盒子波调查技术在六盘山黄土塬区的应用分析     

潘家智  许孝坤  何京国  宁鹏鹏  叶春学 《物探与化探》2015,(1):104-111,117

六盘山盆地被巨厚的黄土所覆盖,是表层和深层双复杂区域。巨厚的黄土和复杂的地形条件使该区干扰波非常发育,严重影响了地震资料的信噪比。为了有效调查该区干扰波发育特征,并进行针对性地压制,通过盒子波调查技术在该区的应用分析,提出了和生产结合进行盒子波调查的有效方式,克服了静校正问题对盒子波调查数据的影响。针对两种地形条件下的盒子波资料,分析了在不同地形和表层条件下干扰波场的变化,认为影响浅层和中深层信噪比的干扰波特征存在差异;并通过组合压噪效果分析,提出对不同深度勘探目标进行针对性压噪的组合接收方式,提高了六盘山地区巨厚黄土塬勘探区目标层采集资料的信噪比。  相似文献   

塔里木盆地柯坪-巴楚地区奥陶系层序界面特征及成因分析     

姜海健  陈强路  尤东华  黄继文  陈跃 《新疆地质》2015,(1):84-89

通过综合分析塔里木盆地柯坪-巴楚地区露头剖面的宏观组合和微观结构,总结出奥陶系不同级别层序界面的表现特征、成因机制,指导盆地内层序界面的研究。柯坪-巴楚地区奥陶系主要有3个级别的层序界面:一级层序界面发育在构造变革期,如受到造山运动或区域构造隆升作用等影响,表现为角度不整合面、平行不整合等特征;二级层序界面发育在沉积环境重大转换阶段,主要受到全球海平面变化的影响或局部构造运动影响,表现为平行不整合、淹没不整合等特征;三级层序界面与局部构造运动有关,表现为局部平行不整合。层序界面的表现形式包括古土壤层、喀斯特化、地层削截、地层超覆、岩性岩相突变等。通过总结不同层序界面的性质和成因,分析不整合面的规模和发育部位,预测有利岩溶储层发育的区带。  相似文献   

Characteristic and Controlling Factors of Organic Pores in Continental Shale Gas Reservoir of Chang 7th of Yanchang Formation, Ordos Basin     

CAO Qian  ZHOU Wen 《《地质学报》英文版》2015,89(Z1):1-2

<正>The goals of this paper are to document the characteristics and controlling factors of organic pores distributed in continental shale reservoir of Chang 7th of Yanchang Formation in Ordos Basin.In this experiment,by using Argon ion polishing,SEM images and nitrogen adsorption experiment,more than 105 blocks samples were collected from the core of 399.04m from 18 wells,and 83 pieces of casting thin section were made.The TOC  相似文献   

Strenulagus (Mammalia: Lagomorpha) from the Middle Eocene Irdin Manha Formation of the Erlian Basin, Nei Mongol, China     

?ucja FOSTOWICZ-FRELIK  LI Chuankui  LI Qian  MENG Jin  WANG Yuanqing 《《地质学报》英文版》2015,89(1):12-26

New material of Strenulagus solaris, a stem lagomorph, from the lower part of the Middle Eocene Irdin Manha Formation at the Irdin Manha and Huheboerhe localities, Erlian Basin, Nei Mongol, China includes remains of isolated cheek teeth, fragmentary upper incisors(d I2) and postcranial elements, reported from the species for the first time. The tarsal bones display advanced features, such as a wide calcaneofibular articulation surface and, along with an increase in hypsodonty, the new data document the early stage of lagomorph evolution in the Middle Eocene of the Erlian Basin. This finding is stratigraphically well constrained and probably predates that of the type material of S. solaris from the Khaychin Formation, Bugin-Tsav Basin, Mongolia.  相似文献   

Lithospheric Electrical Structure across the Eastern Segment of the Altyn Tagh Fault on the Northern Margin of the Tibetan Plateau     

ZHANG Letian  YE Gaofeng  JIN Sheng  WEI Wenbo  Martyn UNSWORTH  Alan G. JONES  JING Jianen  DONG Hao  XIE Chengliang  Florian LE PAPE  Jan VOZAR 《《地质学报》英文版》2015,89(1):90-104

Project INDEPTH (InterNational DEep Profiling of Tibet and the Himalaya) is an interdisciplinary program designed to develop a better understanding of deep structures and mechanics of the Tibetan Plateau. As a component of magnetotelluric (MT) work in the 4th phase of the project, MT data were collected along a profile that crosses the eastern segment of the Altyn Tagh fault on the northern margin of the plateau. Time series data processing used robust algorithms to give high quality responses. Dimensionality analysis showed that 2D approach is only valid for the northern section of the profile. Consequently, 2D inversions were only conducted for the northern section, and 3D inversions were conducted on MT data from the whole profile. From the 2D inversion model, the eastern segment of the Altyn Tagh fault only appears as a crustal structure, which suggests accommodation of strike slip motion along the Altyn Tagh fault by thrusting within the Qilian block. A large-scale off-profile conductor within the mid-lower crust of the Qilian block was revealed from the 3D inversion model, which is probably correlated with the North Qaidam thrust belt. Furthermore, the unconnected conductors from the 3D inversion model indicate that deformations in the study area are generally localized.  相似文献   

The Geological Characteristics of Chengkou Type Shale Gas of Lower Cambrian in Dabashan     

YE Jun  LIU bin  WANG Sheng  YU Ping  CHENG Jing 《《地质学报》英文版》2015,89(Z1):294-296

<正>1 Introduction After the successful implementation of large-scale shale gas exploration、development and utilization in United States,the domestic shale gas exploration and development is in a rapid development.However,the progress of exploration and understanding of the highEvolution shale gas in the complex structure zone of the outer basin are relatively slow,the evaluation method and  相似文献   

长江与嘉陵江交汇区水流结构的数值模拟          下载免费PDF全文

王协康  周苏芬  叶龙  王海周 《水科学进展》2015,26(3):372-377

针对天然河流交汇区域复杂的地形条件及水流运动特性,采用水气两相流三维数值模型,对长江与嘉陵江交汇区水流运动进行深入研究,分析了交汇区域分离区、剪切层、流速场及螺旋度的变化特性。研究结果表明:长江与嘉陵江交汇的水流分离区形状受地形影响明显,随着水位的增加向右岸移动,剪切层整体呈一个扭曲的曲面;干支流原有的环流在交汇之后重新汇合,左岸未出现明显的环流,右岸逆时针的环流有减弱趋势,交汇区域纵向流速呈现高速与低速带分布特征。此外,长江和嘉陵江在交汇口下游螺旋度呈现左侧为负、右侧为正的对称分布,水流结构表现出逐渐形成双螺旋流的趋势,其中左侧的螺旋流逆时针运动,右侧的螺旋流顺时针运动。  相似文献   

黄土高原西部地区黄土地层有机质主要来源分析*     

饶志国  郭文康  薛骞  陈发虎 《第四纪研究》2015,35(4)

黄土有机质的主要来源是决定其稳定碳同位素(δ13Corg.)能否应用于重建过去C3/C4相对丰度变化及相应的古气候变化的关键基础科学问题.如若黄土地层当中的有机质主要由粉尘携带而来,而非当地植被,显然其δ13Corg.不是一个局地植被过去C3/C4相对丰度变化及古气候变化的良好指示器.本文对黄土高原西部地区(六盘山以西)新获得和已发表的相关数据进行综合分析,尝试对该地区黄土有机质的主要来源进行定量的分析.结果表明,总体而言,该地区黄土地层有机质主要来源于当地植被,由粉尘携带而来的有机质贡献量不超过8％,所造成的有机碳同位素变化幅度不超过1.7‰.这些结果说明该地区的黄土地层有机质δ13Corg.是可以用来重建过去C3/C4植物相对丰度及相应的古气候变化的.为了更精确的重建,后续的工作应当更多考虑粉尘搬运过程当中的有机质输入以及粉尘沉积之后的微生物活动的可能潜在影响.  相似文献   

鄂尔多斯盆地LFP区块长2段沉积相研究     

叶亚坤  苏海伦  薛永康  李阳阳 《地下水》2015,(4)

储层的沉积相研究通常是油气藏勘探开发过程中一项十分重要的任务,它控制着储集砂体的成因类型及宏观分布。在岩芯观察的基础上,结合综合录井资料和野外露头剖面信息,运用沉积学、沉积构造、剖面结构、古生物及测井相等划分沉积相的标志,对研究区内钻井进行单井沉积相划分,对不同钻井之间的沉积相进行综合比对,结果认为LEP区块长2段主要从三角洲前缘高建设的水下分流河道骨架砂体沉积为主。  相似文献   

辽宁兴城地区地球物理探测效果评价     

张黎  刘万崧  张晨曦  赵倩 《世界地质》2015,34(1):194-202

以辽宁兴城实验区为重点,详细分析了重力、磁力、大地电磁测深和地震勘探等不同的物探方法对研究区内地质目标的识别作用。根据重力剖面测量、磁力剖面测量、大地电磁测深以及地震勘探等方法对实验区进行野外勘探工作和详细的数据分析。结果表明,重力异常对于构造单元划分、断裂识别、基底起伏的识别等均能发挥重要的作用;磁异常对于断裂识别、不同磁性岩石单元的识别、岩浆活动的分析等方面均能发挥重要的作用;大地电磁测深,在划分构造单元、确定断裂分布、垂向地层分层方面均能提供重要信息;地震勘探横向上可划分出盆地等构造界限,纵向上可分层。  相似文献