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tectonic相关的网络例句

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Jurassic Tectonic Revolution in China and New Interpretation of the Yanshan Movement;2. The Indo-Chinese movement and Yanshan movement were two important tectonic movements in the Mesozoic era.

中生代印支运动和燕山运动是对济阳坳陷有重大改造的2次构造运动,印支期主要发育NW向逆推断层,燕山早期则为逆断层向正断层的过渡阶段,燕山中、晚期NW向断层发生构造反转,由逆断层转换为正断层。

The Geopark is situated at the junction of the north east trending Yanshan tectonic belt and the north-north east trending Taihanshan tectonic belt ,and is one of the typical intracontinental orogenic belts in China having complicated geological background.

园区地处北东向燕山构造带和北北东向太行山构造带衔接区内,是我国陆内造山带的典型地区之一,具有复杂的地质背景。

The preservation conditions of oil-gas reservoir about rift-subsidence basins inc lude tectonic evolution of basin, sealing histor y of faults after the accumulation of oil and gas, tectonic uplift and denudatio n, magmatic activity,dynamics of ground water, seal of cap rocks, a nd seal of the major faults, etc.

以盆地构造演化史研究为基础,对成藏期以后断裂的封闭史、构造抬升剥蚀、岩浆活动、地下水活动、盖层封闭和控油断层封闭进行了定性和定量分析,总结了断陷盆地油气藏保存条件的研究内容和以模糊评判为主的评价方法。

It is overall a monoclinal structure dipping to south, on which three group faulted structures with the directions of E-W, NEE, and NE-SW are developed, and they are tensional faults. The Orinoco heavy oil belt has been divided into two tectonic zones by one regional fault with the trend of NE in the plane, and the characteristics are different in the two tectonic zones.

奥里诺科重油带是目前世界上唯一一个还基本未开发的大规模重油富集带,它位于东委内瑞拉盆地边缘隆起带,总体是一北倾单斜,其上主要发育E-W向、NEE向和NE-SW向三组断裂,且以张性断裂为主,其中有一条北东向区域性大断裂将奥里诺科重油带在平面上划分为两大构造区,其各自的构造特征不同。

Tectonic subsidence play dominant role in their geometric shapes, basin fillings, sequence evolution and sediment distribution in the Wushi Sag. Outline of the sequences are in shape of box-wedge or sheet-wedge and boundaries of sequences are varied from bilateral fault to monoclinal fault overlap, so that the sequences show distinct semigrabens which overlay in different ways. Seven sequences were formed in different stage of tectonic evolution. The sequence of SQ1 formed in initial rift stage and deposited alluvial sequence. Sequences SQ2-SQ4 developed in intense rift stage and sediment lacustrine sequence. Sequences SQ5-SQ7 formed in late period of rift before thermal subsidence and deposit mere and delta sediment. The place adjacent to the synsedimentary fault is the subsidence center and depocenter; meanwhile, controlling fracture migrates in horizontal made subsidence and sedimentary center of the sag changed.

构造沉降是控制层序几何形态,充填叠置方式、演化及沉积体系分布的最重要因素:凹陷由多个半地堑在不同层序发育时期以不同方式叠置联结而成;受断层控制,层序外部形态有箱状-楔形、楔形-席状披覆型,边界终止方式有双断终止型、单断终止超覆型;不同构造演化阶段层序内部充填的沉积体系各具特征,初始断陷阶段的SQ1沉积冲积层序,强烈断陷阶段的SQ2-SQ4充填湖相层序,晚期断陷阶段SQ5-SQ7内部充填浅湖和河流三角洲沉积;同沉积断层陡坡带沉降迅速、可容纳空间快速增长,是凹陷的沉积和沉降中心,断陷期主控断裂活动时间和空间的变化导致了凹陷沉积和沉降中心的迁移。

On the basis of plan form and crosscutting relationship of the faults, two kinds of tectonic systems were developed in Wu-Xia area, one was strike north-east, and another was strike east-west, the first was developed early and control the structural framework of Wu-Xia area, after that three times longitudinal compress action was happed. According to the intensity of tectonic deformation, The Wu-xia faulted zone from north to south can be divided into the thrust faulted belt, the fault fold belt and the monocline belt. from east to west have three regulatory faults, Wuerhe fault fold belt, Wuxia thrust faulted belt and Xiahong fault fold belt. Base on that 9 secondary structural unit can be divided.Structural accommodation zone and the distribution of reservoir strata have intimate business connection. Usually, Structural accommodation zone was the source zone of arenaceous sediment. The Wu-xia faulted zone have 3 kinds of structural accommodation, concordant approach, concordant overlap and concordant colinearity.

首先研究本区的构造特征,根据断裂的平面形态及相互切割关系,乌夏地区发育两种构造体系:北东向构造体系和近东西向构造体系,前者形成早,控制了该区的构造格局,晚期有3次近南北向挤压作用叠加;乌夏地区南北根据构造变形的强度不同分为冲断带、断褶带、单斜带,东西由于横向调节断层的存在分为乌尔禾断褶区、乌-夏冲断区和夏-红断褶区,进一步划分为九个次级单元;构造调节带与储集层的分布关系密切,通常是大量富砂质沉积的源区,乌夏地区发育三种类型的构造调节带:同向接近型、同向叠覆型和同向共线型。

We summarized the ages of the tectonic events in this area and study the nappe and the strike-slip event of East-TianShan using ~(40)Ar/~(39)Ar method.Therefore,we further understand the Paleozoic tectonic evolution in Tianshan and adjacent areas.

2总结了区内构造事件的年代学成果,并对东天山地区的推覆及走滑事件进行了~(40)Ar/~(39)Ar年代学研究,对天山及邻区古生代构造演化取得了更深入、更全面的认识。

Trace elements in granite tectonic discriminate diagram shows that it is a post-collisional granite, and indicates that the end of Late Carboniferous orogenesis in Kalamaili region and the start of plate tectonic evolution.

花岗岩微量元素构造判别图显示它是一种后碰撞花岗岩,标志卡拉麦甲地区在晚石炭世造山作用的结束和板内构造演化的开始。

Hutuo group of greenschist facies of the mainly sedimentary rocks appears a tectonic style of the huge invert-fan synclinorium in Wutaishan, illustrates the material components of the above crust and inner continental orogenesis. It is a typical example of the tectonic—magma event in the world at 2100—1800Ma, would be a new research hot after Rodinia.

以沉积岩为主的绿片岩相变质的滹沱群,在五台山的构造样式为巨型反扇形复式向斜,代表上地壳的物质组成和陆内造山作用,是研究全球范围内的2100-1800Ma的构造岩浆事件的典型实例,有望成为继Rodinia超大陆研究之后新的研究热点。

In the Triassic-early Jurassic, the emplacement mechanism of monzonitic granite and orthoclase granite is dominated by tectonic extension and the diapirism is strong. The strong balloon swelling is dominant and tectonic extension is subordinate during the emplacement mechanism of early Jurassic alkali granite.

晚三迭世-早侏罗世二长、正长花岗岩体就位过程中构造扩展机制起主导作用,岩浆底辟作用也较强;早侏罗世碱性花岗岩体岩浆就位过程中以强力的气球膨胀作用为主,构造扩展机制为辅。

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