Stochastic geometry in petroleum geology     

K. S. Deffeyes  B. D. Ripley  G. S. Watson 《Mathematical Geology》1982,14(5):419-432

Many aspects of the generation, migration, trapping, and discovery of petroleum, as well as its primary and enhanced recovery, depend upon geometry. The scale of the relevant geometric features varies all the way from that of continental margins and basins down to the pores and fissures in reservoir rocks. Because the spatial complexity is so great for each of these processes, it is reasonable to describe them statistically. The primary purpose of this paper is to survey possible ways in which statistical or stochastic geometry enters and might be used in petroleum geology and engineering. While it offers some new theory, this paper does not directly suggest any specific new methods for the estimation of hydrocarbon resources or reserves. This deficiency is mainly due to the current lack of relevant data. When data are available the point of view explained herein will be fruitful. The survey ties together many topics in a novel way.  相似文献   

Models of bed formation     

Michael F. Dacey 《Mathematical Geology》1979,11(6):655-668

The model for bed formation by Kolmogorov consists of an unending sequence of alternating periods of deposition and erosion of sediments, with the amounts of deposition and erosion being independent random variables. This paper examines this model in relation to recent mathematical studies that are relevant to, and simplify, the analysis of the thickness of the bed that remains after the sequence is operated for a long time. This thickness obeys the exponential probability law when the amounts of deposition and erosion also obey the exponential law distributed. For the discrete version formulated by Schwarzacher, the thickness obeys the geometric probability law when the amounts of deposition and erosion obey the geometric law.  相似文献   

The low seismic activity of the Korean Peninsula surrounded by high earthquake countries   总被引：1，自引：0，他引：1  

S.G. Kim  E. Lkhasuren  P.-H. Park 《Journal of Seismology》2004,8(1):91-103

Although the Korean Peninsula is locatednear several great earthquake regions suchas NE China and SW Japan, it has neversuffered from catastrophic earthquakes forthe last 2000 years according to historicaland instrumental records. We investigatedthe low seismicity of Korea based on thehypothesis of the Baikal-Korea Plate (BKP)or Amurian Plate movement which isinitiated by the Baikal Rift Zone spreadingin a southeastward motion with acounter-clockwise rotation due to thecollision of the Indian Plate against theEurasian Plate. Many disastrous earthquakesof NE China, SW Japan and Sakhalin releaselarge amounts of seismic energy along theboundary of the Baikal-Korea Plate. It isnecessary to compute the released seismicenergy along the presumed boundary of theBaikal-Korea Plate compared to the KoreanPeninsula in order to estimate themicro-plate boundary. The total energyreleases (1900–1999) from the majordisastrous earthquakes (M6.0) alongthe Baikal-Korea plate are about10³–10⁴ times as much as theKorean Peninsula (M3.0). The focalmechanisms for the intra-continentalearthquakes near and/or along theBaikal-Korea Plate boundary of NE China, SW Japan, Sakhalin and Mongolia mostlyrepresent the horizontal motions of theright-lateral strike slip type, indicatingthat the Baikal-Korea Plate is acounter-clockwise and transcurrent motion. The relative displacement vectors of GPS(global positioning system) also indicatedthat the Baikal-Korea Plate movescounter-clockwise around the KoreanPeninsula. These factors may indicate thatthe Korean Peninsula is not located at thePlate boundary, but just within a margin ofthe Baikal-Korea Plate which movessoutheastward with a counter-clockwiserotation from the Baikal Rift Zone in NEAsia. Therefore there is no enoughaccumulated strain to generate largeearthquakes in the Korean Peninsula and itmakes the Korean Peninsula free fromseismic hazard of large catastrophicearthquakes.  相似文献   

Tropical systematic and random error energetics based on NCEP (MRF) analysis-forecast system — A barotropic approach     

S. De  D. R. Chakraborty 《Journal of Earth System Science》2004,113(2):151-166

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一种新的基于Wold分解的纹理分析方法     

王淑晴  臧晓兵  关泽群 《测绘工程》2006,15(1):20-23

针对纹理图像具有结构性和随机性的特点,提出一种新的统一的纹理描述方法。该方法基于Wold分解,在图像为均匀同质随机场的条件下,将纹理图像分解为结构性成份和随机性成份,用少量参数对纹理特征进行描述,为纹理图像的分割、检索、压缩提供了一个统一的纹理模型。  相似文献   

一种基于嫦娥一号CCD影像的影像匹配方法     

何钰  蓝朝桢  邢帅 《测绘科学技术学报》2012,(4):281-284

月球测绘是完成月球探测任务的基础保障。这里提出了一种适合于CE-1获取的CCD影像的多尺度约束自动匹配方法。首先利用SURF算子提取影像上特征点;然后进行基于准核线和最小欧式距离约束的影像匹配;最后采用随机采样算法对误匹配点进行剔除而得到同名点信息。实验结果表明,该匹配方法提取的同名点有利于CE-1月球影像DEM的生成。  相似文献   

全局局部细节感知条件随机场的高分辨率遥感影像建筑物提取     

朱祺琪  李真  张亚男  李佳伦  杜禹强  关庆锋  李德仁 《遥感学报》2021,25(7):1422-1433

条件随机场模型由于其较强的上下文信息建模能力,被广泛应用于建筑物提取任务中。然而,面对高分辨率遥感影像丰富的地物信息,基于条件随机场的提取方法存在建筑物边界模糊的问题。本文提出了一种全局局部细节感知条件随机场框架,该框架提出全局局部一体化D-LinkNet,在有效利用多尺度建筑物信息的同时保留局部结构信息,解决了传统条件随机场一元势能丢失边界信息的问题。同时,该框架融合分割先验以缓解建筑物类内光谱差异较大的影响,利用更大尺度的上下文信息来精确提取建筑物,并引入局部类别标记代价从而保持细节信息以获取清晰的建筑物边界。实验结果表明,该框架在WHU卫星和航空数据集上的精度评价指标均优于其他对比方法,其IoU分别达89.82%和91.72%,对于复杂场景下的建筑物信息能够获得较好的提取效果。  相似文献   

钠基蒙脱土水合演化机制     

张云龙  项伟  黄伟  刘清秉  DAO Minh huan 《岩土力学》2019,40(11):4391-4400

为了查明钠基蒙脱土的水合演化过程,以天然钠基蒙脱土为研究对象,开展在相对湿度（ ）为0～0.98区间的水汽等温吸-脱附试验,通过吸附速率曲线、BET曲线界定钠基蒙脱土各水合阶段及相应的水合主控因素;通过测定晶层 值变化规律,从吸附水影响黏土矿物晶层厚度的角度探讨钠基蒙脱土的水合演化特征;基于傅里叶红外光谱,从水分子结构伸缩振动信息角度对钠基蒙脱土水合演化过程进行定性定量验证;通过热重/差热分析,以吸附水相变所需能量与吸附水重量变化的角度解释钠基蒙脱土的吸附水特征与其水合机制的关系。试验结果表明：在较低相对湿度下（0 0.15）,以钠基蒙脱土矿物外表面吸附为主,形成表面吸附水;0.15 0.40为钠基蒙脱土层间阳离子水合阶段;0.40 0.98,为晶层内外表面水合阶段,水分子逐步完整的包裹蒙脱土,形成多层吸附层。钠基蒙脱土的水合演化过程受控于层间钠离子与晶层基面,层间钠离子的水合能影响了钠基蒙脱土水合演化的起始顺序。  相似文献   

柴达木盆地及邻区侏罗纪原型盆地恢复及油气勘探前景     

冯乔  付锁堂  张小莉  陈琰  汪立群  周飞  倪金龙 《地学前缘》2019,26(1):44-58

侏罗系是柴达木盆地最重要的源储层系之一。通过野外地质、剖面实测、地震解释、显微构造分析等大量系列资料的综合应用与分析,认为研究区自中生代以来,经历了印支期右行逆冲-走滑构造运动、早—中侏罗世伸展运动、早白垩世北西-南东向挤压及新生代南北向挤压运动,它们与早侏罗世至中侏罗世早期(小煤沟组至大煤沟组)在NE向伸展应力场作用下形成的断陷盆地、中侏罗世晚期至晚侏罗世(彩石岭组—洪水沟组)热力沉降坳陷盆地、早白垩世南北向挤压坳陷盆地密切相关。侏罗纪原型盆地发育三类沉积边界,即盆缘不整合边界(缓坡型和陡坡型边界)、盆内正断层边界、后期逆断层改造边界。不同的现存盆地边界类型对原型盆地恢复的作用不同。侏罗纪盆地以东昆仑构造带为界具有"北陆南洋"的古地理格局,柴达木地区的侏罗纪盆地主要发育在沿岸造山带和岛弧带的山前坳陷以及薄弱的柴北缘加里东俯冲碰撞带之上,形成相对分隔的独立盆地群。柴达木早、中、晚侏罗世原型盆地的分布因受到古特提斯洋向北偏东方向的俯冲作用和阿尔金断裂左旋走滑作用的影响,其沉积中心和沉积范围呈现出从早到晚向东北方向逐渐迁移的规律。早侏罗世盆地的沉积沉降中心主要位于柴北缘西部的冷湖—马海一带,中侏罗世盆地的沉积沉降中心主要位于柴北缘中段的大柴旦—怀头他拉一带,而晚侏罗世盆地的沉积沉降中心主要位于德令哈—乌兰一带。  相似文献   

基于伪随机信号的磁电法渗漏模型试验     

张化鹏  钱卫  刘瑾  武立林  宋泽卓 《物探与化探》2022,(1):198-205

磁电法是近些年在国内兴起的一种电磁勘探方法,该方法在探测地下渗流等长走向的良导地质体方面具有技术优势,但是其抗干扰能力差,易受外部噪声影响,一直未能推广.近年来,伪随机信号在物探领域开始广泛应用,该技术通过对冲激响应及阶跃响应进行卷积运算来达到降噪目的 ,可极大地提升抗干扰能力,因此,本文结合磁电法的勘探原理及伪随机辨...  相似文献