准噶尔盆地西部车排子凸起新近系沙湾组成藏体系与富集规律   总被引：6，自引：1，他引：5  

沈扬  贾东  赵宏亮  韩祥磊 《地质通报》2010,29(4):581-588

准噶尔盆地西部车排子凸起远源成藏,新近系油气藏和油气显示基本都在一套厚砂层和其上的薄砂层中,厚砂层和薄砂层之间存在密切的油源联系。针对这一成藏现象,利用区域构造、油源对比、输导体系、化验证据、成藏特征等手段,系统研究车排子的成藏体系。结果表明,车排子轻质油源岩为侏罗系,主要来自昌吉凹陷西部,油气运移指向为东南到西北方向。区域构造运动形成的白垩系与侏罗系的不整合面和红车断裂的长期活动使得油气能从深部生烃区向浅层凸起区长距离运移。沙湾组一段区域展布的厚砂层高效的横向输导作用是车排子凸起油气规模富集的关键,喜马拉雅期小断层的纵向沟通促成了沙湾组二段薄砂岩性体的最终成藏。白垩系与侏罗系的不整合面-红车断裂-沙湾组一段厚砂层的紧密接触、良好匹配构成了复式、高效的输导格架。通过成藏体系研究,归纳总结了车排子地区的成藏模式,并提出沙湾组二段岩性油气藏和一段上倾尖灭或超覆油气藏是最有利的勘探方向。  相似文献   

羌塘腹地新生代火山岩的地球化学特征与青藏高原隆升   总被引：31，自引：3，他引：28  

谭富文  潘桂棠  徐强 《岩石矿物学杂志》2000,19(2):121-130

羌塘腹地新生代火山岩产出于青藏高原地壳向北减薄、地壳泊松比值向北发生异常增高的过渡地区。该区火山岩在藏北地区新生代火山岩中形成时代最老,为 4 4.1± 1.0Ma～32.6± 0.8Ma。岩石学及地球化学研究表明,区内新生代火山岩形成于大陆碰撞造山后的拉张环境,为壳源岩浆和幔源岩浆的混合产物。藏北高原的隆升与岩石圈地幔的拆离、地壳拉伸减薄及火山活动密切相关,由此推测藏北高原的主要隆升起始期为 4 0Ma左右。  相似文献   

热液汉体泵吸上浸管流动力学模拟及其预测意义   总被引：16，自引：1，他引：15  

赵伦山  岑况 《地学前缘》2000,7(1):205-215

地球流体相在各种地质过程中的行为和作用,是地球物质科学的核心课题。通过对山西义兴寨脉状金矿热液流体上侵动力学的模拟计算证明,构造泵吸驱动的矿液流动具有有压管流的性质,并探索引入柏努利方程对其流动状态进行描述。论证了地质流体因其性质和所处地质环境的不同,可划分为多孔介质中的渗流和较宽阔裂隙中的管流（流动）两种。赋 于地壳中深部或由岩浆冷却分异形成的成矿流体,在张前性断裂活动中,主要由构造泵吸机制驱使  相似文献   

The history of crustal uplift and metamorphic evolution of Panzhihua-Xichang micro-palaeoland,SW China: Constraints on Sm-Nd, <Superscript>40</Superscript>Ar/<Superscript>39</Superscript>Ar and FT ages of granulites     

XU Shijin  LIU Wenzhong  WANG Rucheng  YU Hangbo  LI Daming  WAN Jinglin & FANG Zhong . Department of Earth Sciences  State Key Laboratory for Mineral Deposits Research  Nanjing University  Nanjing  China  . Institute of Geology  China Seismological Bureau  Beijing  China 《中国科学D辑(英文版)》2004,47(8):689-703

Panzhihua-Xichang micro-palaeoland (Panxi ter-rane) is located on the western margin of the Yangtze Block. The western boundary of the Panxi mi-cro-palaeoland, and also the western boundary of the Yangtze Block, is the Jinhe-Jinghe fault, which defines the eastern boundary of the Songpan-Ganzi Fold Belt. The eastern boundary of this micro-palaeoland is the Ganluo fault. On the east side of the Ganluo fault is the Sichuan Basin in the Yangtze Block (fig. 1). Panxi micro-palaeoland is on…  相似文献   

浙皖赣相邻区加里东期构造变形特征   总被引：7，自引：0，他引：7  

余心起 张达汪隆武  颜铁增邓国辉 《地质通报》2006,25(6):676-684

浙皖赣相邻区在加里东时期受到华南加里东构造事件的影响,前震旦纪基底及早古生代早期盖层强烈隆升并褶皱变形,皖浙赣邻接部位早-中石炭世地层直接覆盖在中元古代浅变质岩系之上,东端清凉峰一带的中石炭统覆盖在上寒武统之上,但尚未见到有加里东期岩浆活动的证据.同时,古陆南侧及东侧震旦纪-早志留世盖层向南(东)滑脱,接触带附近与基底一并形成倒转产状及倒转褶皱;北侧向北滑脱形成滑覆褶皱及临溪盆地、兰田残留向斜盆地.印支、燕山事件对加里东构造形迹产生了不可忽略的改造,最终形成了基本延续至今的构造格局.  相似文献   

玉龙—哈巴雪山断块差异隆升的基本特征及其地质灾害效应   总被引：5，自引：0，他引：5       下载免费PDF全文

张西娟曾庆利  马寅生 《中国地质》2006,33(5):1075-1082

青藏高原新生代以来的持续性、阶段性隆升是地球演化过程中重要的地质和环境事件。尤其是晚新生代以来的加速隆升,使青藏高原主体及其周缘地区成为中国大陆地貌的最高一级阶梯。笔者主要从新构造运动条件下青藏高原东南缘玉龙—哈巴雪山断块这样一个典型的第四纪以来断块快速差异隆升的地区出发,通过详细研究该断块的组成以及几何学运动学特征来探讨其隆升机制,并在此基础上进一步研究该快速隆起的地质灾害效应(如地震、崩塌、滑坡和泥石流等)及其对本区地质灾害发育和发展的控制作用,进而得到地球内动力地质作用与重大地质灾害(外动力地质作用)之间存在必然的耦合关系的结论。  相似文献   

Experimental and analytical studies of structures seismically isolated with an uplift‐restraining friction pendulum system     

Panayiotis C. Roussis  Michael C. Constantinou 《地震工程与结构动力学》2006,35(5):595-611

This paper presents findings from a comprehensive analytical and experimental study on the uplift‐restraining XY‐FP sliding isolation system. To investigate the effectiveness of the XY‐FP isolator and provide a rational basis for evaluating the efficacy of the developed mathematical model, an extensive experimental program was conducted on the earthquake simulator at the University at Buffalo. The experimental program involved a slender, five‐storey, scale‐model frame seismically isolated with four XY‐FP isolators subjected to simulations of historical horizontal and vertical ground motions. The experimental response demonstrates the validity of the concept and provides evidence for the effectiveness of the XY‐FP isolator in preventing uplift. A comprehensive analytical model capable of emulating the mechanical behaviour of the XY‐FP isolator is developed and implemented in program 3D‐BASIS‐ME. The newly enhanced program is used to predict the dynamic response of the seismically‐isolated model structure. Comparison of analytical predictions with experimental results attests to the efficacy of the analytical model for simulating the response of the XY‐FP isolator. With its appealing conceptual simplicity and its proven effectiveness, the new uplift‐restraining isolator has the potential to facilitate the application of seismic isolation even under the most extreme of conditions, including but not limited to near‐fault strong ground motions and uplift‐prone structural systems. Copyright © 2005 John Wiley & Sons, Ltd.  相似文献   

Bedrock gorges in the central mainland Kachchh: Implications for landscape evolution     

M. G. Thakkar  B. Goyal  A. K. Patidar  D. M. Maurya  L. S. Chamyal 《Journal of Earth System Science》2006,115(2):249-256

Kachchh possesses a fault-controlled first-order topography and several geomorphic features indicative of active tectonics. Though coseismic neotectonic activity is believed to be the major factor in the evolution of the landscape, detailed documentation and analysis of vital landscape features like drainage characteristics, bedrock gorges and terraces are lacking. The present study is a site-specific documentation of gorges developed in the central part of the mainland Kachchh. We analyzed and interpreted four gorges occurring on either side of Katrol Hill Fault (KHF). The Khari river gorge is endowed with six levels of bedrock terraces, some of which are studded with large potholes and flutings. Since no active development of potholes is observed along the rivers in the present day hyper-arid conditions, we infer an obvious linkage of gorges to the humid phases, which provided high energy runoff for the formation of gorges and distinct bedrock terraces and associated erosional features. Development of gorges within the miliolites and incision in the fluvial deposits to the south of the KHF indicates that the gorges were formed during Early Holocene. However, ubiquitous occurrence of gorges along the streams to the south of KHF, the uniformly N40‡ E trend of the gorges, their close association with transverse faults and the short length of the exceptionally well developed Khari river gorge in the low-relief rocky plain to the north of KHF suggests an important role of neotectonic movements  相似文献   

桩-桶基础抗拔承载力分析     

刘文白  王梦瑜  周健 《上海国土资源》2006,(3):24-28,39

根据新型基础一桩-桶基础在上拔荷载作用下的颗粒流模拟试验结果,分析了桩桶基础在上拔荷载作用下土体的破坏过程,并对颗粒流模拟试验的颗粒的破坏面进行拟合,提出桩桶基础的上拔承载力计算模式。桩-桶基础的极限上拔承载力由破坏土体侧表面抗剪强度在竖直方向投影的集合及其包围土体土重和桩-桶基础自重组成,建立了桩-桶基础的上拔承载力计算公式,分析了上拔承载力影响因素。  相似文献   

液压阻尼系统控制浮放立式储罐提离失稳   总被引：1，自引：0，他引：1  

袁朝庆  张云峰  孙建刚 《地震工程与工程振动》2005,25(6):49-52

立式圆柱储罐在油田、石油化工等企业用途广泛，多用作存贮易燃、易爆介质，一旦遭遇震害，后果将十分严重。本文针对浮放立式储罐地震响应的提离失稳问题，采用液压阻尼系统（HDS）用以控制储罐的提离反应，建立了安装HDS储罐的力学分析模型并进行了数值计算，对安装HDS后储罐的提离反应进行了分析。仿真计算结果表明：HDS可以有效地减小提离应力，从而地震烈度可以降低1度进行储罐的提离设计。  相似文献