地震静态应力触发模型的全球检验   总被引：19，自引：0，他引：19  

万永革  吴忠良  周公威  黄静  秦立新 《地震学报》2002,24(3):302-316

运用1976～2000年哈佛大学矩心矩张量目录，采用地震对概念对地震静态应力触发模型进行检验．结果表明，从全球角度来看，地震静态应力触发效应确实存在，但只是一种很弱的效应．将地震分为正断层、逆断层、走滑断层等分别对静态应力触发模型进行检验，发现非走滑断层地震具有明显的触发效应，而走滑断层地震触发效应则不明显．按地震对中后续事件的延迟时间分为延迟时间t1天、t＜１天、t10天、t＜10天和1天 t10天5个时间段的地震对，分别对地震静态应力触发模型进行研究，发现静态应力触发效应在地震之后的短时间内不随延迟时间的变化而变化．对全球不同区域的地震静态应力触发情况的研究表明，消减带地震对的触发效应较为明显．为了研究地震静态应力触发模型在中国应用的可能性，对中国及邻区的地震进行了检验，发现就中国及邻区的地震类型而言（以走滑断层为主），不容易观测到地震静态应力触发现象．   相似文献   

福州盆地活动断裂的探槽研究   总被引：4，自引：1，他引：4       下载免费PDF全文

闵伟  朱金芳  冉勇康  宋方敏  杨晓平  黄宗林 《地震地质》2002,24(4):514-523

在前人对福州盆地及其周缘活动断裂 1/ 1万填图研究的基础上 ,通过室内航卫片判读、野外详细调查等方法 ,经过详细论证 ,在福州盆地及周缘 6条活动断裂上选择了 11个认为可能是断层通过的位置 ,进行了探槽开挖。大部分探槽只揭露到了基岩中的断层 ,有些探槽在开挖深度内既没有揭露到基岩 ,在第四系中也没有揭露到断层。对于没有揭露到断层的探槽 ,认为断层没有错断开挖深度内的第四纪地层 ,以探槽最底部的地层年代作为断层最新活动时代的上限。有些探槽揭露到了基岩中的断层 ,这些断层向上没有错断第四系 ,就以上覆第四系底部的时代作为断层最新活动时代的上限。只有在沿桐口 -洪山桥断裂开挖的探槽中 ,揭露出 2条断层 ,它们向上都错断了相同层位的第四纪地层 ,并被更新的第四系所覆盖。根据测年结果 ,这些断裂不是全新世活动断裂 ,其中 ,闽侯 -南屿断裂可能为晚更新世活动断裂 ,其它断裂晚更新世以来都已不活动  相似文献   

断裂地震地表断错危险性评价   总被引：6，自引：1，他引：6       下载免费PDF全文

梁小华  蒋溥  董津城  刘守华 《地震地质》2002,24(4):495-502

引入地震断错危险性概念 ,用概率表示发生断错的可能性大小 ,断错危险性涉及到地震危险性和断错发生与分布特点。断错危险性的表达式为 :P =P1×P2 ×P3,式中 ,P表示断错危险性 ;P1表示地震发生的危险性 ;P2 指不同震级条件下地表断错出现的概率 ;P3为断错量值分布概率。以中国和世界地表地震断错资料为基础 ,建立震级 -断错概率指数P2 和断错幅度及其分布概率指数 ,包括幅值及其分布、宽度和覆盖层厚度影响等指数P3,为地表断错危险性量化评估奠定了基础  相似文献   

Human’s digital footprints on the Qinghai-Tibet Plateau: Variations during festivals and impacts on nature reserves     

Du  Yunyan  Tu  Wenna  Liang  Fuyuan  Yi  Jiawei 《地理学报(英文版)》2021,31(2):179-194

Mobile internet and wireless communication technologies have produced unprecedented location-aware data. Such big geospatial data can be used as a proxy measure of the ‘digital footprints' left by us on the planet and provide a valuable opportunity to understand the dynamic and short-term human disturbance on the nature at fine scales. This study investigated the spatiotemporal variations of human's digital footprints on the Qinghai-Tibet Plateau using smartphone-users-generated Tencent's location request data. The results showed that human's digital footprints cover less than 5% of Qinghai and Tibet, exhibiting either a U-shaped or an N-shaped temporal change pattern during the major festivals. Spatial changes of the digital footprints manifested a transition process from dispersion to concentration in Xining and Lhasa. Human disturbance assessment of seven large nature reserves on the plateau showed that the Qinghai Lake is the most disturbed one as shown by 14.6% of its area is stained with human digital footprints and the areal average of footprint intensity is 1.59, and the disturbance was significantly escalated during the National Day holiday. By contrast, the Qangtang and Hoh Xil are the least affected nature reserves with the two indices less than 1% and 0.1, respectively.  相似文献   

新疆天山金矿可持续发展建议     

马华东  涂其军  张玉萍 《陕西地质》2008,26(1):25-31

新疆天山成矿带是我国重要的金成矿带,主要发育韧性剪切带型、火山型和穆龙套型3种类型金矿床。随着社会经济的快速发展,黄金的需求量在逐年增大,这就要求新疆对金矿的勘查开发要加大力度。本文通过研究新疆天山金矿的特征并就可持续发展提出建议。  相似文献   

南京附近新近纪岩石地层若干问题探讨   总被引：1，自引：0，他引：1       下载免费PDF全文

邵家骥  刘志平  杨武  尚培颖 《江苏地质》2008,32(4):257-262

通过南京附近新近纪砂砾层代表性剖面描述及对比,新近纪玄武岩的喷发期次及其与砂砾层的层序关系,着重讨论了新近纪砂砾层的岩石地层层序及不同时段砂砾层的岩性特征。建议建立大雨花台组（群）（N1-2y）来包含南京附近所有的新近纪砂砾层;建议该区新近纪玄武岩统一命名为方山（旋回）玄武岩。  相似文献   

吉林省煤铁矿产资源勘查工作部署     

孙众志  王凤生  刘恩峰 《吉林地质》2008,27(3)

吉林省煤炭、铁矿资源储量严重不足,原煤、铁矿石自给率低,严重影响地方经济发展,通过加大勘查投资,煤、铁资源储量有望取得重大突破,提出了全省2008年煤、铁矿勘查部署和保证措施。  相似文献   

A SAURON look at galaxy bulges     

J. Falcn‐Barroso  R. Bacon  M. Bureau  M. Cappellari  R. L. Davies  E. Emsellem  D. Krajnovi&#x;  H. Kuntschner  R. McDermid  R. F. Peletier  P. T. de Zeeuw 《Astronomische Nachrichten》2004,325(2):92-95

Kinematic and population studies show that bulges are generally rotationally flattened systems similar to lowluminosity ellipticals. However, observations with state‐of‐the‐art integral field spectrographs, such as SAURON, indicate that the situation is much more complex, and allow us to investigate phenomena such as triaxiality, kinematic decoupling and population substructure, and to study their connection to current formation and evolution scenarios for bulges of early‐type galaxies. We present the examples of two S0 bulges from galaxies in our sample of nearby galaxies: one that shows all the properties expected from classical bulges (NGC5866), and another case that presents kinematic features appropriate for barred disk galaxies (NGC7332). (© 2004 WILEY‐VCH Verlag GmbH & Co. KGaA, Weinheim)  相似文献   

Ultrahigh-pressure and Retrograde Metamorphic Ages for Paleozoic Protolith of Paragneiss in the Main Drill Hole of the Chinese Continental Scientific Drilling Project （CCSD-MH）, SW Sulu UHP Terrane   总被引：5，自引：1，他引：4  

LIU Fulai  XU Zhiqin  XUE Huaimin  ZHOU Kaifu Institute of Geology  Chinese Academy of Geological Sciences  Bejing 《《地质学报》英文版》2006,80(3):336-348

Laser Raman spectroscopy and cathodoluminescence (CL) images show that most zircon crystals separated from paragneiss in the main drill hole of the Chinese Continental Scientific Drilling Project (CCSD-MH) at Maobei, southwestern Sulu terrane, contain low-pressure mineral-bearing detrital cores, coesite-bearing mantles and quartz-bearing or mineral inclusion-free rims. SHRIMP U Pb dating on these zoned zircons yield three discrete and meaningful age groups. The detrital cores yield a large age span from 659 to 313 Ma, indicating the protolith age for the analyzed paragneiss is Paleozoic rather than Proterozoic. The coesite-bearing mantles yield a weighted mean age of 228 ± 5 Ma for the UHP event. The quartz-bearing outmost rims yield a weighted mean age of 213 ± 6 Ma for the retrogressive event related to the regional amphibolite facies metamorphism in the Sulu UHP terrane. Combined with previous SHRIMP U-Pb dating results from orthogneiss in CCSD-MH, it is suggested that both Neoproterozoic granitic protolith and Paleozoic sedimentary rocks were subducted to mantle depths in the Late Triassic. About 15 million years later, the Sulu UHP metamorphic rocks were exhumed to mid-crustal levels and overprinted by an amphibolite-facies retrogressive metamorphism. The exhumation rate deduced from the SHRIMP data and metamorphic P-T conditions is about 6.7 km/Ma. Such a fast exhumation suggests that the Sulu UHP paragneiss and orthogneiss returned towards the surface as a dominant part of a buoyant sliver, caused as a consequence of slab breakoff.  相似文献   

Magmatic Event at the End of the Archean in Eastern Hebei Province and Its Geological Implication   总被引：20，自引：0，他引：20  

GENG Yuansheng  LIU Fulai  YANG Chonghui Institute of Geology  Chinese Academy of Geological Sciences  Beijing 《《地质学报》英文版》2006,80(6):819-833

1 Introduction With a wide distribution of the early Precambrian rocks, eastern Hebei Province is one of the classical regions for early Precambrian study of China. From the 1960s up to now, a great deal of geological surveys and researches have been undertaken in the region. The region was well-known among geologists of the world for the first report of the isotopic age of c. 3500 Ma (Rb-Sr Group, Laboratory of Isotopic Geology and Composite Research Group, Institute of Geology, Academ…  相似文献