排序方式： 共有58条查询结果，搜索用时 15 毫秒
11.
The Kerinitis Delta in the Corinth Rift, Greece, is a footwall derived, coarse‐grained, Gilbert‐type fan delta deposited in the hangingwall of a linked normal fault system. This giant Gilbert‐type delta (radius 3·8 km, thickness > 600 m) was supplied by an antecedent river and built into a brackish to marine basin. Although as yet poorly dated, correlation with neighbouring deltas suggests that the Kerinitis Delta was deposited during a period of 500 to 800 ka in the Early to early Middle Pleistocene. Facies characterizing a range of depositional processes are assigned to four facies associations (topset, foreset, bottomset and prodelta). The dominantly fluvial topset facies association has locally developed shallow marine (limestone) and fluvial‐shoreface sub‐associations. This delta represents a subsidence‐dominated system in which high fault displacement overwhelmed base‐level falls (creation of accommodation predominantly ≥ 0). Stratal geometries and facies stacking patterns were used to identify 11 key stratal surfaces separating 11 stratal units. Each key stratal surface records a landward shift in the topset breakpoint path, indicating a rapid increase in accommodation/sediment supply. Each stratal unit records a gradual decrease in accommodation/sediment supply during deposition. The cyclic stratal units and key stratal surfaces are interpreted as recording eustatic falls and rises, respectively. A 30 m thick package of foresets below the main delta records the nucleation of a small Proto‐delta probably on an early relay ramp. Based on changes in stratal unit geometries, the main delta is divided into three packages, interpreted as recording the initiation, growth and death of the controlling fault system. The Lower delta comprises stacked, relatively thin, progradational stratal units recording low displacement on the young fault system (relay ramp). The Middle delta comprises vertically stacked stratal units, each recording initial aggradation–progradation followed by progradation; their aggradational component increases up through the Middle delta, which records the main phase of increasing rate of fault displacement. The Upper delta records pure progradation, recording abrupt cessation of movement on the fault. A major erosion surface incising basinward 120 m through the Lower and Middle delta records an exceptional submarine erosion process (canyon or delta collapse). 相似文献
12.
13.
有效厚度拟合定量恢复原始地层超覆点位置 总被引：1，自引：0，他引：1
地层超覆点的迁移是层序地层分析和海平面变化曲线编制的重要依据。受构造抬升、海平面下降或二者共同作用影响,地层超覆点在沉积后常被剥蚀。如何恢复其原始沉积时的位置,至今尚无定量方法提出。基于地层厚度自盆地边缘向盆地中心依次增大,或先增大、后减小的分布特点,采用指数与线性相结合的分段函数模型,利用未剥蚀区地层厚度数据拟合外推恢复原始地层超覆点位置。该方法适用于被动大陆边缘、大型三角洲沉积区及坳陷型盆地,应用于巽他陆架晚新生代地层分析,取得满意效果. 相似文献
14.
DENG Jun HUANG Dinghua WANG Qingfei WAN Li SUN Zhongshi YANG Liqiang & GAO Bangfei . State Key Laboratory of Geological Processes Mineral Resources China University of Geosciences Beijing China . Faculty of Earth Sciences China University of Geosciences Wuhan China . Department of Earth Sciences Jilin University Changchun China 《中国科学D辑(英文版)》2005,(7)
~~Experimental remolding on the caprock’s 3D strain field of the Indosinian-Yanshanian epoch in Tongling deposit concentrating area1.Chang,Y.F.,Liu,X.P.,Wu,Y.C,The Cu,Fe Metallogenic Belt in the Middle-Lower Reaches of Yangtze River(in Chinese with English abstract),Beijing:Geological Publishing House,1991,1-379.
2.Yin,H.F.,Wu,S.B.,Du,Y.S.,South China is the part of multi-islands and multi-oceans system of Tethys,Earth Sciences(in Chinese),1999,24(1):1-12.
3.Wu,G G,Zha… 相似文献
15.
火山岩冷却单元的识别是火山岩地层和岩相研究的重要环节。松辽盆地东南缘露头区和徐家围子断陷营城组火山岩剖面的剖析显示,冷却单元主要存在4种主要的单元类型:碎屑岩型、熔岩型、碎屑岩+熔岩型和熔岩+碎屑岩型。碎屑岩型和熔岩型是端元类型,分别反映蒸汽喷发和岩浆喷发的作用过程;碎屑岩+熔岩型是基本组合单元类型,反映蒸汽-岩浆喷发的连续作用过程;熔岩+碎屑岩型属于改造的或特殊机制的类型。冷却单元本身及其堆叠具有相的意义,是火山岩地层的基本成因地层单元,因此成为解释火山岩地层结构、了解形成与保存过程的重要基础。通过火山岩冷却单元识别与叠置分析,构建了松辽盆地徐家围子断陷营城组一段的地层结构。 相似文献
16.
Sandstones of the Dainan Formation in the Gaoyou Sag of the Subei Basin are important hydrocarbon reservoirs. This paper studies the sedimentary facies and sandstone dispersal patterns in the Gaoyou Sag, based on the analysis of sedimentology and seismic geomorphology. The data used in this study include lithological data, wire-line-log data and three-dimensional (3D) seismic data. The target strata are the Eocene Daiyi Member (E2d13, E2d12 and E2d11) and the lower Dai'er Member (E2d25), which belong to three third-order sequences. Five types of depositional systems were identified in the Dainan Formation based on core observation and log-facies analysis. They are, respectively, delta, fan delta, sub-lacustrine fan, nearshore subaqueous fan and lacustrine system. Stratal slices from 3D seismic volumes have been used to map the sandstone dispersal patterns and to document the evolution of the depositional systems within these third-order sequences and associated systems tracts. In the low-stand systems tract and the high-stand systems tract, sandstones of delta, fan delta and nearshore subaqueous fan were well developed and can be delineated by stratal slices showing distinct progradation towards the deep lake centre. In the transgressive systems tract, sandstones are less common. Stratal slices indicate that the depositional environments of individual third-order sequences evolved from gravel-rich or sand-rich fans to lacustrine mudstones, and finally to mixed sandstone–mudstone fans. Sandstone dispersal patterns appear to be primarily controlled by syn-sedimentary faults, and generally sandstone thickness decreases with distance from the syn-sedimentary faults. Deltas and fan deltas have different characteristics in sand-body thickness because they have different sedimentary subfacies. The proposed geomorphology and sedimentary evolution of the lacustrine depositional system may aid in the prediction of potential reservoir distribution in the Gaoyou Sag. 相似文献
17.
沾化凹陷三合村洼陷沙河街组沙三下亚段（Es3L）作为重要储集层段,勘探潜力巨大,精细刻画三合村洼陷沙三下亚 段物源体系对沉积体系重建、有利区带预测具重要意义。采用古地貌宏观区分物源区与沉积区,并精细刻画西南部与南部 物源通道（I~VI号）,运用岩心、岩屑组成特征明确沉积区沉积相类型及原始物质成分,通过地震属性与地层切片精细描绘 沉积区内“源-汇”配置及时空演化关系,从不同角度、不同层次对三合村洼陷古物源体系进行综合刻画。结果表明,洼 陷西南部斜坡区（约3°）物源来自陈家庄凸起西段（I、II号沟槽输导）,相对富砾,以碳酸盐岩岩屑为主;南部坡折区 （约8°）物源来自于陈家庄凸起东段（III~VI号沟谷输导）,相对富砂,发育单晶石英或多晶石英颗粒。平面上,沉积区扇 三角洲沉积体系规模与物源通道的宽深比及延伸距离呈正相关,垂向上,低位体系域（LST）形成扇体规模远大于高位体 系域（HST）扇体,且交汇区物源体系由南部向西南部迁移转化。 相似文献
18.
方差体的改进算法及在地震解释中的应用 总被引：1，自引：0，他引：1
传统的三维地震方差体算法计算时间较长。为了缩短解释周期,在算法分析的基础上,采用递推算法对传统的方差体算法进行改进,并开发出方差体分析处理软件。通过对实际资料处理与测试表明,改进算法速度较常规方法快,方差体技术对断层、裂隙发育带等地质异常体具有良好的识别效果,提高了地震资料的解释精度。 相似文献
19.
利用点云切片提取技术分析桥梁形变 总被引：1，自引：1，他引：0
三维激光扫描技术作为近年来发展迅速的测绘手段,在桥梁健康监测中,已经成为监测技术的重要组成部分。本文以武汉市某跨江大桥为例,首先采用Trimble SX10三维激光扫描仪对桥梁进行长期监测扫描,并对桥梁钢结构和桥墩的点云进行切片;然后在Trimble Business Center 和 Trimble RealWorks软件的帮助下对每期的扫描点云进行处理,提取桥拱断面点坐标并对桥墩切片点云进行最佳垂直圆柱体拟合,获取拟合平面中心点坐标;最后对比分析每期特征点平面坐标的偏差和三维偏移量。本文研究成果验证了三维激光扫描仪在桥梁变形监测中的可行性,丰富了桥梁监测数据的表现形式,可以为相关研究提供依据和参考。 相似文献
20.