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The Haiyuan earthquake relates to both NS and EW structures extending to the top of the asthenosphere and the movement of the material of the asthenosphere.

海原大地震的发生既与延至软流层顶部的近NS向和近EW向的构造有关,也与软流层的物质活动有关。

The eight major research topics are :①understanding coremantle processes, by deep drilling into a large oceanic plateau in the Western Pacific;②detailed investigation of material circulation during greenhouse Earth, and the transition process from greenhouse to icehouse environments, by drilling Cretaceous to Cenozoic sediments in the Pacific,③understanding the process of continental crust formation by deep drilling into oceanic arc,④Understanding the process of oceanic lithosphere formation by deep drilling of the back arc spreading system,⑤understanding of continentoceanatmosphere linkage, by drilling in the marginal seas and continental slopes of Asia,⑥investigation of the carbon cycle and the deep biosphere in accretionary prisms,⑦investigation of the mechanism and cycles of great earthquakes, tectonics, and mass circulation in convergent plate margins,and ⑧biology of extreme microorganisms living in deep accretionary prism environment.Keywords : Japan IODP Drilling Scientific goals.

其八项研究目标为:①钻探西太平洋洋底高原,认识核—幔作用过程;②钻探太平洋白垩纪—新生代沉积物,详细研究地球温室期间的物质循环及从温室环境到冰室环境的转化过程;③钻探大洋岛弧,认识大陆地壳形成过程;④钻探扩张的弧后,认识洋壳岩石圈形成过程;⑤钻探亚洲边缘海及陆坡,认识陆壳—洋壳—大气圈关系;⑥调查增生楔中的碳循环及深部生物圈;⑦调查汇聚板块边缘大地震周期及形成机制、构造及物质循环;⑧研究生活于增生楔环境中极端微生物生物学。

Based on the seismicity of intracontinental subduction zone on both sides of Tianshan range, integrating the structural study in this paper with the existing Chinese and international geophysical research results, the author proposes a geodynamic model to explain the complicated Late Cenozoic intracontinental deformation of Central Asia.

通过对天山南北两侧陆内俯冲带地震活动特征的综合研究,结合前人的地球物理研究以及本文对库车再生前陆逆冲带构造研究的结果提出了一种解释晚新生代中亚地区陆内变形过程的地球动力学模型。

Direct observations and measurements on deformational and sedimentary structures, fluid activities, physical properties, and chemical compositions of core samples from accretionary prisms at different pressure and temperature settings are critical to understanding seismogenic mechanisms of subduction zone earthquakes.

对增生楔不同压力-温度条件下的构造变形、流体活动、沉积特征、岩石物性和化学组成等多方面的直接观测,可以帮助分析俯冲带地震的蕴育和发生的环境与机理。

Based on the whole, dynamic and synthetical basin analytical methods, the structural characteristic of the South Ordos basin in the Late Mesozoic and the Cenozoic is researched with the data of seismic, geological and former achievements. In order to discuss deeply to the geodynamical background of Ordos basin and study the dominant factors controlling the sediment evolvement of the basin, we discusses the evolvement of basin from an even more extensive view.

采用&整体、动态、综合&的盆地分析方法,根据地震、地质等资料,结合野外地质及前人研究成果,对鄂尔多斯盆地南部中-新生代以来后期改造特征进行了研究,深入探讨控制鄂尔多斯盆地形成演化的地球动力学背景,研究盆地构造沉积演化的主控因素。

The geological and geophysical data show that in the lower crust of young continental tectonic units may occur pervasive, non-seismic, subhorizontal and ductile flow related to thermal softening. The laminar flow drives fault-block movement of the upper crust, results in the formation of orogenic belts and sedimentary basins, and causes coupling between ductile lower crust and brittle upper crust/mantle.

大量的地质和地球物理资料表明,年轻的大陆构造活动区的下地壳可能因热软化而出现透入性非地震式顺层韧性流动,这种下地壳层流作用驱动大陆上地壳发生地震式脆性断块运动,形成盆山格局,发生圈层耦合。

To better understand the regional tectonics, we have inverted local and teleseismic broadband waveform data to determine the focal mechanism of this earthquake.

为了更好的认识区域构造,我们利用近震及远震波形反演的方法得到了此次文安地震的震源机制。

When the shockwave energy weakened, mountain collapse often occurs in the ringed mountain, particularly in the previously steeper inside, while plagioclase slope slide (primary meteorite-stricken slope slide) occurs in the outside mountain, and the mountain structure is constantly adjusted in aftershocks to achieve the gravity balance; during the long geological ages after the formation of meteorite crater, under the action of erosive transit and dryness and humidity of hydrosphere and air current, volcano and earthquake activities, etc., the physiognomy gradually reverts to the original state.

在冲击波能量减弱时,环形山原来较陡峭的内侧多发生山体崩塌,外侧山体发生斜岩滑坡,在余震中山体构造不断调整以达到重力平衡;在漫长的地质年代里,陨击坑成型以后,在水圈、大气环流的侵蚀搬运、寒暑燥湿、火山和地震等因素作用下地貌逐步趋于还原。

When the shockwave weakened, landslides often occurs in the ringed mountain, particularly in the previously steeper inside, while plagioclase avalanche (primary meteorite strike landslide) occurs in the outside mountain, and the mountain structure is constantly adjusted in aftershocks to achieve the gravity balance; after the formation of meteorite crater, during the long geological ages, under the action of hydrosphere, erosive transit and dryness and humidity of air current, volcano and earthquake activities, etc., the landform gradually reverts and returns to the original state.

在冲击波能量减弱时,环形山原来较陡峭的内侧多发生山体崩塌,外侧山体发生斜岩滑坡,在余震中山体构造不断调整以达到重力平衡;在漫长的地质年代里,陨击坑成型以后,在水圈、大气环流的侵蚀搬运、寒暑燥湿、火山和地震等因素作用下地貌逐步趋于还原。

In viewpoint of the lack of enough basic data of foreign oilfields, under the conditions of insufficient core data, no constrains of seismic interpreted cross and fault data, the rational fine 3D geological model has been established by fine oil reservoir characterizing technique including the contrast results of individual layers, second well logging interpretation and so on.

针对国外油田多数基础资料不全,必须在缺乏取心资料,无地震解释层面及断层数据约束的条件下,运用层序地层学小层对比结果和二次测井解释等精细油藏描述技术,并插入虚拟井控制井间构造,进而建立了合理的精细三维地质模型,为该油田的储层预测及数值模拟提供了基础数据,并在实际应用中取得了良好效果。

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