GPS measurements (2003–2006) in the Sikhote Alin network,the Far East     

V. Yu. Timofeev  P. Yu. Gornov  D. G. Ardyukov  Yu. F. Malyshev  E. V. Boiko 《Russian Journal of Pacific Geology》2008,2(4):314-324

This paper considers results of geodynamic studies using the GPS method in the territory of the Far East. GPS measurements using TRIMBLE-4700 geophones were launched along the Sikhote Alin profile in 2003. The technology of the GPS measurements and the problems of selecting the measurement sites and network configuration with reference to the region’s structure are discussed. The results of GPS measurements in 2003–2006 were used to study the fault system of the Far East continental margin. Different models of the Eurasia rotation (from the known NNR-NUVEL-1A to the recent ones) were analyzed. The solid-body rotation of Eurasia was predicted in the framework of the AR-IR-2006 model with a pole located at 51.045°N latitude, 255.842° longitude and rotating at a rate of 0.2423°/Ma. The parameters of the Amur plate rotation were preliminarily estimated (57.6° ± 0.5°N, 117.1 ± 0.5°E, and 0.083° ± 0.004°/m.y) using results on the Sikhote Alin and Transbaikalian network.  相似文献   

Spreading change of Africa–South America plate: insights from space geodetic observations     

Shuanggen Jin  J. Wang 《International Journal of Earth Sciences》2008,97(6):1293-1300

The results derived from geological data show that the half-spreading rate between the African and South American plates has remained relatively constant at 2 cm/year over the past 80 million years (Silver et al. in Science 279:60–63, 1998). In this paper, we have reestimated a new relative angular velocity of Africa–South America plates using the selected space geodetic station data through a new method. Our angular velocity estimates the spreading rates of Africa–South America plate over several years that are similar in azimuth but significantly slower in rate than the NUVEL-1A predictions averaged over the past 3 million years. The implied rates of deceleration coincide with longer-term trends over the past 35 million years and may reflect the effects of plate interaction and coupling of Africa–South America plates. An erratum to this article can be found at  相似文献   

塔里木板块上元古界阿勒通沟组和黄羊沟组: 新识别的冰期和间冰期？   总被引：3，自引：2，他引：1  

寇晓威  王宇  卫巍  何金有  徐备 《岩石学报》2008,24(12):2863-2868

通过库鲁克塔格地区孜厄肯—厄格孜达坂一带实测地层剖面研究重新建立了阿勒通沟组和黄羊沟组的地层层序。阿勒通沟组含三层冰成杂砾岩,为冰川沉积与滨-浅海沉积交替发育,代表海相环境下的冰川沉积。黄羊沟组底部白云岩具负的δ¹³C同位素值,下部以火山岩、上部以细碎屑岩和碳酸盐岩为主,沉积环境具有向上变深的特征,代表了阿勒通沟冰期结束后温暖环境下的海平面上升。结合冰成杂砾岩的特征、“盖帽碳酸盐岩”的分布、碳同位素和化学蚀变指数方面的证据,可将两者分别确定为独立的冰期和间冰期,并分别沿用阿勒通沟冰期和黄羊沟间冰期的称呼。阿勒通沟冰期的划分使得库鲁克塔格地区晚元古代冰期达到四次。根据库鲁克塔格地区已有的同位素年龄,阿勒通沟冰期可能与Sturtian冰期对比,贝义西冰期可能与Kaigas冰期而不是与Sturtian冰期对比。  相似文献   

珠江三角洲晚第四纪垂直构造运动速率   总被引：8，自引：1，他引：8       下载免费PDF全文

陈伟光  赵红梅  常郁  卢邦华 《地震地质》2001,23(4):527-536

根据珠江三角洲 16 6个第四纪古三角洲沉积物的测年数据 ,在扣除了古海平面变化、沉积层的压实效应和地壳静力均衡沉降等非构造因素的影响后 ,估算出晚第四纪以来三角洲地区的垂直构造运动速率。估算按北东、近东西和北西向 3组断裂所切截的 11个断块构造区分别进行。结果表明 ,位于三角洲南部的斗门断块和中部的广州 -番禺断块的活动速率相对较高 ,这个特征得到了三角洲晚第四纪古地理演变、断层活动年代学和地震活动研究的初步验证  相似文献   

地震动加速度过程的小波模拟   总被引：3，自引：0，他引：3  

谢异同  张同亿  吴敏哲 《地震工程与工程振动》2001,21(2):19-23

本文应用基数B－样条小波模拟地震动加速度过程，将小波分析引入地震动加速度过程的研究，实现了地震动加速度的模拟，并可给出其解析表达式，便于设计地震动的调整及地震反应的求解。  相似文献   

不同类别场地地震动参数的计算分析   总被引：45，自引：2，他引：45  

李小军  彭青 《地震工程与工程振动》2001,21(1):29-36

基于188个工程场地计算剖面及场地地震反应分析的等线性化波动分析方法，通过对场地地震反应的计算及计算结果的分析，研究了4类场地条件对场地地震动影响的特点及规律，给出了每一类场地地震动参数变化的经验关系。  相似文献   

大型结构地震反应值模拟中的波动输入   总被引：11，自引：6，他引：11  

李山有  廖振鹏  周正华 《地震工程与工程振动》2001,21(2):1-5

解耦的时域有限元数值模拟技术在考虑土－结构相互作用的大型结构地震反应分析中的应用日趋成熟。为完善其中的波动输入技术，本提出 了一种波动输入时步数值模拟的简便方法，替换对自由场的频域计算，从而使结构反应分析可以完全通过时步数值模拟实现。同时，通过数值实现，对这一实施方案的有效性进行了检验。  相似文献   

Seismic Response of Base-Isolated Structures underMulti-component Ground Motion Excitation     

Jiang Yicheng Tang Jiaxiang School of Civil Engineering  Huazhong University of Science  Technology  Wuhan 《中国地质大学学报(英文版)》2001,12(1)

INTRODUCTIONConcept of base isolation has attracted considerable attention in recent years (Sun et al., 1994). The basic isolationsystem consists of an array of bearings between the base of thebuilding and its foundation. It shifts the fundamental frequencyof the structure away from the energetic region of the earthquake spectrum and limits the earthquake energy transmitted tothe superstructure (Tang and Liu, 1993 ). Base isolation isused widely to protect structures from the destructive…  相似文献   

内蒙古中部早古生代地体的拼合与增置   总被引：5，自引：0，他引：5  

李双庆 《内蒙古地质》1997,(1)

内蒙古中部布龙山、温都尔庙一带的蛇绿岩套、蓝门石片岩及其南邻的华北地台两者在空间上以川井－布鲁台庙深大断裂带为界，在时间上具有截然不同的地质演化特点。其内部在构造演化史上也不尽相同，可进一步划分为布龙山－哈拉地层地体和白乃庙－温都尔庙混杂地体。这两个曾分离着的地体，经长时期的运移，于晚志留世之前拼合联为一体，构成早古生代联合地体。直到早二叠世才增置于中朝古板块北缘（或华北地台北缘）。  相似文献   

A NUMERICAL ANALYSIS ON TYPHOON ASYMMETRIC STRUCTURE AND MOTION     

袁金南  王国民 《热带气象学报(英文版)》1997,3(2):159-167

Five prediction experiments are carried out with two typhoons in 1992 using a limitedarca primitiveequations and two-way interactive model in a movable,nested mesh. The result indicates good agreementin terms of motion between the prediction and observation. Studying the asymmetric structure in the cases selected, a close link is uncovered between the temporal evolutions of the structure and the track of motion in a tropical cyclone. Understanding of real asymmetric structure will help to improve the skill offorecasting tropical cyclones.  相似文献