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tectonic相关的网络例句

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The Paleogene tectonic framework in Bohai Bay was controlled by both Mesozoic sinistral strike slip and Paleogene extension resulted from diapiric intrusion of mantle.

中生代左行走滑和早第三纪伸展作用共同控制了渤海海域早第三纪的构造格局。

Located offshore in the South China Sea, Yinggehai basin has a peculiar sedimentary, tectonic and evolution model. As a result, the basin is abundant in hydrocarbon resources. A series of oil/gas fields have been found, that are closely related to fault system and overpressure fluid activity in diapirs area.

莺歌海盆地位于我国南海海域,具有独特的沉积、构造和演化模式,因而烃源丰富,资源潜力巨大,在浅层已经发现了一系列与底辟区的断裂输导系统和超压流体的活动有着密切的联系的气田和含气构造。

As the main research object in this dissertation, DF1-1 dispir is the typical structure in diapirs area in Yinggehai basin. On the basis of analyzed logs, geochemistry materials and a large numbers of seismic profiles, the dissertation has discussed the tectonic stress field since late Tertiary, the distribution regularity of THE fault system and its genetic mechanism in DF1-1, genesis and distribution of overpressure system, characteristics of OFA. The innovative research in the dissertation is about coupling relationship between fault system and OFA.

本文以盆地内底辟区典型的DF1-1构造为重点,采用多学科结合、局部构造解析与区域构造分析结合以及物理模拟与数值模拟结合等方法,在详细解剖钻井、分析化验资料,及有关的地震剖面的基础上,分别探讨了盆地晚第三纪以来的构造应力场;DF1-1底辟构造断裂系统的分布规律及其成因机制;底辟区超压体系的成因、分布、超压流体活动特征。

In Songliao basin, the stronge tectonic inversion occurred in the Late Mingshui Formation, and during the declining of compressive force from the SSE to the NNW, the reactivation of basement faults formed positive inversion faults; released from thermal fluid diapirs, CO2 was migrated upward and then accumulated in inversion structural belts; as the development of fault-style inversion tectonics in the southern part is better than the northern part, and the western is better than the eastern part, CO2 is richer in the south than in the north, richer in the west than in the east in Songliao basin.

松辽盆地强烈的构造反转发生在明水组末期,挤压应力自南南东向北北西方向衰减的过程中,基底断裂复活形成正反转断层,CO2气从热流底辟体中脱出上运而聚集在反转构造带上,断层式反转构造南部比北部发育,西部比东部发育,因此松辽盆地南部比北部、西部比东部CO2气更富集。

The author has made a detailed analysis of the satellite gravity data over Wenchuan, Motuo, Zhongba, Jiashi and Taiwan Areas in China, where earthquakes more than magnitude of 6 took place in recent several decades. It is surprising that the gravity field patterns over these areas are extremely similar, which is characterized by the following features:(1)Paired positive and negative anomaly.(2)Epicenters usually were located between the pairs where the gradient of gravity field was the steepest.(3)The value of positive peak increased and its width decreased at higher order field.(4)The distance between positive and negative peaks varies in different tectonic background.(5)Different styles of crustmantle material diapirism in different stress fields. Geologically, rheological diapirism of high density crustmantle material could be a reasonable explanation to this unique pattern.

笔者详细分析了中国汶川、墨脱、仲巴、伽师和台湾等地的卫星重力资料(这些地区在近几十年来均发生过6级以上的大地震),惊奇地发现,在这些地区,卫星重力场的样式具有极大的相似性,它们表现在:(1)卫星重力场的正负异常值成对出现;(2)震中通常位于重力场峰值间的陡梯度带;(3)由低阶到高阶的重力场正异常的峰值增大而宽度变窄;(4)正、负峰值间的距离随所处的大地构造背景而变;(5)不同应力场壳幔物质底辟的样式不同,从地质上看,高密度壳幔物质的流变底辟作用,可以合理地解释这种独特的样式变化。

The observations and measures on many faults in the Tertiary as well as in the Cretaceous rocks in the Kuqa Depression, Tarim Basin, could help us to reconstruct Late Tertiary tectonic paleostress field by inversing a lot of fault-slip data.

基于对库车坳陷内第三系和同时卷入变形的白垩系中发育断层的野外观测,采用断层滑动数据反演方法,对库车坳陷的第三纪构造古应力进行恢复。

It was floruit of volcanic activity in middle Caledonian between 446 Ma and 440 Ma. Mass volcanic rock was squirted, and ore bearing magma was risen by tectonic fissure, then formed a large-scale valuable polymetallic sulfide orefield.

随着构造岩浆活动的继续,能量的积聚,458.99Ma岩浆熔岩涌出地表,揭开了本区岩浆火山活动事件的序幕。446Ma~440Ma,是本区火山活动全盛时期,在本区大范围内形成有价值的多金属硫化物矿床。

The Ordos craton basin was relatively stable- featured in the following aspects, such as the lithosphere texture, thermal flow, subsidence /sedimentation, and tectonic evolution.

鄂尔多斯克拉通有其稳定的一方面,表现在岩石圈结构、沉积沉降、热流、构造的相对稳定,不仅在克拉通层序的构造沉积稳定,在后期仍然表现为相对稳定。

The research result about abnormal pressure shows insufficiency of compaction disequilibrium as the sole cause of high pore fluid pressures, and tectonic compression, aquathermal expansion, diagenesis, hydrocarbon generation etc also can be the generating mechanisms.

一般认为欠压实是最主要的异常高压成因机制。由于构造挤压引起压应力的改变,由于水热膨胀、成岩作用、烃类生成等引起体积的膨胀,或由于流体流动和浮力作用也可产生异常超压。

According to the varying characters of above information as well as tectonic history and thermal history,it is concluded that the gas migrated from south to north in the primary forming period of Ordos deep basin gas trap.

根据以上信息的变化特征及盆地构造史和地热史分析结果表明,鄂尔多斯盆地上古生界深盆气藏在主形成期时,天然气由南向北运移。

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