地层不整合遮挡油气藏地质储量计算新方法及其应用     

袁丽 《地球科学与环境学报》2011,33(2):163-167

从几何学的观点出发,针对纯油藏和具有气顶的油气藏,采用单储系数、横截面面积与油层横向分布长度三者乘积的方式改进采用单储系数、含油面积与油层厚度三者乘积方式的传统容积法,提出相应的地层不整合遮挡油气藏地质储量计算新公式,并根据油气藏的特点提出水平井钻遇油气藏厚度的预测公式。地层不整合遮挡油气藏的地质储量计算目前主要采用容积法,这类方法不仅计算繁琐,而且不确定因素较多;改进后的新方法计算简单方便,理论性更强,存在的不确定因素显著减少。采用新方法在高青油田高424块高424-1井区进行了实践应用。实践表明:改进的新方法适用于地层不整合遮挡油气藏的地质储量计算及预测水平井钻遇油气藏厚度。  相似文献   

内蒙古乌斯尼黑蛇绿混杂岩带形成时代的地质新证据   总被引：3，自引：0，他引：3  

鲍庆中  张长捷  吴之理 《地质与资源》2011,20(1):16-20

贺根山-乌斯尼黑蛇绿混杂岩带的属性和形成时代存在明显的认识上的分歧.早期认为是二叠纪侵入的超镁铁质岩体.该超镁铁质岩体侵入了下二叠统格根敖包组,并被哲斯组地层不整合覆盖,形成时代为二叠纪.20世纪80年代以来,通过中国北方板块构造研究,在硅质岩中采集到的一系列化石资料表明,贺根山地区蛇绿混杂岩的形成时代应为中-晚泥盆世...  相似文献   

雪峰山基底隆升带及其邻区印支期陆内构造特征与成因   总被引：7，自引：0，他引：7  

李三忠  王涛  金宠  戴黎明  刘鑫  周小军  王岳军  张国伟 《吉林大学学报(地球科学版)》2011,41(1):93-105

狭义的华南陆块东部包括扬子地块和华夏地块,而雪峰山陆内构造系统是扬子地块的重要组成部分。通过对雪峰山地区印支期地层角度不整合时空分布规律的分析表明,高角度不整合—微角度不整合—平行不整合—整合的空间分布区域依次由东往西递变渐新。根据褶皱变形分析得出,雪峰山地区在印支期发育了北东东向和北北东向2个轴迹方向的褶皱,后期叠加了南北向弧形逆冲推覆构造。区域构造背景和动力学分析表明,扬子地块内部印支期总体北东向的变形形迹与东西轴向的秦岭—大别造山带和扬子地块南部东西轴向的构造线相垂直;其原因是:扬子地块与华夏地块最终陆内收缩变形的时间比扬子与华北沿秦岭—大别造山带的陆间碰撞拼合的时间早,印支早期的先存北北东向构造线在印支晚期由于扬子地块顺时针旋转变位为北东东向,从而决定了印支早期现今北东东向的构造线,随后的第二幕北北东向构造线的形成是在与早期第一幕变形的应力场相同的同一构造应力场作用下形成的。但是,秦岭—大别造山带近东西向的构造线取决于主动大陆边缘,即总体近东西向的华北陆块南缘边界,其原始方位为总体近东西向。这些复杂边界条件和旋转决定了先形成彼此近于垂直的构造线,然后拼接形成现今构造线垂直的格局。  相似文献   

Nature and significance of the Neoproterozoic Sturtian–Marinoan Boundary,Northern Adelaide Geosyncline,South Australia     

T. A. Fromhold  M. W. Wallace 《Australian Journal of Earth Sciences》2013,60(6):599-613

The Cryogenian succession of the Northern Flinders Ranges reveals a complex sedimentary record between the Sturtian and Marinoan glacial deposits. A major unconformity separates the Sturtian and Marinoan-aged sedimentary successions in the area. This forms a subaerial erosion surface with terrestrial and marginal marine infill directly above the Angepena and Balcanoona Formations in their respective localities. This exposure surface is here correlated with the previously documented submarine unconformity between the Yankaninna Formation and the underlying deep marine Tapley Hill Formation. This erosional event provides a chronostratigraphic marker horizon that coincides approximately with thepreviously defined Sturtian–Marinoan Time Series boundary in the Northern Flinders Ranges. These stratigraphic relationships also constrain lateral facies relationships between the Oodnaminta ReefComplex (Balcanoona Formation) and the Angepena Formation. Similarly, the shallow-water Weetootla Dolomite is correlated with the deeper water carbonates of the Yankaninna Formation.  相似文献   

Comparison of the Ordovician-Carboniferous Boundary Between Korea and NE China: Implications for Correlation and Tectonic Evolution   总被引：2，自引：0，他引：2  

Jeong Hwan Kim  Yong Il Lee  Maosong Li  Zhiquiang Bai 《Gondwana Research》2001,4(1)

There is a great hiatus between Ordovician and Carboniferous strata in the Northeast China and Korean Peninsula. In order to understand geology and tectonic evolution, and to find out the similarities and differences in both regions, two sections in the Western Hill near Beijing in NE China and several sections in the Korean Peninsula were selected to examine their geologic boundaries between Lower and Upper Paleozoic strata to compare their characteristic features. At four sites in the two sections in the Western Hill near Beijing were examined their contact relations. The Hui Yu section is the same horizon where one site is top of a quarry hill and the other of down hill. Mid-Carboniferous Qingshuijian Formation rests on the Ordovician Majiagou Formation. Limestone beds are more commonly intercalated with shale and sandstone at site 2 of the Hui Yu section, while at site 1, conglomerate beds are dominant. Site 1 of the Se Shu Fen section shows eroded and concealed karst topography and conglomerate beds are intercalated within shale beds. Silurian and Devonian strata are absent in these areas. In the Korean Peninsula, most O-C contacts occur between Ordovician limestone formation and Carboniferous strata, although Silurian strata occur beneath the Carboniferous strata in the Jeongseon area and Pyeongnam Basin. Most contact relations are parallel unconformity and angular unconformity is rarely seen. The O-C relations in both regions are similar to each other, and these indicate that the Korean Peninsula was located near or belonged to the Sino-Korean paraplatform during Paleozoic time.  相似文献   

Relationship between statistical thermal alteration index and vitrinite reflectance for sedimentary rocks in northern Japan with reference to effects for unconformity,faulting, and contact metamorphism     

Yoshihiro Ujiié 《Island Arc》2009,18(4):661-669

Two organic maturity indices, the statistical thermal alteration index (stTAI) and vitrinite reflectance (R_O), are used to gain insight into the geological histories of sequences of Tertiary and Upper Cretaceous sediments in northern Japan that contain an unconformity and which are affected by faulting and contact metamorphism. The stTAI is based on the brightness, or gray level, of fossil pollen of Pinus, Podocarpus, Abies, and Picea species. Pollen brightness is measured using a transmitted‐light microscope equipped with a computer‐driven digital image processor. The stTAI represents the mean value of the modes for the complete array of indigenous pollen in rock samples. The stTAI indicates the level of organic maturation for Neogene sedimentary rocks of Japan, from incipient diagenesis to early catagenesis (R_O ≤1.0%). With the progressive diagenesis and catagenesis of sedimentary rocks, stTAI values generally show a progressive decrease, whereas R_O values increase. The effects of an unconformity and faulting are more clearly recorded in stTAI trends than in R_O trends. During early stages of organic maturation (R_O ≤0.7%), stTAI shows a rapid decrease, while R_O shows a rapid increase during the mature and post‐mature stages (R_O ≥0.8%). The occurrence of a range in R_O values for a given level of organic maturity makes it difficult to determine the influence of the unconformity on the increasing R_O trend. R_O values show a progressive increase toward an igneous dyke, but this trend is not apparent in stTAI values. Measurements of Tertiary and Upper Cretaceous rocks in Japan reveal that stTAI is more sensitive to heating duration than R_O, although R_O is more sensitive to heating temperature.  相似文献   

造山带区域相对海平面变化与全球海平面变化的不一致性   总被引：2，自引：1，他引：1  

蔡雄飞 《海洋地质前沿》2005,21(2):5-7

影响区域相对海平面变化的因素错综复杂,既可以单一作用,也可以相互作用;既可以受全球海平面变化的影响,也可以受局部因素的控制,因此,全球海平面与区域海平面相对变化既可以同步,也可以不同步,尤其在造山带地区可以不一致,甚至相反。只有找出这种控制主导因素,才可以把局部地质场放到全球统一场中去。  相似文献   

不整合空间结构与油气成藏综述   总被引：15，自引：5，他引：10  

王艳忠  操应长  王淑萍  宋玉斌 《大地构造与成矿学》2006,30(3):326-330

不整合是由不整合面及其上、下岩石三部分组成,在空间上具有三层结构,即不整合面之上的岩石、不整合面之下的风化粘土层以及风化粘土层之下的半风化岩石。风化粘土层在上覆沉积物压实作用下岩性较致密,具有良好的封盖能力。不整合面之上的高孔渗岩石(主要为砂岩、砾岩)和不整合面之下裂隙、溶蚀孔洞发育的半风化岩石(主要为砂岩、砾岩、碳酸盐岩、火山岩及变质岩)既可作为油气运移通道,又可成为油气聚集的有效储层。由于构造部位、岩性等因素的影响,不整合空间结构复杂多变,导致不整合油气藏成藏规律复杂,因此,不整合空间结构研究对不整合油气藏勘探具有重要的指导意义。  相似文献   

黔北务-正-道地区铝土矿地质特征及资源潜力分析   总被引：24，自引：3，他引：21  

武国辉  刘幼平  张应文 《地质与勘探》2006,42(2):39-43

文章简要介绍了务-正-道地区铝土矿的成矿地质背景和务川瓦厂坪铝土矿床的地质特征.重点从含矿层位下二叠统梁山组地层的分布、厚度变化;构造运动控制务-正-道地区古地理的变迁;褶皱构造控矿等几方面分析了与铝土矿成矿的关系,进而又对比了省内各铝土矿集区找矿勘探工作程度,综合分析了该区的找矿勘探潜力.认为务-正-道地区应存在大中型规模的铝土矿床,中下志留统韩家店组之上的不整合面,下二叠统梁山组和向斜构造是其成矿的主要控矿因素.  相似文献   

塔中地区奥陶系碳酸盐岩不整合带的结构   总被引：8，自引：2，他引：6  

刘克奇  蔡忠贤  张淑贞  赵桂青 《地球科学与环境学报》2006,28(2):41-44

塔中地区中上奥陶统与下奥陶统之间发育碳酸盐岩不整合,不整合带是溶解作用发生的有利地带,可以作为烃类运移通道或油气聚集的场所。应用地质和地球物理方法对塔中地区奥陶系碳酸盐岩不整合进行了研究。塔中地区奥陶系碳酸盐岩不整合输导体在流体运动特点上不整合面上、下分属于两个不同的流体流动场,不整合面下,流动孔隙主要由孔洞缝孔隙体系构成,因此,流体的运动属于复杂介质条件下的流体运动,而不整合面上的层状渗透性体大多数情况下属于孔隙型介质,流体在其中的流动通常可以用达西定律加以描述。因此,不整合输导体中,流体从不整合面下向不整合面上运动,在流型上必然发生明显转换,这种转换对烃类的聚集是非常重要的。  相似文献