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It suggests that,when considering the reasons of crack′s happening, not only the stress level, but also the friction state, or restriction condiction on the fault is an important factor,too.

说明在考虑地震发生条件时,不能只着眼于应力场是否增强,断层摩擦强度,或更广义地说,构造约束条件的变化也是一个不容忽视的重要因素。

The mechanical strength of the crust and the seismicity of geotectonic units were strongly affected by geothermal characteristics of the units.

研究表明,各主要构造单元的地壳力学强度和地震活动性均受其地热特征的影响。

The Es formation was divided into seven third order sequences based on the seismic, drilling and logging data, and plans deposition system plane distribution maps of different time were plotted by dominance phase principle. The lower Es4 is flood-overlake facies mainly; the upper Es4 is meandering stream and braided river delta deposition above the shore shallow lake background; in the Es3 period, the south mainly developed braided river, meandering stream delta, the northeast area main developed meandering stream delta, the middle area mainly developed semi-deep lakean d deep lake sediments. From lower Es3 to upper Es3, the delta scale gradually increased and the depositional area gradually moved to the east and the southeast; the Es2 period was dominated by shore-shallow lake sediments and widely developed braided river delta and delta deposits; the Es1 period was dominated by shore-shallow lake shoal deposits, and in the south developed meandering stream and braided river delta deposits.The lothological traps of the Shahejie group are mainly fluxoturbidite and stratum lateral pinch-out, and its formation and the distribution of the lothological trap were controlled mainly by the basin structure characteristic, palaeogeomorphology and tectonic activity and so on. It had a beneficial geological condition to develope sublacustrine slump turbidite fans in Jishan, Jiangjiadian and Wawu.

利用地震、钻井、测井等资料,将古近系沙河街组划分出7个三级层序,通过剖面沉积学分析,以优势相原则绘制不同时期各亚段沉积体系平面分布图:沙四下总体以洪水-漫湖沉积为特征,沙四上沉积时期是在滨浅湖背景之上发育了曲流河三角洲和辫状河三角洲沉积;沙三段沉积时期南部主要发育辫状河、曲流河三角洲,西北部地区发育曲流河三角洲,中部地区主要为深湖—半深湖沉积;由沙三下至沙三上,西北部三角洲规模逐渐增大,沉积范围逐渐向东、东南方向推进;沙二段沉积时期为滨浅湖沉积,在背景之上广泛发育了辫状河三角洲和三角洲沉积;沙一段以滨浅湖滩坝沉积为特征,南部发育了曲流河三角洲和辫状河三角洲沉积;沉积地层中的岩性圈闭以滑塌浊积岩岩性圈闭和地层侧向尖灭型岩性圈闭为主,其形成和分布主要受盆地结构、沉积古地貌和构造活动强度等因素控制,北部基山、南部江家店和瓦屋具有发育滑塌浊积扇的良好地质条件。

The comparison analysis of narrow anti wide azimuth seismic data in mountain front areas of Turpan Basin, western China, shows that the observation direction bevelling the direction of faults or fault zones will cause the imaging loss of small faults, and the little fault will be poorly imaged in seismic data.

通过对中国西部吐鲁番盆地北部山前带的宽、窄方位角地震数据进行对比分析研究表明:不同窄方位观测时,由于观测方向与断裂走向斜交存在较为严重的构造假象,并造成小断层难以成像。

Domestic unseating prevention system without design is done as construction measures, which, therefore, can't ascertain the effect of unseating prevention system.

目前国内所采用的防落梁装置一般是作为构造措施,没有经过计算和设计,在地震作用下很难起到真正的防落梁效果。

And expatiate the effect of investigating thick of covering layer, weathering zonation of base rock, position and dip of fault structural belt, and other engineering geological problem using shallower seismic refraction and high density resistivitty.

并结合典型探测资料,阐述了浅层地震折射波法和高密度电阻率法用于调查覆盖层厚度、基岩风化分带及断裂构造带的位置和产状等工程地质问题中的有效性。

On the other hand, the S wave velocity structure shows an EW variation, this distribution feature corresponds to the distribution of epicenters and volcanoes, and the strike of faults.

另外,S波速度结构还反映出这一构造格局呈南北向的空间展布,并且与该区地震震源分布、断裂走向、火山分布有很好的对应关系。

This dissertation focuses on the basin geothermal history, tectonothermal evolution and the relationship between geothermal field evolution and hydrocarbon generation Based on the research of present-day geothermal field, geothermal history of Eastern Subdepression of Liaohe Basin was reconstructed with available data from drillings, loggings, seismic cross-sections, BHTs and thermal indicators

本文综合运用钻井、测井、地震、古温标等数据资料,在现今温度场研究的基础上对辽河盆地东部凹陷新生代热历史进行了恢复。全文以盆地热史研究为主线,进行了盆地构造-热演化分析,并探讨了温度场演化与油气形成之间的关系。

Results show that the Wenchuan earthquake is characterized mainly by thrust motion with right-lateral strike slip also, and two faults-Yingxiu-Beichuan fault and Guanxian-Jiangyou fault participated simultaneously during the rupture process.

结果显示汶川大地震主要是沿龙门山构造带的映秀—北川断裂和灌县—江油断裂发生的逆冲兼右旋走滑破裂事件。

In accordance with features of petrology, sedimentary structure, profile structure, electrofacies and seismic facies, underwater distributary channel, frontal sill-like sand, mouth bar, distal bar, front fan-delta mud and mere mud and so on, were identified, and depositional features of them in detail were discussed respectively.

根据羊邑组二段-三段的岩行学、沉积构造、剖面结构、测井相和地震相等特征,进一步识别出水下分流河道、前缘席状砂、河口坝、远砂坝、前扇三角洲泥和浅湖泥等沉积微相,并详述了各微相的沉积特征。

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然而,正如其名字所指出的那样,CD盘不能写,也不能用任何方式改变其内容。

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