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91.
溱潼凹陷西斜坡是岩性、构造-岩性等隐蔽油藏勘探的有利区,具有砂体薄、横向变化快、圈闭面积小、断裂关系复杂等特点。常规地震处理剖面保幅性差、频率低,导致小断层识别困难、地层尖灭线刻画精度低、岩性圈闭不落实。开展以提高地震资料保幅性、提高分辨率为核心的“双高”处理方法研究,构建以保幅去噪、一致性处理、高精度Radon变换法压制多次波、反Q滤波提高分辨率、五维数据规则化及精细速度建模等为主的技术体系,并确定对应的质量控制方法。“双高”处理的地震资料保幅性好、信噪比高,波组产状与地质认识更吻合,目的层主频提高10 Hz,有效频宽拓宽20 Hz,小断层及地层尖灭点较清晰。新处理资料的解释发现了一批有利油气目标。 相似文献
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L. Lwemark S. Steinke C.-H. Wang M.-T. Chen A. Müller L.-J. Shiau S.-J. Kao S.-R. Song H.-L. Lin K.-Y. Wei 《Dynamics of Atmospheres and Oceans》2009,47(1-3):138-153
We provide new evidence for the development of a stable estuarine circulation characterized by stagnating water bodies, nutrient recycling and increased primary productivity in the South China Sea (SCS) during glacial intervals. This circulation was caused by the closure of the shallow and narrow straits connecting the SCS in the south and west. Our main evidence is derived from newly measured Mn concentrations and Mn/Al ratios in two sediment cores from the northern and southeastern SCS covering the last 500 ky. Concentrations and Mn/Al ratios of the redox sensitive element Mn show clear glacial–interglacial cycles with maxima during interglacial periods and minima during glacial periods. These cycles indicate ventilation cycles of the bottom water, and are connected to the glacial–interglacial changes in sea level. In contrast, total organic carbon (TOC) concentrations display an opposite pattern with pronounced maxima during glacial times, especially in the southern part of the basin. The variations in TOC can be ascribed to two factors. Firstly, variations in primary productivity are controlled by variations in the intensity of the winter monsoon. Secondly to the degree of preservation of TOC controlled by variations in ventilation, which in turn is ultimately controlled by sea level. Consequently, variations in TOC represent a superimposition of primarily sea level influenced preservation control and winter monsoon driven variations in primary productivity intensity. The decrease in Mn correspond to times when sea level dropped 40–60 m below the present level. The larger amplitude of the variations in TOC and Mn in the southern part of the basin compared to the northern site suggest that oxygen depletion and nutrient recycling was stronger in the parts of the basin situated the furthest away from the only remaining opening to the open Pacific, the Luzon Strait. 相似文献
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The role of diagenetic carbonate concretions in the preservation of the original sedimentary record 总被引:1,自引:0,他引:1
The Upper Cretaceous organic rich limestones and marls of the Tarfaya basin of southwest Morocco contain numerous calcite concretions, which formed during early diagenesis. Relative textural similarities are observed both in the concretions and in the host sediments. However, the biological content of the concretions is considerably higher than in the host marls and limestones. Evidence for fossil dissolution in the host marls, and the absence of concretions in some fossil-rich zones, suggest that the difference in fossil abundance between the concretions and host rock is a function of dissolution, rather than preferential precipitation in fossil-rich areas. Consequently, the carbonate concretions appear to represent the 'memory' of the sediment and allow quantification of the original biological components and are potential tools for estimating the original biological material deposited in the soft sediments. 相似文献
97.
Dona J. Stewart 《The Professional geographer》2001,53(3):361-373
This article presents a methodology for a more detailed investigation of urban landscape change in rapidly growing cities of the less developed world beyond typical macrolevel approaches. This research is an attempt to bridge the gap between traditional landscape analysis and geographic information science (GIS). The article presents the preliminary results from a pilot project in Zamalek, Egypt, highlighting the benefits and drawbacks of the two techniques. Rarely used to study the less developed world, these techniques are utilized to assess change within a portion of Cairo's urban landscape. Large‐scale historic maps and high‐resolution satellite imagery, combined with field attribute collection, are the major data sources in this applied landscape analysis. A motivating factor in the desire to examine landscape change at such a large scale is the need to create monitoring systems for historic preservation in cities of the less developed world. 相似文献
98.
Relationships of Louisiana Colonial Land Claims with Potential Natural Vegetation and Historic Standing Structures: A GIS Approach* 总被引:1,自引:0,他引:1
Peter B. Mires 《The Professional geographer》1993,45(3):342-350
Louisiana's French, Spanish, and British colonial administrations left a vivid imprint on the landscape in the form of unique cadastral survey systems. The collective distribution of these colonial land claims presents a picture of the colonial occupation of the state. Settlement shows up clearly along the waterways of the bayou state. Equally significant are the areas devoid of land claims. This paper discusses the compilation of the colonial Louisiana land claims map and demonstrates its utility to GIS-based historical geography and historic preservation. By merging this map with other digitized datasets such as potential natural vegetation and historic structures, the seemingly chaotic 18th century occupance of an extremely heterogeneous physical environment becomes patterned, and prior assumptions about the colonial settlement process may be tested with greater precision. 相似文献
99.
矿床四维时空定量评价的新认识——以西藏玉龙斑岩铜矿床为例 总被引:4,自引:3,他引:1
大型、超大型斑岩铜矿的定量研究正在受到广泛关注,集中体现在现代矿产资源勘探模式趋向于从经验找矿、理论找矿和信息找矿3大传统找矿方法向集成信息技术方向发展。本项研究以青藏高原典型的玉龙斑岩铜矿床为例进行分析,提出了矿床定量评价的4个方面的新认识:(1)区域矿床发生、发展的年代与消亡速率的确定是研究矿床规模与保存环境的重要参数;(2)研究区的古地理、古气候特征有利于斑岩体的剥蚀起始时间的估算,研究区不同时代地层剖面的对比分析以及成矿古地理环境的模拟有利于正确评价斑岩矿床的形成与保存现状;(3)地层、岩体、构造和DEM数据的三维空间定量研究是正确评价"多位一体"成矿模式的重要因素;(4)3S技术发展了三维可视化技术、数据融合和模拟技术,能够最大限度地利用各种多元数据(地质、地球物理、地球化学和遥感等)资料,有助于提高发现大型矿床或潜在矿床的成功率。 相似文献
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