8级特大地震前地震活动平静特征——以中国大陆西部近期2次8级地震为例     

陈玉华  马震 《高原地震》2008,20(4):1-7

中强地震平静图像已被许多研究者认为是强震前的一个典型异常指标。近期中国大陆西部2次8级地震前地震活动图像的研究认为,8级特大地震前不仅中强震出现大面积平静,而且中小地震也会出现大规模平静现象,形成地震空区。震前依据震级由大而小逐级形成配套出现的地震空区,可作为中国大陆西部8级特大地震的中短期预测与8级地震发生地区的判定的一项有实际意义的指标。  相似文献   

Stretching characteristics and its dynamic significance of the northern continental margin of South China Sea   总被引：5，自引：0，他引：5  

Zhang YunFan  Sun Zhen  Zhou Di  Guo XingWei  Shi XiaoBin  Wu XiangJie  Pang Xiong 《中国科学D辑(英文版)》2008,51(3):422-430

To investigate the thinning of the whole crust, and the contribution of the upper versus lower crust to the stretching since Cenozoic, we calculated the stretching factor of the northern margin of South China Sea with data such as whole crustal thickness, depth of Cenozoic sedimentary basement and the horizontal displacement of faults. An isometric line drawing on whole crustal stretching factor is then obtained. Along the seismic Line 1530 in Baiyun sag, we also calculated the stretching factors of the upper and lower crust. The results suggest that the whole crustal thickness decreases seaward while the whole crustal stretching factor increases from shelf to slope. The Moho upwells highest beneath where the crust is thinned most. The value of the whole crustal stretching factor ranges from 1.5 to 6. Two areas were thinned intensely: the center of Yinggehai Basin, and the Baiyun sag in the Pearl River Mouth Basin. The calculation of the upper and lower crustal stretching factors from DSP1530 in Baiyun sag shows that the original crust of Baiyun sag should be thinned before deformation. Its pre-Cenozoic evolution as well as tectonic position during Cenozoic might be responsible for that.  相似文献   

Mesozoic paleogeography and tectonic evolution of South China Sea and adjacent areas in the context of Tethyan and Paleo-Pacific interconnections   总被引：4，自引：0，他引：4  

Di  Zhou  Zhen  Sun  Han-zong  Chen  He-hua  Xu  Wan-yin  Wang  Xiong  Pang  Dong-sheng  Cai  Deng-ke  Hu 《Island Arc》2008,17(2):186-207

Abstract   During the Mesozoic era, the South China Sea and its environs were located at the south-eastern margin of the Eurasian continent. There has been hot debate on the influences of Tethyan and Paleo-Pacific tectonics to the Mesozoic evolution of the area. This paper compiles lithofacies maps of six time slices and discusses the paleogeographic and tectonic evolution of the area based on this compilation and other data on structural deformation and magmatism. In the Early Triassic, the Paleotethys Ocean extended eastward to the study area through the Song Da passage. Then a significant east–west differential evolution began. In the Late Triassic, the western area uplifted as a result of the collision between the Indosinian and South China blocks during the Indosinian orogeny, and the Song Da passage has closed since then. Meanwhile, a transgression of Paleo-Pacific waters occurred in the eastern and south-eastern portions of the area, forming the 'East Guangdong–North-west Borneo Sea'. In the Early Jurassic, seawater transgression was even more pronounced, resulting into the connection of this sea with the Mesotethys Ocean to the west. Large quantities of Tethyan water carrying Tethyan organisms entered the area. In the Middle Jurassic, a short-lived transgression occurred in the eastern Mesotethys and resulted in the formation of the 'Yunnan–Burma Sea'. The Late Jurassic to Early Cretaceous was the climax of the subduction of both the Mesotethys and Paleo-Pacific towards the Eurasian continent. This led to the formation of the great 'Circum South-east Asia Subduction–Accretion Zone' in the Middle or Late Cretaceous. This paper also presents various lines of evidence for a newly recognized segment of this Mesozoic subduction–accretion zone buried under Cenozoic sediments in the north-eastern South China Sea.  相似文献   

降雨作用下碎石土滑坡解体变形破坏机制研究   总被引：16，自引：3，他引：13  

许建聪  尚岳全 《岩土力学》2008,29(1):106-112

为了揭示碎石土滑坡的变形解体破坏机制,结合工程实例,通过资料搜集整理和分析、现场工程地质调查与勘探和室内外的物理力学试验,采用不平衡推力法、数理统计分析方法和三维弹塑性接触有限元算法,以及运用碎石土边坡地下水管网状排泄系统理论,分析降雨作用下碎石土滑坡的变形解体破坏过程,揭示了降雨作用下中深层碎石土滑坡变形解体破坏的主要机制和一般的力学机制。结果表明,一定强度的长时间连续降雨或强降雨是中深层碎石土滑坡发生失稳的主要触发因素;采用考虑降雨作用的弹塑性接触有限元算法,可以更好地反映该类型滑坡在降雨作用下所处的实际状态及滑坡的滑动过程,可以为该类型滑坡稳定性的准确评价和预测预报提供可资借鉴的方法。  相似文献   

川口油田长6储层成岩作用   总被引：2，自引：0，他引：2  

薛军民  解伟  王震  张林 《吉林大学学报(地球科学版)》2009,39(6):1007-1012

详细分析了川口油田长6储层的成岩作用类型、储层物性演化及影响因素。通过岩石学、铸体薄片、电镜扫描等研究方法说明川口油田长6储层主要成岩作用包括压实-压溶作用、胶结作用、交代蚀变作用及溶蚀作用等,成岩阶段属晚成岩A期。其中,机械压实作用、化学胶结作用是导致砂岩孔隙度降低、储集性能变差的主要因素。机械压实作用主要表现为软碎屑的塑性变形、颗粒间由点接触向凹凸接触演变;胶结作用表现为浊沸石、绿泥石、粘土矿物、碳酸盐胶结;石英和长石的次生加大、溶蚀作用特别是浊沸石的溶蚀在一定程度上提高和改善了砂岩储集性能。结果表明,影响储层物性的主要因素为沉积作用和成岩作用。  相似文献   

曲线简化中节点重要性度量方法比较及垂比弦法的改进   总被引：2，自引：1，他引：1  

邓敏  陈杰  李志林  徐震 《地理与地理信息科学》2009,25(1)

在曲线简化过程中,一个最基础的问题是如何度量曲线上节点的重要性程度.该文简要回顾了现有的一些节点重要性度量方法,即角度度量法、面积度量法、弧比弦度量法和垂比弦度量法,指出其局限性.结合弧比弦度量法与垂比弦度量法的优点,提出了一种改进的垂比弦度量方法,并给出具体的评价方法.最后,根据曲线简化实验结果,发现相比于弧比弦度量法.改进后的垂比弦度量法选取的节点能较好地保持曲线的形状.  相似文献   

库姆塔格沙漠大尺度风场特征分析   总被引：4，自引：4，他引：0  

曾晓青  王式功  尚可政  杨德保  曾淑玲 《中国沙漠》2009,29(3):391-396

利用美国NCEP/NCAR1979—2006年27 a地面10 m高度的日平均风场再分析-2资料以及46 a的地面常规气象站观测资料和1 a的沙漠中自动气象站观测资料,对库姆塔格沙漠地区风场进行了统计与诊断分析。结果表明：沙漠地区,一年四季北风和东北风为近地面主要存在的风向,春季风速最强,夏季次之,秋冬季最弱;在夏秋冬季节,由于北风的逐渐减弱,加上受到南侧阿尔金山和青藏高原风场的影响,南下的气流在沙漠南侧分为三支,分别流入新疆、青海和甘肃。春夏季节在沙漠北侧基本都是以东北风或者西北风吹向库姆塔格沙漠,秋冬季节,沙漠地区出现西南风。根据沙漠周围6个气象站风场风速显示,库姆塔格沙漠地区风速存在明显的周期变化,在过去的10多年中库姆塔格沙漠周围风场风速处于一个低谷期,但最近几年风速有不断加强的趋势。  相似文献   

沿高度变刚度复合墙板结构弹塑性分析     

姜南  王真 《地震工程与工程振动》2009,29(3)

本文研究沿高度变刚度混凝土灌芯纤维石膏墙板结构(以下简称复合墙板结构)在水平荷载作用下的受力机理,建立简化计算模型,推导出了复合墙板结构的受力破坏路径,并建立了各阶段内力计算方法及计算公式。通过实例计算,得到沿高度均匀结构以及非均匀结构在水平荷载情况作用下位移的曲线与非均匀结构的受力破坏路径。结果表明,沿高度适当改变灌芯方式,侧移曲线更趋合理;各区段结构破坏路径均是石膏板先开裂且先达到极限状态。  相似文献   

Spatio-temporal point pattern analysis on Wenchuan strong earthquake     

Peijian Shi Jie Liu    Zhen Yang Agricultural College  Jiangxi Agricultural University  Nanchang  China China Earthquake Networks Center  Beijing  China 《地震学报(英文版)》2009,(3):231-237

For exploring the aftershock occurrence process of the 2008 Wenchuan strong earthquake, the spatio-temporal point pattern analysis method is employed to study the sequences of aftershocks with magnitude M≥4.0, M≥4.5, and M≥5.0. It is found that these data exhibit the spatio-temporal clustering on a certain distance scale and on a certain time scale. In particular, the space-time interaction obviously strengthens when the distance is less than 60 km and the time is less than 260 h for the first two aftershoc...  相似文献   

薄油层时移地震差异波形特征探讨   总被引：1，自引：1，他引：0       下载免费PDF全文

王大伟  刘震  陈小宏  吴时国 《地球物理学进展》2009,24(1):170-175

开发导致的时移地震差异代表了油藏的岩石物理性质变化,本文从差异波形角度出发,明确了声波阻抗界面的反射系数与油层声波阻抗变化之间的函数关系,进而分析薄油层时移地震差异波形特征.通过分析得出,开发前后油层阻抗变化越大,时移地震的差异振幅幅度越大;薄油层的差异波形特征仅与油层的声波阻抗变化有关,油层声波阻抗增大导致与地震子波微分形式相同的差异波形,油层声波阻抗减小产生的差异波形与180°相位的地震子波微分形式相同;油层声波阻抗变化方向导致差异波形振幅幅度变化的快慢.  相似文献