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分析了岩心电性实验的内涵,介绍了油藏条件下岩石电学性质的研究现状以及对岩心电性实验方法的冲击.结合目前对不同地层特性岩石的电学性质的认识,就复杂储层评价的岩心电性实验方法、岩心电性实验技术装备、岩心电性实验技术规范化、岩心数值实验方法等方面对岩心电性实验的研究方向做了展望,认为：①岩心电性实验方法应立足于储层岩石的岩性、物性、孔隙结构、非均质性等地层特性;②系统地模拟和控制储层的温度、压力、润湿性条件、毛管与电性平衡等油藏条件,并使各种相关技术规范化,是其发展的必然趋势;③岩心数值实验方法可能作为实验室岩心电性实验的辅助手段之一在储层含油性评价中发挥作用. 相似文献
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《地球物理学进展》2015,(5)
针对中国东部某盆地D凹陷盐S块砂砾岩岩性复杂,非均质性强,岩石骨架对测井曲线的影响比常规砂岩储层突出的特点,在综合利用岩心、录井和常规测井资料的基础上,分析了S块沙四段的储层特征,建立了有效储层的判断标准,并对砂砾岩的有效储层进行了划分.研究结果表明,D凹陷S块有效储层的物性标准为:物性标准为孔隙度大于等于6%,渗透率大于等于0.85×10-3 um2;有效储层的电性标准为:声波时差大于等于197us/m,补偿密度小于等于2.57g/cm3,地层电阻率大于等于15Ω·m.核磁共振测井对于储集物性的反映具有直接性,充分利用核磁共振测井在分析储层的渗流能力和优势. 相似文献
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陆域天然气水合物通常发育于冻土层下方破碎带和岩层裂隙处,其储层会表现明显电性各向异性特征.音频大地电磁法（AMT）能有效探测陆域水合物储藏范围,且不易受高阻冻土层的压制和干扰,可用于陆域天然气水合物探测研究.本文采用AMT对角各向异性二维正演方法,对多种陆域天然气水合物各向异性储层模型及相关参数进行了模拟试算,分析其视电阻率和相位响应特征.结果表明AMT能清晰显示各向异性储层空间位置和分布情况,并对储层的水合物饱和度变化以及储层数量等特征都有所反映.天然气水合物电性各向异性模拟研究为这一新型潜力能源的勘查工作提供了新的思路. 相似文献
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DB气田非均质储层级别划分及常规测井识别方法 总被引：1，自引：0，他引：1
DB气田以裂缝-孔隙型、孔隙型岩屑砂岩储层为主,非均质性强,裂缝发育程度是决定产能高低的关键因素之一.立足于储层的录井、岩心分析和测井资料,开发了储层级别划分和常规测井识别储层级别的方法.首先,定义了每米产能指数作为标准化的产能参数;其次,基于产能参数与储层物性参数关系的考察,筛选综合物性参数(孔隙度和总渗透率的乘积)作为储层级别划分的评价指标,将DB气田储层分成了2个级别,给出了分级的物性标准;最后,应用主成分分析法计算了综合主成分,基于综合主成分与每米产能指数交会图给出了应用常规测井资料识别储层级别的标准.2口井的应用效果表明,依据上述方法划分及识别的储层级别与生产情况吻合得较好. 相似文献
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长期以来,矿井水害是煤矿开采的重大安全隐患之一,严重威胁着煤矿的安全高效生产,防止突水事故的发生已成为煤矿亟待解决的重要问题.因此利用新技术、新方法开展煤矿富水区精细探测具有重大意义.本文采用大功率广域电磁法,以高频率密度、多频同步收发技术对新元煤矿六采区3 km2范围内进行了面积性勘探工作.通过对实测数据的处理与反演,获得了1200 m深度范围内的电性结构,并对主要目的层位进行了划分,识别断裂8条、富水异常区6处,最后通过巷道钻探验证了探测方法的有效性.该工作说明了广域电磁法可以实现煤矿富水区的精细探测,为矿区后续安全生产提供了可靠依据. 相似文献
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本文通过对高密度电阻率法勘探中的长测线多排列数据进行连接处理,实现了同一测线采用同一套参数的规范化处理,克服了因不同排列采用不同参数处理而导致假异常和信息丢失等弊端,同时解决了在成像时,因各个电性剖面的色标值不一致,剖面坐标与实际桩号对应不直观,导致对整个区域的电性趋势认识产生误导的问题.从实例处理来看,能为整个勘探区提取更丰富的电性信息,不但突出了整条测线的地下电性趋势,更客观、更全面地把握和认识勘探地区的电性分布规律,而且从宏观上把握了一些比较隐蔽的地质现象. 相似文献
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在矿井瞬变电磁超前探测数据处理和解释中,为了更好地识别巷道前方含水体电性分界面,利用扩散场与波动场间的函数关系,将矿井瞬变电磁法超前探测中瞬变电磁波场转换为拟地震波场,实现波场转换.同时,为了解决波场转换后信号幅值偏弱,以增加信噪比利于解释,利用雷达的合成孔径方法对波场转换后的拟地震信号进行相关叠加处理.将矿井瞬变电磁法巷道超前探测的同一测点不同探测方向的数据作为孔径数据进行合成孔径成像,以突出弱异常而提高信噪比,结合应用实例验证了方法的效果.研究表明,矿井瞬变电磁法合成孔径成像方法能够提高电性界面信息的信噪比和界面几何分辨率,对矿井瞬变电磁法精细超前探测含水构造具有重要的理论意义和应用价值. 相似文献
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《地球物理学进展》2017,(2)
齐家北地区高台子油层为高含钙致密储层,钙质发育导致部分水层的电阻率大幅提高,高阻水层、油水同层、油层在电测曲线上具有相同的电性特征,给以电测特征为解释基础的油层、油水同层的判别带来极大的困难.针对上述解释技术难题,本文在储层"四性"关系研究的基础上,提出了剥层法:其核心思想是根据各流体类型储层典型的电性特征,将干层、水层、油水同层从其他储层中逐一剥离出来.即依据干层的电性特征,首先将干层与产层区分开;再利用水层识别图版,将水层特别是钙质水层与油水同层区分开;最后利用油层与油水同层解释图版,再将油层与油水同层区分开来.该方法尽可能地降低干层、水层特别是钙质水层对油水同层和油层解释的干扰,提高测井解释符合精度.研究表明:感应测井曲线可反映致密砂岩孔隙中低阻可动水含量,是钙质水层、油水同层解释的敏感曲线;多曲线联合定性识别方法与解释图版相结合可提高油水层测井解释符合率;所建立的测井解释图版精度均达到了90%以上,经过3口实际试油井进行的背对背验证,油层的测井解释符合率达到了100%. 相似文献
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福建沿海、台湾海峡GPS观测分析及地球动力学特征研究 总被引：1，自引：1，他引：1
利用 3期GPS联测结果所获得的福建沿海地壳水平运动信息 ,采用ITRF94全球框架为基础的GPS测站地壳运动模型及其处理软件 ,对所获得的观测数据进行处理和精度分析。得到福建省高精度的GPS测站大地坐标、边长及其位移矢量 ,其精度达到 1 7×10 - 8。计算了福建地壳运动速率、主应变率 ,东西与南北向线应变率、面应变率、剪应变率、大地转动率和最大剪应变率等值线并给出了它们的分布图象。根据多年形变和现今GPS观测资料 ,分析福建地壳垂直运动与水平运动 ,显示区域应力场优势分布特征。最后 ,对福建沿海及台湾海峡地壳动力学特征作了初步的探讨 相似文献
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Zhivanovich I. Solov’ev A. A. Efremov V. I. Miller N. O. 《Geomagnetism and Aeronomy》2020,60(7):865-871
Geomagnetism and Aeronomy - Two main features define a sunspot as an object: a strong magnetic field and a low umbra temperature. The same can be said about a facular knot, in the center of which... 相似文献
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Michele Caputo 《Pure and Applied Geophysics》1964,57(1):66-82
Summary Adopting thePizzetti-Somigliana method and using elliptic integrals we have obtained closed formulas for the space gravity field in which one of the equipotential surfaces is a triaxial ellipsoid. The same formulas are also obtained in first approximation of the equatorial flattening avoiding the use of the elliptic integrals. Using data from satellites and Earth gravity data the gravitational and geometric bulge of the Earth's equator are computed. On the basis of these results and on the basis of recent gravity data taken around the equator between the longitudes 50° to 100° E, 155° to 180° E, and 145° to 180° W, we question the advantage of using a triaxial gravity formula and a triaxial ellipsoid in geodesy. Closed formulas for the space field in which a biaxial ellipsoid is an equipotential surface are also derived in polar coordinates and its parameters are specialized to give the international gravity formula values on the international ellipsoid. The possibility to compute the Earth's dimensions from the present Earth gravity data is the discussed and the value ofMG=(3.98603×1020 cm3 sec–2) (M mass of the Earth,G gravitational constant) is computed. The agreement of this value with others computed from the mean distance Earth-Moon is discussed. The Legendre polinomials series expansion of the gravitational potential is also added. In this series the coefficients of the polinomials are closed formulas in terms of the flattening andMG.Publication Number 327, and Istituto di Geodesia e Geofisica of Università di Trieste. 相似文献
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D. Zidarov 《Pure and Applied Geophysics》1973,105(1):655-668
Summary The paleomagnetic field (declination and inclination) in different geological epochs is represented through the field of the so-called magnetic dipole. The optimal dipole coordinates so obtained show that during older geological times the optimal dipole lay outside the earth's centre and moved towards and around the earth centre. It is supposed that the optimal dipole trajectory in the earth coincides with earth core trajectory. This core motion brought about a motion of the masses of the mantle in a direction opposite to the motion of the core. This in turn brought about the break-down of Pangea and the separation of the continents. The drift of the continents, the relative changing of the earth's rotational axis and many other geological and geophysical phenomena may be explained through such a motion, that is through the motion of an eccentrical core towards the earth centre. 相似文献
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Prof. Dr. W. A. Heiskanen 《Pure and Applied Geophysics》1958,41(1):1-18
Summary The author mentions the aims of the World-wide gravity project he established in the Ohio State University in Columbus, in 1950. He outlines the practical procedure of the gravimetric computations of the undulationsN and the vertical deflection components and and emphasizes that only by the global international cooperation and additional gravity observations at sea carried out during the last decade it has been possible to gather to Columbus the needed gravity material. Since there exist still large gravimetrically unsurveyed areas it is of vital significance to study what gravity anomalies are best to be used for these regions. The given figures concerning the accuracy of theN, and , estimated theoretically and obtained in practice, indicate that in the gravimetrically well surveyed parts of the world like in Europe and the United States we can get gravimetrically on basis of existing gravity material theN-values with accuracy of about 5–10 meters, and and with the accuracy of about 1. The geoid undulationsN are already computed in Columbus for more than 6000 points of the northern hemisphere. The sample maps show the interesting geoid of Europe and vicinity between the latitudes 60° and 30° and longitude 5° W and 30° E, drafted on basis of more than 1000N-values computed at the corners of 1°×1° squares. It is interesting to realize that the geoid undulations in all this area are positive, the extreme values being between 40 and 50 meters. The geophysical significance of the geoid maps of this kind is pointed out. 相似文献
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针对我国当前较具典型的几种地震社会心理，指出职能部门疏导、防治的工作重点，并从顺应国情、民情及国家经济体制改革的方向出发，提出相应的对策建议。 相似文献
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本文搜集了2001—2013年间在太行山与燕山构造带交汇部位先后布设的4个宽频带流动地震台阵和首都圈固定地震台网共192个台站记录到的全球5.5级以上远震事件波形资料,综合采用接收函数H-κ和CCP叠加分析获得了134个基岩台站下方的地壳厚度和泊松比结果.综合分析与前人研究相吻合但更加精细的地壳约束分布信息,发现研究区域的地壳厚度和泊松比在整体上呈现出从西北到东南方向渐变的特征,在南北重力梯度带两侧及其附近呈现出明显的小尺度地壳结构和物质组分的差异,且可明显区分出太行山地区和燕山构造带及盆山交界处的地壳厚度与泊松比的相对差异,这可能反映了这些地区在华北克拉通的构造演化过程中所经历的不同地壳改造过程. 相似文献
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Geomagnetism and Aeronomy - The behavior of the correlation between the radial BR and normal BN components of the interplanetary magnetic field (IMF) in the dependence on the time, the flow type of... 相似文献
19.
Kenneth A. Goettel 《Surveys in Geophysics》1976,2(4):369-397
Progress in understanding the condensation of planetary constituents from a solar nebula necessitates a re-examination of models for the origin and composition of the Earth. All models which appear to be viable require the Earth to have an Fe–FeS core and the full, or nearly full, solar (i.e. chondritic) K/Si ratio. The crust and upper mantle do not contain the requisite potassium for the entire Earth to have the solar K/Si ratio. Therefore, these models require that much of the Earth's potassium, about 80–90%, must be in the deep interior—in the lower mantle or in the core.The hypothesis that a substantial fraction of the Earth's potassium is in the Fe–FeS core is based on the chalcophilic behavior of potassium. Data including the stability of K2S, the occurrence of potassium in sulfide phases in meteorites and in metallurgical systems, and most importantly, experiments on potassium partitioning between solid silicates and Fe–FeS melts support this hypothesis. The present data appear to require at least several percent of the Earth's total potassium to be in the core. Incorporation of much larger amounts of potassium into the core, possibly most of the 80–90% of the Earth's potassium which is postulated to be in the deep interior, is not contradicted by the present data. Additional experimental data, at high pressures, are required before quantitative estimates of the core's potassium content can be made.It is likely that40K is a significant heat source in the core. Decay of40K is a plausible energy source to drive core convection to maintain the geomagnetic field, and to drive mantle convection and seafloor spreading. 相似文献
20.
1 工作特点美国的地质学、地球物理学和海洋学家们利用他们所掌握的科学知识 (地球物理、地质和历史等方面的知识 )来确定水资源、矿产资源和能源等的状况 ,围绕如何保护环境 ,预测未来地质灾害 ,利用土地资源等问题开展工作。他们利用先进的仪器对地球和水资源进行分析研究。地质学家 ,同时也包括地球物理学家们研究地球的过去、现在和未来。例如他们研究地球运动 ,试图预报地震与火山会在何时何地发生 ,以及它们对周围地区的影响。虽然地质学、地球物理学、海洋学领域密切相关 ,但也有很大的不同。地质学家研究地球的构成、过程和历史。… 相似文献