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adjusting fault
相关语句
  调节断层
     South ramp region results in differential settlement of deposit slope on the same slope due to a series of development of reverse adjusting fault, controlling a set of braided river delta or shallow lake shore system.
     南部缓坡带发育一系列反向调节断层,导致同一斜坡差异沉降,主要发育辫状河三角训或滨浅湖沉积体系。
短句来源
  “adjusting fault”译为未确定词的双语例句
     The traditional Altyn fault is the adjusting fault of the compression deformation of the Western Kunlun and Northern Qilian mountains of the northern margin of the Qinghai Tibet Plateau since Cenozoic.
     新生代以来 ,阿尔金断裂是“调节”青藏高原北缘西昆仑、祁连造山带挤压变形的构造 ,为新生代左旋挤压型转换断层。
短句来源
     The researches are very important to the design,manufacture,installation, adjusting,fault mechanism analyses and treatements of the similar large hydraulic system.
     这一研究对类似的大型液压系统的设计、制造、安装、调试、故障处理和维修有重要的指导意义。
短句来源
  相似匹配句对
     Method of adjusting the extraction advance direction of fault
     调整断层带位置回采推进方向过断层方法
短句来源
     Fault Analyzing and Preventing Measures of Adjusting Speed Inverter
     变频调速器的常见故障分析和预防措施
短句来源
     THE FAULT DELTA
     断块型三角洲
短句来源
     adjusting the microclimate;
     调节小气候 ;
短句来源
     fault inference;
     第二种是“过错推定说” ;
短句来源
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A transform fault is essentially a displacement fault whose terminal parts are adjusted by other tectonic types and whose displacement component is absorbed by other structures intersected with the terminal parts at high angles or met at right angles. The main elements of a transform fault are the steep dipping displacement faults and the adjusted structures intersected with the terminal parts at high angles. According to the combination of the tectonic features formed by the two ends of the displacement...

A transform fault is essentially a displacement fault whose terminal parts are adjusted by other tectonic types and whose displacement component is absorbed by other structures intersected with the terminal parts at high angles or met at right angles. The main elements of a transform fault are the steep dipping displacement faults and the adjusted structures intersected with the terminal parts at high angles. According to the combination of the tectonic features formed by the two ends of the displacement fault and the structures intersected with the terminal parts, the transform fault can be divided into three types, including the adjusted transform fault of extensional normal fault, the adjusted transform fault of compressive fold and thrust fault, and the compound transform fault. The traditional Altyn fault is the adjusting fault of the compression deformation of the Western Kunlun and Northern Qilian mountains of the northern margin of the Qinghai Tibet Plateau since Cenozoic.

转换断层按其“平移”段运动方向分为左旋与右旋 ;按其“平移”段两终端与之高角度相交的构造性质组合进一步分为伸展正断“调节”型转换断层、挤压褶皱 -冲断“调节”型转换断层及复合型转换断层。新生代以来 ,阿尔金断裂是“调节”青藏高原北缘西昆仑、祁连造山带挤压变形的构造 ,为新生代左旋挤压型转换断层。

Tertiary system in Dongying sag is of typical faulted lake-basin deposits, and its structural activity is tightly relative to sedimentation. Dongying sag is divided into three facies belt such as actic region, sag region and ramp region. Through the study, the authors find that the north of the slope break region of the slope structure in the basin developed mainly the variable genesis glutenite fan bodies, the subsalt relief and fault activity controlled the genetic type and through-going of the fan bodies....

Tertiary system in Dongying sag is of typical faulted lake-basin deposits, and its structural activity is tightly relative to sedimentation. Dongying sag is divided into three facies belt such as actic region, sag region and ramp region. Through the study, the authors find that the north of the slope break region of the slope structure in the basin developed mainly the variable genesis glutenite fan bodies, the subsalt relief and fault activity controlled the genetic type and through-going of the fan bodies. Because the fault activities in the single-fault slope break are different from that in step-steep slope break, the sedimentary system of glutenite fan bodies controlled by the fault is also different. Basin deep sag lies in downthrow of fault with developing sidely delta front fluxoturbidite. There are totally three propels from east to west. Three propels correspond to structure action of S3, S2 and S1 respectively. South ramp region results in differential settlement of deposit slope on the same slope due to a series of development of reverse adjusting fault, controlling a set of braided river delta or shallow lake shore system. Tertiary palaeostructral activity in Dongying sag and its control on settlement system and skeletal sand are studied to find the arrangement relation between reservoir and fracture system. It's of great importance to next exploration for subtle reservoirs.

东营凹陷下第三系是典型的断陷湖盆沉积,沉积与古构造活动关系密切。北部陡坡带主要发育各种成因的砂砾岩扇体,基岩的起伏和断层活动控制了扇体的成因类型和展布。由于该带上的单断式构造坡折带与台阶式构造坡折带的断层活动有差异,造成扇体的沉积体系不同;中部洼陷带位于主控断层下降盘,广泛发育三角洲前缘滑塌浊积体系。东营三角洲的3期由东向西的进积分别与沙三段沉积期的3期构造运动相对应;南部缓坡带发育一系列反向调节断层,导致同一斜坡差异沉降,主要发育辫状河三角训或滨浅湖沉积体系。通过对东营凹陷早第三纪古构造活动对沉积体系、骨架砂体控制作用的研究,明确了储集体与断裂体系的配置关系,对该区下一步隐蔽油藏勘探和井位部署有一定指导意义。图4参9(马丽娟摘)

Because of thrust action of Qilian Fold Belt from south to north in Cenozoic,the complex foreland basin was formed laterally in Jiuquan Basin,having following structures successfully:South-Margin frontland thrust belt,South foreland depression,foreland slope,Heishan-Helishan frontal uplift and Huahai-Jinta post-uplift depression;vertically there is characteristic of double-layer structure that the Cenozoic foreland structural layer was stacked on Mesozoic strengthening structural layer.Mainly through the synthetic...

Because of thrust action of Qilian Fold Belt from south to north in Cenozoic,the complex foreland basin was formed laterally in Jiuquan Basin,having following structures successfully:South-Margin frontland thrust belt,South foreland depression,foreland slope,Heishan-Helishan frontal uplift and Huahai-Jinta post-uplift depression;vertically there is characteristic of double-layer structure that the Cenozoic foreland structural layer was stacked on Mesozoic strengthening structural layer.Mainly through the synthetic study of seismic sections and outcrop,the analysis in the paper centers on the characters of geologic structures and structural deformation in Jiuquan Basin since Neogene and the next oil/gas exploration direction,in which the following acknowledge is gained:the structural deformation of South-Margin frontland thrust belt is characteristic of the lateral stack of multiple thrust belts and structural deformation and structures are characterized by clear east-west segmentation because of the divide action of adjusting fault,the strength of structural deformation is generally showed as strong in west and weak in east and trust block is widely thrust above the Lower Cretaceous;oil geologic condition is superiority in South-Margin foreland thrust belt that is most important oil/gas accumulation zone in that basin,among which the thrust structure on the side of down-thrown of thrust block is main targets of next oil/gas exploration.

酒泉盆地在新生代受祁连山褶皱带由南往北的逆冲推覆作用 ,在横向上形成了复杂的前陆盆地结构 ,依次有南缘山前冲断带、南部前陆拗陷、前陆斜坡、黑山—合黎山前缘隆起和花海—金塔隆后拗陷 ;在纵向上表现为新生代前陆构造层叠置在中生代伸展构造层之上的双层结构特征。本文主要通过对地震剖面及地面露头资料的综合研究 ,重点分析了自晚第三纪以来酒泉盆地的地质结构特征、构造变形特征及下步油气勘探方向 ,并获得以下认识 :南缘山前冲断带构造变形表现为多个逆冲推覆带侧向叠置 ,并且由于调节断层的分割作用 ,构造变形及结构具有明显的东、西分段特征 ,构造变形强度总体表现为西强东弱 ,推覆体广泛逆掩于下白垩统之上 ;南缘山前冲断带石油地质条件优越 ,是盆地内最主要的油气聚集区 ,其中逆冲推覆体下盘掩伏构造是下步油气勘探的主攻方向

 
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