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地壳断裂

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The Earth crust activity of different geotectonic elements could be estimated with the fracture fractal dimension.

利用断裂尺度分布的分形维数值的大小,可以定性判断不同大地构造单元的地壳稳定性。

The Earth crust activity of different geotectonic elements could he estimated with the fracture fractal dimension.

利用断裂尺度分布的分形维数值的大小,可以定性判断不同大地构造单元的地壳稳定性。

Fault controlled not only the evolution and the transverse inhomogenity of regional tectonics, but also the laminary structure of the earth crust-lithosphere.

断裂以不同形式产出于地壳~岩石圈的表层、中深层和深层,其规模小到以毫米计或更小尺度,大可到全球范围。

We divide the evolution of becoming rocks into four periods: early region's metamorphic process and mixed lithifaction,sedimentation and becoming rocks process in middle and late Proterozonic Era and in the Paleozonic Era,trasformation process of burial hill layers in earth shell'uplift period in the Mesozonic Era, and transformation process to burial hill in the Cenozonic Era.

将储层的成岩演化划分为四个阶段:即早期区域变质作用和混合岩化作用、中晚元古代和古生代沉积成岩作用、中生代地壳抬升阶段潜山地层的改造作用和新生代断裂对潜山的改造作用。

These characteristics suggest that the magma originated by partial melting of the lower crust. The rock mass rose and was emplaced rapidiy along fault in a post-orogenic extensional environment,and the magmatic differentiation was incomplete.

地球化学特点表明岩浆由下地壳部分熔融产生;岩体是在造山后伸展构造环境中沿断裂快速上升定位,分异作用不完全状态下形成。

Between the two LVZ, near surface and in upper crust, there may be fracture zone, which is the channel for the thermal fluid in the deep to move upward.

地表低速区可能有断裂通道与上地壳低速区相连。

Based on the result of numerical modeling, thought that main power-source of the plateau uplift is driving and compressing of Indian plate toward NNE, a series of folding and uplifting of the crust successively appeared from the south to the north, and these folds and uplifts possessed a sequence and consequence on the plane and section.

根据数值模拟结果认为,青藏高原隆升的主要动力源是印度板块NNE方向的推挤力,地壳层依照自南而北的次序逐步产生一系列褶皱隆起,从平面、剖面上均具有密切的时序因果关系;高原隆升与活动构造的发育、分布具有密切关系,断裂活动强度自南向北递进式扩展,因此,祁连山脉是高原最年轻的新生活动山链。

Pliocene-Quaternary faulting in grabens around the Ordos block displays predominantly normaldip slip displacements with a right-lateral or left-lateral slip component,indicating a NW-trending extension.

鄂尔多斯周缘地堑系上新世~第四纪的断裂作用表征为以正向倾滑活动为主,同时具有右旋或左旋走滑分量的运动型式,指示了NW-SE向地壳引张作用。

The relationships between large igneous rock province, mantle plume and petroleum show that there is a low velocity-high conductive layer of mid-crust in the basin and this layer is the main source of oil and gas. Weathered granites and volcanic rocks are the best reservoir beds for hydrocarbon accumulation and the faults are the main migration pathway. It is suggested that granite and volcanic reservoirs be the future exploration targets.

通过研究花岗岩和火山岩油气藏的形成模式,指出大火成岩省、地幔柱与油气的关系表明盆地中地壳的低速-高导层可能是油气的主要来源,而花岗岩、火山岩的风化壳是油气成藏的最佳储集层,断裂则是其最主要的运移通道,花岗岩和火山岩油气藏将是未来勘探的重要目标。

The earthquakes at 30-40km depths in the mantle anomalous area of the west Tien Shan reveal a possibility of brittle failures within the mid-lower crust and that means that some faults can extend into greater depths.

天山西部地幔异常区30-40km深度的地震活动和高速异常表明地壳中下层结构仍然具备发生脆性破裂的可能性,推测浅表层的断裂有可能延伸到更大的深度。

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索夫农 、森那库斯和苏格拉底式的对话采用的模仿没有一个公共的名称;三音步诗、挽歌体或其他类型的诗的模仿也没有——人们把&诗人&这一名词和格律名称结合到一起,称之为挽歌体诗人或者史诗诗人,他们被称为诗人,似乎只是因为遵守格律写作,而非他们作品的模仿本质。

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交际能力和语法的关系应该是目标与途径的关系。

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这不是纸上谈兵式的交易,这是人与人的业务,而且涉及金额巨大。