砂砾岩体精细划分与对比新探索

通过深入研究东营凹陷北带盐22块砂砾岩体,探索出一套利用常规测井资料可操作的基于沉积动力分析的对比方法。对比岩心及成像测井刻画的沉积剖面与常规测井曲线发现:在测井曲线整体平直的背景上,有2种岩相厚度发育较薄,测井响应明显:代表最大沉积动力的块状巨砾岩相具有高GR、低AC、低CNL的特征,是基准面下降到极低点的沉积响应;代表相对较小沉积动力的平行层理砂岩或砂泥互层相具有(中)高GR、高AC、高CNL的特征,是基准面上升到极高点的沉积响应。以常规测井易识别的岩相"段"代替不易识别的"面"在单井上划分沉积旋回(或基准面旋回);利用高分辨率层序地层学原理实现侧向对比,建立高精度等时层序地层格架。     

FMI测井的地质应用

ＦＭＩ（ＦｕｌｌｂｏｒｅＦｏｒｍａｔｉｏｎＭｉｃｒｏＩｍａｇｅ）测井是在ＦＭＳ（ＦｏｒｍａｔｉｏｎＭｉｃｒｏＳｅａｎｎｅｒ）测井基础上发展起来的，是解决地质问题的又一重要测井技术，它充分体现了测井的高分辨率与连续性的特点，对沉积相研究，储层评价和地层对比等多方面的地质问题研究具有重要的作用。     

CMR和FMI测井在碳酸盐岩储层评价中的应用

碳酸盐岩储层具有的低孔、各向异性和非均质性强的特点,常使得常规测井解释评价变得困难和不确定。应用MAXIS-500测井系列的成像测井(FMI)可以直观识别地层裂缝,确定裂缝发育状况,获取井旁地层构造等信息;核磁共振测井(CMR)可以提供精确的有效孔隙度、孔隙结构等信息。华北油田的应用实例表明,两种测井技术的有机结合可以确定储集空间类型,物性参数,为碳酸盐岩储层评价提供更精确、直观的方法。     

五百梯气田长兴组储层裂缝发育程度的常规测井神经网络预测

川东五百梯气田二叠系长兴组生物礁储层的基质孔隙度和渗透率较低,其高产的主控因素是裂缝的存在,使储层的渗透性有了提高。因此使用常规测井资料对单井裂缝发育程度进行判别预测就成为该地区研究工作的重点任务。通过提取岩心显示裂缝发育段的常规测井响应特征值作为样本,建立了储层裂缝发育程度的常规测井响应BP神经网络预测模型。通过该模型预测的裂缝总缝密度极大程度地与岩心观察相吻合,证明该模型适用于研究区,并且可以用来对该地区的单井裂缝发育程度进行判别预测。     

成像数据对常规测井的刻度

在裂缝和溶孔发育井段由成像测井解释得到的面孔率来刻度常规测井，利用径向基函数神经网络进行训练，初步得到不同的常规测井曲线的相对权系数组合，确定出常规测井曲线对裂缝贡献的相对权系数，同时还建立了成像测井求取的裂缝孔隙度与裂缝常规测井孔隙度的经验关系，它们具有线性相关关系。     

3D seismic and formation micro-imager (FMI) integrated study to delineate depositional pattern of Abu Madi (Upper Miocene) clastic reservoir rocks in El-Wastani gas field,onshore Nile Delta,Egypt

Ten wells (EW-4, EW-5, EW-6, EW-7, EW-8, EW-9, EW-10, EW-12, EW-13 and EW-15) were interpreted using the composite well logs, data of core analysis, gamma-ray logs, formation micro-imager logs (FMI), and 3D seismic data in SEGY format to understand the stratigraphy of the onshore, Nile Delta, Egypt.The amplitude analysis of 3-D seismic horizon slice of Lower Abu Madi rock unit together with the lithostratigraphic correlation through the study area depending on the gamma-ray log “HSGR” (left to right increasing), and the identification of type of bed geometry, nature of bed contacts, type of the sedimentary structures and the dominant formative paleocurrents by using some available borehole micro-resistivity images (FMI) and core photos. All of these techniques are used together to define the different depositional facies and depositional environment of the Messinian clastics (Lower Abu Madi rock unit), which is considered to be the main reservoir in the El-Wastani gas field, onshore Nile Delta, Egypt.The present study of depositional pattern of the Upper Miocene clastics reservoir (Lower Abu Madi rock unit) revealed that it is represented by high sinuous meandering channels or paleo-valley and three types of fluvial facies were defined; channel fill, channel margin, and floodplain basin.     

Characterization of fractured basement reservoir using statistical and fractal methods

This study presents a characterization of fractured basement reservoir by using statistical and fractal methods with outcrop data, seismic data, as well as FMI log data. In the statistical method, fracture intensity and length have been calculated from various outcrop data. The optimum statistical distribution functions of fracture length for outcrops have been identified with the use of discriminant equation derived from Crofton’s theory. The Fisher distribution constant, representing the fracture orientation, has been computed from FMI log data. With the statistical values and distribution functions, a 3D fracture network system has been generated. The result shows that there is no distinction in orientation of the fracture network system, and it excellently matches with the outcrop data. In the fractal method, fractal dimensions of fracture length and strike for the seismic fracture network in areal distribution were calculated; a greater value in fractal dimension means that the fracture network system has intensive fractal characteristics. Meanwhile, vertical distribution and dip angle of the fracture system have been evaluated from FMI log data. The resulting 3D fracture system presents that the overall strike and distribution of the fracture system are excellently matched with those of seismic data.     

基于FMI标准的传动系统模型在环虚拟车辆仿真研究

针对虚拟车辆传动系统模型在环台架仿真问题,在Simulink环境中搭建了整车仿真模型,该模型由SimulationX双离合变速箱和差速器模块与d SPACE ASM发动机及车辆动力学模块共同组成,各模块都根据实车数据进行了参数化。对DCT离合器控制和挡位切换逻辑策略进行了研究,提出了一种基于FMI标准的协同仿真方法,并讨论了协同仿真模型各模块的步长设置。对比了模拟NEDC驾驶循环测试结果与实车转鼓试验台上测得的数据。研究结果表明:在早期系统验证阶段使用模型在环仿真具有较高的实用价值,可以提早发现系统问题并修改需求;该工作可为接下来的硬件在环测试提供了参考基础。     

成像测井在珠江口盆地惠州凹陷古近系勘探中的应用

针对珠江口盆地惠州凹陷海上钻井较少,对深层古近系各种地质情况了解不深的问题,在该地区古近系地层的钻探过程中首次使用了FMI成像测井技术。结合常规测井及岩心资料对惠州A构造的岩性、沉积构造及沉积相特征等进行了有效识别。通过井旁构造分析,对该区断层转换带地震资料处理中的困惑进行了解答,证实了在该区文昌组发现的水平层现象是由地震多次波引起,识别出地震上无法显示的微小断层,并对古水流方向进行了分析,极大地促进了惠州凹陷古近系油气藏勘探的进程。     

裂缝性碳酸盐岩储层裂缝网络测井响应特征——以沾化凹陷富台潜山为例

裂缝测井响应特征研究和裂缝网络模式划分是裂缝性碳酸盐岩储层测井评价的关键.裂缝发育的不均匀性造成储层各向异性,使得测井响应特征复杂化,常规测井评价方法难度大.以沾化凹陷富台潜山为例,选择岩心收获率较高且有成像测井资料的典型层段,利用岩心描述裂缝特征与成像测井资料对比,建立起不同状态裂缝在成像测井资料的显示模式,进而综合标定常规测井资料,分析描述了裂缝网络的常规测井响应特征.在此基础上,利用参数交会法建立测井参数与裂缝特征的相关性,归纳划分出9种裂缝网络模式.该方法为常规测井资料定量识别裂缝类型、研究裂缝网络的分布规律奠定了基础.