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fault dip相关的网络例句

查询词典 fault dip

与 fault dip 相关的网络例句 [注:此内容来源于网络,仅供参考]

The sealing properties of fault are not only related to tectonic stress, but also to strike and dip angle of fault, depth, lithology of each fault wall, and fluid pressure.

断层的开启与封闭,不仅与构造应力直接相关,而且与断层的走向、倾角、深度、两盘岩性及流体压力直接相关。

Thrust fault - a dip-slip fault in which the upper block, above the fault plane, moves up and over the lower block.

冲断层 -断层平面上面的岩体向上运动并压住下面的岩体的一种倾滑断层。

Normal Fault Flash Animation 正向断层Flash动画 thrust fault - a dip-slip fault in which the upper block, above the fault plane, moves up and over the lower block.

冲断层 -断层平面上面的岩体向上运动并压住下面的岩体的一种倾滑断层。

Normal fault - a dip-slip fault in which the block above the fault has moved downward relative to the block below.

正断层-断层上面的岩体相对于下面的岩体作向下运动的一种倾滑断层。

Because the main territorial cap rock which could block off hydrocarbon migration in another side of fault in Paleozoic stratum is huge thick mudstone in upper mbr of Shangshihezi group and Shiqianfeng group, this make only backward fault to dip direction can block to form fault-block trap in the reservoir stratum of carbonatite eluvial horizon in Ordovician and thick sandstone in Permian .

古生界具有侧向封堵条件的区域性盖层主要是上石盒子组上段—石千峰组大套泥岩,这决定了断块区奥陶系碳酸盐岩风化淋滤带及二叠系大套砂岩储层在反向断层遮挡下能形成断块圈闭。

Hechi-Yishan fault zone is located in the north of Guizhong depression, which general strike is NW-EW and consists of a series of obduction fault. Generally, there are two main faults, the fault-fold belt about 5-20km is made of main faults, subsidiary faults and concomitant folds; The dip of main faults is N or S; It can be divided into four different structural sections along its strike (Hechi section, Yishan section, Liucheng section and Yingshan section). There are some differences among these sections in structure characteristic, such as fault structure, associated structure, fold association style, deformation of rock, and so on.

河池-宜山断裂带展布于桂中坳陷北部,总体走向NW-近EW 向,由一系列逆冲断层组成,主干断裂一般为2条,主干断裂与次级断裂及伴随的褶皱构造构成宽5-20km 不等的断褶带;主断裂倾向N 或S;沿走向可分为河池、宜山、柳城、英山四个构造段;各段断裂结构、伴生构造、褶皱组合样式、岩石变形等构造特征存在一定差异。

Firstly, by comparing with the corresponding problems in full space, we applied the BIEs to investigate the features of spontaneous rupture on a planar fault in half space for theoretical numerical models, and obtained some significative results on the roles of asperity radius, critical slip-weakening distance, fault depth, dip angle of fault, initial stress distribution and strength distribution in the rupture propagation processes.

在理论数值模型的研究部分,通过与全空间中断层破裂问题的比较,本文详细地研究了在各种不同的控制参数下半空间中断层破裂过程的特征。

This paper describes laminar small faults affected a number of factors to take specific measures :Pre-stack time migration through the use of technology to improve inter-layer tomography for the accurate identification and de脚本ion interlayer fault lay the foundation;Through meticulous depicts dip scanning technology to small fault;Phase-edge technology frequency bands using a broadband seismic data to better identify the fault system.

本文针对影响描述层间小断层的因素采取了多项有针对性的措施:通过采用叠前时间偏移技术改善层间断层成像,为准确识别与描述层间断层奠定基础;通过地层倾角扫描技术来细致刻画小断层;利用优势频带分频相位技术较好地实现了宽频带地震资料的断裂系统识别。

The main factors influencing the gas preservation condition includes the fault amplitude, fault fragmented intervals, fault surface dip, and the position of fracture cavity system in the faulted zone.

大断裂影响缝洞系统保存条件的主要因素包括:大断裂断距、断层上消失层位、断面倾角、盖层厚度以及缝洞系统所处断裂带位置等。

The shape of the fault He125 in plane was illustrated by using striking, rotation and angle of branch fault. And its profile features include fault horizontal slip, vertical slip, and dip, fault throw and growth index were interpreted by selecting precise points. Based on these features, 3-D structural elements, fault plane system and structural style were studied.

从走向、转度、分支断层间的夹角三个要素入手阐明断层平面形态,通过精确取点利用三角函数解释断层的水平滑距、垂直滑距、倾角、生长指数、古落差等剖面几何要素,研究了河125断层的三维结构要素、断面体系及构造样式。

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