中深层天然气藏地震预测技术研究   总被引：1，自引：0，他引：1  

李红梅  李惠玲  魏文  王树刚  王凡剑 《华北地震科学》2008,26(3):5-9

济阳坳陷天然气资源丰富,已在多个层系发现了不同类型的中深层天然气藏,由于气藏地质条件、地震反射复杂,针对不同的气藏需采用不同的地震预测技术。本文在中深层天然气藏地质特点分析的基础上进行了岩石物理、地震反演、地震属性等预测技术研究,结果表明：中层气藏储层物性较好,储层与围岩的岩石物理参数差异明显,应用亮点、AVO、叠前弹性阻抗反演技术可较好地识别预测三角洲砂岩气藏;针对深层低孔低渗砂岩气藏,地震属性及多属性反演是有效的储层预测技术,并预测了孤北地区二叠系有利储集相带分布,结合构造分析,指出了孤北地区深层气勘探方向。  相似文献   

萍乐坳陷西段早三叠世飞剑潭组的创建及地层层序研究     

袁建芽 《华东地质学院学报》2000,23(2):116-120

描述了创建剖面,划分了6地性段,并从沉积特征研究入手,确定了各种沉积相,微相及沉积体系,通过对小层序组划分,结合层序界面,首泛面和最大海泛面确定体系域和层序,在萍乐坳陷西段早三叠世飞剑组划分出4个正层序。  相似文献   

临川市垃圾填埋场地工程地质条件研究     

周龙茂  夏菲 《华东地质学院学报》2000,23(3):209-213

临川市垃圾填埋场根据所选用的改良厌氧卫生填埋结构对工程地质条件的基本要求,在拟建场区开展１：２０００水文地质调查与工程地质勘察的基础上,进行工程地质特征研究,确定了可建场的主坝及拉污坝的持力层,分析了该场地产生渗的可能性,论证了该场址的适宜性。  相似文献   

用钻进参数仪实时判层   总被引：5，自引：1，他引：4  

滕子军 《煤田地质与勘探》2000,28(2):58-60

利用钻进参数仪采集的各岩石的钻速、钻压、转速3个参数数据进行回归分析,计算各种岩石的视可钻性指数,并在钻进中实时判层。   相似文献   

有关煤层气勘探评价的若干问题     

王涛  黄文涛 《江西地质》2000,14(4):306-308

煤层气的勘探评价,是开展煤层气勘探与开发工作的基础。当前要搞好勘探评价工作,需注意解决以下３个方面的问题：广泛搜集、认真总结国外煤层勘探开发的资料,精心筛选出适合我国国情的勘探评价参数体系;改进与完善煤层气勘探评价参数的测试技术,制定出与国际惯例相容的测试指南,为勘探评价提供准确的、可比性强的定量依据;做好勘探评价的经济财务分析工作,认真开展可行性研究评价,坚持综合勘探、综合评价原则。  相似文献   

青海东北部中强地震序列类型及特征研究     

陈玉华  马文静  张敏 《内陆地震》2000,14(4):330-338

１９７０～１９９９年青海东北部发生Ｍｓ≥５．０地震序列２２个。通过分析发现,主一余型地震序列９个,约占序列占总数的４１％,孤立型序列８个,约占序列总数的３６％,前－主－余型序列３个,约占序列总数的１３％,双震（前－双主－余）型序列２个,约占序列总数的１０％。这些序列分属３个不同的地震带,地震的频率,强度及序列类型在各个地震带表现不一,各具犍色,此外还分析了序列早期（０．５、１、２、３、４、５、７天）及全序列的特征参数ｂ值、ｕ值、ｈ值、ρ值的变化过程,认为ｂ值和ｕ值的变化对该地区震序列类型的早期判断有一定参考价值。  相似文献   

扬子地台西缘志留纪层序地层研究   总被引：1，自引：0，他引：1  

邹光富  陈永明 《四川地质学报》2000,20(3):171-175

应用层序地层学的原理和方法,对扬子地台西缘陕西宁强－四川广元地区的志留系剖面进行了重新研究,识别出９个三级层序。三级层序均发育ＴＳＴ和ＨＳＴ,而缺乏ＬＳＴ和ＳＭＳＴ。通过区内沉积层序的对比,建立了扬子西缘专留纪层序地层格架。最后探讨了该区馨留纪的海平面变化规律。  相似文献   

Stratigraphic and structural evolution of the Selenga Delta Accommodation Zone, Lake Baikal Rift, Siberia     

C. A. Scholz  D. R. Hutchinson 《International Journal of Earth Sciences》2000,89(2):212-228

Seismic reflection profiles from the Lake Baikal Rift reveal extensive details about the sediment thickness, structural geometry and history of extensional deformation and syn-rift sedimentation in this classic continental rift. The Selenga River is the largest single source of terrigenous input into Lake Baikal, and its large delta sits astride the major accommodation zone between the Central and South basins of the lake. Incorporating one of the world's largest lacustrine deltas, this depositional system is a classic example of the influence of rift basin structural segmentation on a major continental drainage. More than 3700 km of deep basin-scale multi-channel seismic reflection (MCS) data were acquired during the 1989 Russian and the 1992 Russian–American field programs. The seismic data image most of the sedimentary section, including pre-rift basement in several localities. The MCS data reveal that the broad bathymetric saddle between these two major half-graben basins is underlain by a complex of severely deformed basement blocks, and is not simply a consequence of long-term deltaic deposition. Maximum sediment thickness is estimated to be more than 9 km in some areas around the Selenga Delta. Detailed stratigraphic analyses of the Selenga area MCS data suggest that modes of deposition have shifted markedly during the history of the delta. The present mode of gravity- and mass-flow sedimentation that dominates the northern and southern parts of the modern delta, as well as the pronounced bathymetric relief in the area, are relatively recent developments in the history of the Lake Baikal Rift. Several episodes of major delta progradation, each extending far across the modern rift, can be documented in the MCS data. The stratigraphic framework defined by these prograding deltaic sequences can be used to constrain the structural as well as depositional evolution of this part of the Baikal Rift. An age model has been established for this stratigraphy, by tying the delta sequences to the site of the Baikal Drilling Project 1993 Drill Hole. Although the drill hole is only 100 m deep, and the base of the cores is only ∼670 ka in age, ages were extrapolated to deeper stratigraphic intervals using the Reflection-Seismic-Radiocarbon method of Cohen et al. (1993). The deep prograding delta sequences now observed in the MCS data probably formed in response to major fluctuations in sediment supply, rather than in response to shifts in lake level. This stratigraphic framework and age model suggest that the deep delta packages developed at intervals of approximately 400 ka and may have formed as a consequence of climate changes affiliated with the northern hemisphere glaciations. The stratigraphic analysis also suggests that the Selenga Basin and Syncline developed as a distinct depocentre only during the past ∼2–3 Ma. Received: 1 December 1999 / Accepted: 26 January 2000  相似文献   

东营凹陷尚南断块东营组沉积层序研究   总被引：3，自引：3，他引：0       下载免费PDF全文

田海芹  马玉新  赵勇生  于文芹  刘克奇  毕义泉  沈国华  谢凤猛 《古地理学报》2000,2(2):37-45

尚南断块位于东营凹陷尚店油田西南部。本文对该区的东营组进行了精细层序地层学研究。东营组顶底均为不整合面或沉积间断面,东营组为一个完整的沉积层序。在东营期,该区发育了较好的湖侵三角洲相沉积。根据该层序的岩性、沉积旋回特征及现存状况,划分出了低位、湖进及高位3个体系域、9个准层序及41个韵律层。在此基础上,利用研究区内的100余口钻井资料及有关的地震资料,通过14条层序地层学剖面的对比,建立了研究区内的精细的、流动单元级别的、层序地层立体空间格架,为油田生产提供了可靠的资料,并已得到很好的验证,取得了一定的经济效益。  相似文献   

渤中凹陷西斜坡BZ3-8区块东营组东二下高分辨率井震层序及地震沉积学     

黄众  朱红涛  周心怀  杨香华  刘浩冉 《海洋地质与第四纪地质》2012,(1):61-67

渤海海域凹陷由于资料的限制,其沉积相研究多为宏观的区域性研究,制约了储层的精细解释。基于最新采集的高精度地震三维资料,结合地震地层学、层序地层学、地震沉积学等理论方法,开展渤中凹陷西斜坡BZ3-8区块东营组重点目的层,东二下层序高分辨率井震层序分析及其地震沉积学研究。结果表明,研究区南北两侧具有不同的物源体系和沉积相模式。低水位体系域(LST)和高水位体系域(HST)时期,研究区北部物源均形成扇形、朵形的地震多属性及振幅切片异常,对应于扇三角洲沉积;南部物源均形成NE向展布的条带状地震多属性及振幅切片异常,对应于辫状河三角洲沉积。海进体系域(TST)时期,湖平面快速上升导致扇体不发育,仅在研究区北部局部发育小规模的扇三角洲沉积。东二下层序LST(富砂)-TST(富泥)-HST(富砂)的岩相演化规律,充分反映了经典层序地层学理论层序格架中的地层岩相组合分布规律,对储层和烃源岩的预测具有指示意义。  相似文献