基于SGS的城市地理信息公共平台建设及应用   总被引：1，自引：1，他引：0  

张鹏程  吴素芝 《地理空间信息》2011,9(3):9-11,14

依托城市基础测绘成果数据,按照<地理信息公共服务平台>、<地理空间框架基本规定>等相关标准及规范,经过数据提取、重组、加工并制作了面向政务服务的地图产品数据;基于超图数字城市地理信息公共服务平台SGSV6.0,快速搭建了广州市政务基础地理信息共享服务平台,使得政府部门可以通过在线浏览、简单系统定制、地图API接口开发和...  相似文献   

渤海海洋石油平台设定地震反应谱的确定   总被引：2，自引：0，他引：2       下载免费PDF全文

荣棉水  吕悦军  彭艳菊  沙海军 《地震学报》2011,33(3):386-396

以渤海海域内已兴建的BZ28-2石油平台为研究对象,综合确定性和概率地震危险性分析方法的优点,通过对渤海海域内地震活动时空分布特征、地震地质背景、发震断裂及其活动性、平台遭受破坏性地震震级与距离的可能组合、设定地震的实际发生概率等几个方面的研究,综合确定了平台不同超越慨率对应的设定地震参数,并基于以上研究结果,给出了B...  相似文献   

内蒙古贝力克玄武岩台地火山地质及成因探讨   总被引：4，自引：0，他引：4       下载免费PDF全文

陈生生  樊祺诚  赵勇伟  隋建立 《地震地质》2011,33(2):430-439

根据火山地质特征,内蒙古锡林郭勒地区的新生代玄武岩可以划分为阿巴嘎玄武岩、贝力克玄武岩和达里诺尔玄武岩,呈NW-SE向展布.贝力克玄武岩以面积小、没有火山锥体、岩性较为单一(绝大多数为拉斑玄武岩)及不含慢源包体的熔岩台地而显著区别于另两种玄武岩.贝力克玄武岩以发育4级高低错落有致、大小不一的熔岩台地为特征,各级熔岩台地...  相似文献   

广西田东布兵石炭纪水下沉积灰岩脉及其地质意义          下载免费PDF全文

周开华  陈春芳  陆刚  田青  李新华  汤新田 《地质论评》2011,57(6):900-905

笔者等首次在德保台地边缘上泥盆统灰岩中发现大量多期次下石炭统杜内阶之灰岩岩脉;通过调查,查明岩脉的形态、沉积物特征、时代及其分布规律,首次在沉积岩脉中采获早石炭世早期牙形刺及Gnathodus与Siphnodella大量混生的现象。经过调查研究,对岩脉的成因有新的认识: 其形成是构造与地震相结合的产物,地震造成台地的隆升、沉降,使上泥盆统已成岩的刚性灰岩发生断裂,形成较深层的张性（拉张）裂隙,早石炭世未成岩的软沉积物及碎屑灌入裂隙中,形成灰岩脉。多期次的构造运动、拉张,造成张性裂隙的多次的张裂,多期次灌入则形成似直立产状的岩墙。这一成因模式既能合理解释岩脉中具有地震造成的液化脉之现象,又能解释形成如此深度岩脉的动力因素,也能解释台地边缘相中有深水相的沉积物及生物之物质来源。通过对岩脉的调查及研究,对理解右江盆地的构造演化具有重要的意义。  相似文献   

扬子地区晚奥陶世碳酸盐台地淹没事件及其地质意义   总被引：2，自引：1，他引：1       下载免费PDF全文

严德天  王清晨  陈代钊  汪建国  邱振 《地质科学》2011,46(1):42-51

碳酸盐岩台地广泛发育及其淹没事件是扬子地区晚奥陶世地层的重要特征之一.基于岩石学、沉积学特征和古生物资料等对扬子地区晚奥陶世碳酸盐岩台地沉积演化、淹没事件及其油气地质意义进行了分析.结果表明:扬子地区晚奥陶世沉积演化分为宝塔一临湘期碳酸盐台地沉积和五峰期深水、浅水陆棚沉积两个阶段;淹没事件开始于五峰初期,主要受控于构造...  相似文献   

Widespread overspill from a saline density‐current channel and its interaction with topography on the south‐west Black Sea shelf     

Richard N. Hiscott  Ali E. Aksu  Roger D. Flood  Vladimir Kostylev  Doğan Yaşar 《Sedimentology》2013,60(7):1639-1667

Seaward of the Bosphorus Strait, the south‐west Black Sea shelf is dominated by the world's largest channel network maintained by a quasi‐continuous saline (ca 35 → 31 psu) underflow. Calculations indicate that >85% of the initial discharge of ca 10⁴ m³s^?1 spills overbank before the shelf edge. This paper documents interaction of the overspill with sea bed topography using multibeam bathymetry, echo‐sounder images of the water column, conductivity–temperature–depth profiles and sediment cores. Overbank spill is widespread, particularly through crevasse channels and on the middle shelf where confinement by channel banks is negligible. Towards the outer shelf, the wind‐driven Rim Current advects mud along the shelf, contributing to levée successions and deposition on stoss sides of elongate transverse ridges. Echo‐sounder profiles reveal metre‐scale eddies over megaflutes, and breaking lee waves and internal hydraulic jumps over ridges. Megaflutes reach 600 m long and 7 m deep, yet form where the underflow, outside the flute, is no thicker than ca 2 to 5 m. Two types of elongate seaward‐facing ridges are recognized. Type 1 ridges, 2 to 5 m high, consist of bivalve‐rich muddy sand in low‐angle (3·5° to 6°) cross‐sets created by the underflow. Type 2 ridges, ca 5 m high, have crests up to 2 km long and a buried wedge‐shaped foundation (the ‘ridge‐core’) comprised of facies similar to Type 1 ridges. These ridge‐cores are blanketed on the landward side by stratified muds, and are capped by obliquely oriented ribs supporting a diverse benthic community. This facies distribution is interpreted to result from stoss‐side and lee‐side velocity and turbulence fluctuations induced by internal hydraulic jumps and breaking lee waves in overspilling portions of the underflow. Experimental results published by W.H. Snyder and co‐workers effectively explain ridge evolution and flow across the ridges, and therefore can be applied with confidence to less easily studied deep‐marine settings swept by turbidity currents.  相似文献   

Neoproterozoic evolution of the basement of the South-American platform     

《Journal of South American Earth Sciences》2013

Neoproterozoic geologic and geotectonic processes were of utmost importance in forming and structuring the basement framework of the South-American platform. Two large domains with distinct evolutionary histories are identified with respect to the Neoproterozoic era: the northwest-west (Amazonian craton and surroundings) and the central-southeast (the extra-Amazonian domain).In the first domain, Neoproterozoic events occurred only locally and were of secondary significance, and the geologic events, processes, and structures of the pre-Neoproterozoic (and syn-Brasiliano) cratonic block were much more influential. In the second, the extra-Amazonian domain, the final evolution, structures and forms are assigned to events related to the development of a complex net of Neoproterozoic mobile belts. These in turn resulted in strong reworking of the older pre-Neoproterozoic basement. In this domain, four distinct structural provinces circumscribe or are separated by relatively small pre-Neoproterozoic cratonic nuclei, namely the Pampean, Tocantins, Borborema and Mantiqueira provinces. These extra-Amazonian provinces were formed by a complex framework of orogenic branching systems following a diversified post-Mesoproterozoic paleogeographic scenario. This scenario included many types of basement inliers as well as a diversified organization of accretionary and collisional orogens. The basement inliers date from the Archean to Mesoproterozoic periods and are different in nature. The escape tectonics that operated during the final consolidation stages of the provinces were important to and responsible for the final forms currently observed. These latest events, which occurred from the Late Ediacaran to the Early Ordovician, present serious obstacles to paleogeographic reconstructions.Two groups of orogenic collage systems are identified. The older system from the Tonian (>850 Ma) period is of restricted occurrence and is not fully understood due to strong reworking subsequent to Tonian times. The second group of orogenies is more extensive and more important. Its development began with diachronic taphrogenic processes in the Early Cryogenian period (ca. 850–750 Ma) and preceded a complex scenario of continental, transitional and oceanic basins. Subsequent orogenies (post 800 Ma) were also created by diachronic processes that ended in the Early Ordovician. More than one orogeny (plate interaction) can be identified either in space or in time in every province. The orogenic processes were not necessarily synchronous in different parts of the orogenic system, even within the same province. This particular group of orogenic collage events is known as the “Brasiliano”.All of the structural provinces of the extra-Amazonian domain exhibit final events that are marked by extrusion processes, are represented by long lineaments, and are fundamental to unraveling the structural history of the Phanerozoic sedimentary basins.  相似文献   

Tectonics of the western part of the Polish Outer Carpathians     

《Geodinamica Acta》2013,26(1-3):127-143

The western part of the Polish Outer Carpathians is built up from the thrust, imbricated Upper Jurassic-Neogene flysch deposits. The following Outer Carpathian nappes have been distinguished: Magura Nappe, Fore-Magura group of nappes, Silesian, Subsilesian and Skole nappes. Interpretation of seismic and magnetotelluric survey from the region South of Wadowice, allows observation of relationship between basement and flysch nappes in the Outer Carpathians. It also allows identification of dislocation cutting both flysch nappes and their basement. All the Outer Carpathian nappes are thrust over the southern part of the North European Platform. The platform basement is composed of older Precambrian metamorphic rocks belonging to the Bruno-Vistulicum terrane. Sedimentary cover consists of Paleozoic, Mesozoic and Neogene sequences. The characteristic features of this boundary are horsts and troughs of general direction NW-SE, turning W-E. Faults cutting only the consolidated basement and the Paleozoic cover were formed during the Hercynian Orogeny in the Carboniferous and the Early Permian. Most of the older normal faults were covered by allochtonous flysch nappes forming thus the blind faults. During the last stage of the geodynamic development the Carpathians thrust sheets moved towards their present position. Displacement of the Carpathians northwards is related to development of dextral strike-slip faults of N—S direction. The orientation of this strike-slip fault zones zone more or less coincides with the surface position of the major faults perpendicular to the strike of the Outer Carpathian thrustsheets. The huge fault cuts formations from the Paleozoic basement through the flysch allochton between the boreholes in Sucha Beskidzka area. The displacement of nappes of the Carpathian overthrust and diapiric extrusion of plastic formations of the lower flysch units occurred along this fault.  相似文献   

水文基础数据通用平台在水情报汛和资料整编中的应用          下载免费PDF全文

王占峰 《水文》2013,33(6):52-57

水文基础数据通用平台,以其开放、可靠、可扩展性等优势,为越来越多的水文信息自动采集和数据处理提供服务,应用范围不断扩大。在实际工作中进行水文信息自动收集、矢量监视图自动更新、水情报文自动生成和转发,以及水文资料整编数据下载和转换为电算整编格式,是水文基础数据通用平台在业务处理方面的重要应用。  相似文献   

扬子东南缘“南华纪”盆地演化——来自新元古代花岗岩的年龄约束   总被引：1，自引：1，他引：0       下载免费PDF全文

孙海清黄建中  江新胜罗 来 马慧英 伍 皓 《中国地质》2013,40(6):1725-1735

提要： 通过对湘西南地区主动侵位的岛弧型花岗闪长岩、二长花岗岩的锆石LA-ICP-MS与SHRIMP U-Pb同位素年代学研究,分别获得加权平均年龄为（835.6±6.7）Ma、（840±8）Ma,属新元古代。对岩体围岩钙质板岩夹灰岩建造的剖面研究和同位素年代学分析及区域对比,确认其属于新元古代“南华纪”板溪期沉积——高涧群,与下伏冷家溪群连续沉积,底界时限应大于835 Ma。指出高涧群及其相当层位分布区在沉积盆地演化过程中,可能没有经历由俯冲造山—伸展裂谷盆地的完整演化过程,盆地从板片俯冲形成岩浆弧的初期演化即已停止,形成所谓的残余盆地,并沿从江—溆浦—双峰—衡阳—萍乡一线形成陡坡边缘盆地古地理格架,与北西侧伸展形成的断阶式陆坡相接,接受来自北西侧的陆缘碎屑及其改造型重力流沉积,完成这一转换过程的时间点在830 Ma左右。  相似文献