations. Just like the modern geomorphology, it is influenced by the tectonic position, climate, base level, and so on. Rebuilding the palaeogeomorphology is a complex work. The Jurassic sedimentary strata of the Ordos Basin develops upon the denudation surface generated during the Indosinian orogeny, and their characteristics...

Palaeogeomorphology is one of the main factors. It controls not only the development and distribution of the late sedimentary facies but also the assemblage of reservoirs and capping formations. Just like the modern geomorphology, it is influenced by the tectonic position, climate, base level, and so on. Rebuilding the palaeogeomorphology is a complex work. The Jurassic sedimentary strata of the Ordos Basin develops upon the denudation surface generated during the Indosinian orogeny, and their characteristics are being controlled by palaeogeomorphology. Therefore, the renewing work of the palaeogeomorphology of Ordos before Jurassic deposition can efficiently direct the exploration of the Jurassic oil reservoir. The palaeogeomorphology of the Ordos Basin shows that the northern and western parts are high but the southern and eastern parts are low in the basin. It includs five palaeogeomorphologic units, that is, highland, valley plain, hilly area depression area and palaeo river. The paper mainly discusses the ways of rebuilding palaeogeomorphology and its relationship with the late oil reservoir through rebuilding the palaeogeomorphology of the Ordos Basin before Jurassic.

古地形地貌是控制一个盆地后期沉积相发育与分布的一个主要因素 ,同时在一定程度上控制着后期油藏的储盖组合。同现在地貌一样 ,古地貌形态受到了所处的区域构造位置、气候、基准面变化及构造运动等因素综合作用的影响。鄂尔多斯盆地侏罗系发育在由印支运动主幕所造成的三叠纪顶部不整合接触面上 ,早侏罗世沉积特点主要受控于沉积前古地形地貌 ,因此开展侏罗纪沉积前古地貌恢复工作及探讨古地貌对后期油气藏关系对于寻找侏罗系油田具有重要的指导意义。作者主要是从沉积学角度出发 ,通过对鄂尔多斯盆地侏罗纪沉积前古地形地貌的恢复研究 ,进一步对古地貌恢复从方法上进行了研究 ,同时探讨了沉积前古地貌对后期油藏的控制作用

 
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