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221.
通过对多自由度体系结构在地震作用下的能量分析,考虑地震动因素和结构自身特性,提出一种框架结构地震总输入能量的简化求解方法.实例计算结果表明:基于等效单自由度体系来估计多自由度体系的地震总输入能,是一种计算简便且较为准确的方法. 相似文献
222.
Forced regression and its sedimentary response to continental lacustrine rift basin: A case of the Member 3 of Shahejie Formation in Laizhouwan sag,Bohai Bay Basin 下载免费PDF全文
Falling stage systems tract(FSST)is an offlap strata with strong relationship with hydrocarbon exploration,which is driven by relative lake-level fall and developed above the highstand systems tract and below the lowstand systems tract of a new sequence. It has no relationship with sediment supply. Based on the theory of sequence stratigraphy and sedimentology,3D seismic data,drilling core data,and well-logging data were comprehensively analyzed. The study showed that the FSST strata was formed in the Member 3 of Shahejie Formation in the Laizhouwan sag. The FSST can be divided into three units,namely as units P1,P2,and P3 from bottom to top. The P1 is the first unit of progradation downlap the bottom of the FSST. The top of the unit P3 is a sequence boundary exhibits subaerial unconformity. The seismic profile along the source direction is characterized by the low-angle oblique progradation reflection that downstream the center of lake basin from west to east. Incised valleys developed on the top of the FSST perpendicular to the source direction. Gamma-ray logging response is manifested by a series of funnel-shaped complex,indicating that the sedimentary response of the FSST was a cycle of coarsening-upward parasequence sets. Comprehensive studies on core interpretation and well-logging analysis showed that the FSST was a fluvial-delta sedimentary system with slumped fan deposits associated with the delta front. Consequently,the FSST is a common result of relative dry climate and falling of lake level,considering regional tectonic evolution,sediment supply,and paleo-climate change. The discovery of the FSST in the Laizhouwan sag has an important geological significance for the sedimentological interpretation,and it offers a guidance for further oil exploration in the study area. In addition,it also serves as a significant reference for future research on the FSST development and exploration in the continental lacustrine rift basin. 相似文献
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On the migration of a system of protoplanets 总被引:1,自引:0,他引:1
W. Kley † 《Monthly notices of the Royal Astronomical Society》2000,313(4):L47-L51
The evolution of a system consisting of a protoplanetary disc with two embedded Jupiter-sized planets is studied numerically. The disc is assumed to be flat and non-self-gravitating; this is modelled by the planar (two-dimensional) Navier–Stokes equations. The mutual gravitational interaction of the planets and the star, and the gravitational torques of the disc acting on the planets and the central star are included. The planets have an initial mass of one Jupiter mass M Jup each, and the radial distances from the star are one and two semimajor axes of Jupiter, respectively.
During the evolution a joint wide annular gap is created by the planets. Both planets increase their mass owing to accretion of gas from the disc: after about 2500 orbital periods of the inner planet it has reached a mass of 2.3 MJup , while the outer planet has reached a mass of 3.2 M Jup . The net gravitational torques exerted by the disc on the planets result in an inward migration of the outer planet on time-scales comparable to the viscous evolution time of the disc. The semimajor axis of the inner planet remains constant as there is very little gas left in its vicinity to induce any migration. When the distance of close approach eventually becomes smaller than the mutual Hill radius, the eccentricities increase strongly and the system may become unstable.
If disc depletion occurs rapidly enough before the planets come too close to each other, a stable system similar to our own Solar system may remain. Otherwise the orbits may become unstable and produce systems like υ And. 相似文献
During the evolution a joint wide annular gap is created by the planets. Both planets increase their mass owing to accretion of gas from the disc: after about 2500 orbital periods of the inner planet it has reached a mass of 2.3 M
If disc depletion occurs rapidly enough before the planets come too close to each other, a stable system similar to our own Solar system may remain. Otherwise the orbits may become unstable and produce systems like υ And. 相似文献
227.
长白山及邻区地壳、上地幔顶部三维速度结构 总被引:2,自引:0,他引:2
根据沿长白山布设的宽频带流动地震台站及吉林省地震台网所记录的近震P波走时数据,利用层析成像方法对长白山及邻区(39°N-45°N、122°E-130°E)深至40 km的地壳和上地幔顶部三维速度结构进行了研究。结果表明:地震的发生和分布多集中于断裂等复杂地质构造。利用较高分辨率的地壳、上地幔顶部三维速度结构证实了长白山火山区岩浆囊存在,并推测岩浆囊的位置位于火山口的西南方向,深度为10~40 km。壳内岩浆囊分布对进一步解释、认识火山灾害提供了重要的深部信息。 相似文献
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鄂尔多斯盆地是我国西北地区东部的一个大型构造沉积盆地,蕴藏着丰富的矿产资源,是我国正在建设 的重要能源基地;鄂尔多斯盆地同时也是一个巨型地下水盆地,赋存相对丰富的地下水资源,将为能源基地建设提 供重要水源。鄂尔多斯盆地是由多种不同类型岩石上下叠置构成的构造沉积盆地,因此它也是一个由不同含水岩 类的多个含水层系统上下叠置构成的巨型地下水盆地。鄂尔多斯盆地总体上构成一个半开启型的地下水盆地,盆 地内不同含水层系统地下水交替循环的方式和深度不同,以寒武系-奥陶系碳酸盐岩类岩溶含水层系统和白垩系 碎屑岩类孔隙-裂隙含水层系统的交替循环深度较大(可达1200~1800m);新生界松散岩类孔隙含水层系统和 石炭系-侏罗系碎屑岩类裂隙含水层系统的交替循环深度较小(一般小于300m)。鄂尔多斯盆地实际上包含了周 边岩溶地下水、白垩系自流盆地地下水和东部黄土区地下水共3个地下水大系统。 相似文献
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西部水资源与生态环境建设 总被引:11,自引:0,他引:11
水不仅是西部经济发展的主要制约因素、山川秀美的重要保证,而且是西部脱贫致富的希望所在,调整能源结构的重要途径。本文在分析我国西部水资源基本态势的基础上,讨论了水资源开发的主要问题,并结合中国工程院“西北地区水资源配置、生态环境建设和可持续发展战略研究”项目,探讨了西部水资源与生态环境建设。 相似文献
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