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1.
导数换算作为常用的位场数据处理手段具有重要的物理意义。由于实际测量误差和噪声的影响,波数域导数换算存在计算过程不稳定、求导结果精度差的问题。为了降低噪声干扰,提高导数计算精度,提出了在波数域常规导数算子基础上附加Chebyshev低通滤波器的任意阶导数换算方法。通过分析该滤波器的滤波特性,并结合位场异常径向平均功率谱曲线特征,确定了Chebyshev低通滤波法的滤波参数,减少了人为因素对求导结果的干扰。二度体和三度体模型试验表明,与其他3种方法(常规FFT(fast Fourier transformation)法、向上延拓法和ISVD(integrated second vertical derivative)法)相比,该方法计算的导数与理论值的均方根误差最小,求导结果精度较高。在虎林盆地布格重力异常数据处理中,利用该方法计算的垂向二阶导数受噪声干扰小,结果可靠性较高,依此划分出的8条大断裂和11条小断裂在以往研究中均得到证实。  相似文献   

2.
根据台劳级数展开式,将窗口内网格结点位场数据在计算点展开,且对应点两两相加,由最小二乘法求得窗口内网格结点的圆滑滤波算子和二次导数算子,将此算子与观测的位场数据褶积,就可得到位场圆滑后的数据及水平、垂直二次导数。  相似文献   

3.
The paper presents a computational algorithm designed for efficient modelling of apparent resistivity over complex geological structures, using finite element method. The algorithm can be used to study variations of apparent resistivities using any electrode configuration at any point on the earth’s surface, not necessarily regular. A Schlumberger apparent resistivity sounding curve over a buried anticline, is presented here as an example and compared with the corresponding analytical curve, to demonstrate the correctness of the FEM algorithm. The various potential derivatives required for the computation of apparent resistivities evaluated through different electrode configurations have been obtained by calculating the ‘influence coefficients’ using reciprocal theorems, an approach successfully applied in structural engineering. In essence, a set of self balancing nodal currents, obtained from the appropriate derivative(s) of the shape functions of the elements contributing to the point of observation, is applied as the load vector. The resulting quantities corresponding to the potential distribution in traditional finite element method, then, turn out to be the potential derivatives at the point of observation for different positions of the current electrodes. These are known as influence coefficients. The continuum nature of the domain beyond the region of interest has been modelled by using ‘infinite elements’ across which the potential is assumed to decay exponentially.  相似文献   

4.
本文首先讨论了强化垂直聚焦测深法(简称聚焦测深法)的视电阻宰表达式,提出了在实际工作中代换该法的简单装置及其观测方案。其次,详细分析了利用线性滤波法计算的聚焦测深法ρs理论曲线,指出了似增层性质及多种因素对ρs曲线的形状和特征点极距的影响作用。最后阐明了聚焦测深法在地质效能上不具有定勘探深度的原因。  相似文献   

5.
位场垂向导数广泛应用于位场数据处理与解释当中,目前求取位场各阶垂向导数方法大致可以分为两类:①在频率域进行;②在空间域进行。针对这两类方法存在着稳定性较差的问题,这里介绍了计算位场各阶垂向导数的ISVD算法,并通过对单一地质体模型和地质体组合模型产生的布格重力异常进行处理分析,证明了ISVD算法在计算位场各阶垂向导数时,特别是在计算位场高阶垂向导数时,比在频率域及空间域计算结果具有较好的稳定性,ISVD算法能够有效地识别出浅层小尺度地质体边界。为了验证该方法对实际资料的处理效果,对某区块实际布格重力异常数据应用ISVD算法试算各阶垂向导数,结合地质背景等资料划分出断裂体系。结果证明,应用ISVD算法计算的位场各阶垂向导数,对于确定浅层小尺度地质体边界有较好的效果。  相似文献   

6.
本文以垂直磁偶极子发射,接地导线测量这样一种发一收装置为例,讨论了求解时间减电磁场问题的计算方法,具体思路是:用线性滤波法,先求解频率域问题,然后且Gaver-Stehfest逆拉氏变换法将频率测深正演问题转化为相对应瞬变测深(时间域)正演问题,得到了垂直磁极子场中,水平层状介质表面瞬变电磁场分量的近似表达式,由此计算了视电阻率曲线,并从理论上探讨了瞬变测深视电阻率曲线的垂向分辨能力,本文试图对中  相似文献   

7.
基于离散余弦变换(DCT)的重力异常垂询二阶导数的计算方法是笔者提出的新方法。以无限长水平圆柱体为例研究了DCT法的计算规律:模型实验证实,该法计算的无限长水平圆柱体重力异常垂向二阶导数的精度与采样闻隔、剩余密度及圆柱体半径大小无关。与圆柱体轴心埋藏深度成正比。通过分析给出了基于DCT的合适的线性滤波方式,滤波后的重力异常垂向二阶导数与理论二阶导数拟合效果好,具有较高的计算精度。  相似文献   

8.
The present study deals with the delineation of lineaments over Sir Creek offshore and its surroundings from EGM2008 gravity data using various derivative techniques owing to their costeffectiveness in prospective hydrocarbon exploration. Initially, 2-D and 3-D synthetic models have been generated with vertical prismatic objects at different depths. The effectiveness of total horizontal derivative (THD) technique has been established by comparing with E-W and N-S Horizontal derivatives and First Vertical derivative techniques. The residuals of Bouguer gravity data have been estimated with different cut-off wavelengths. Further, the residual anomaly map has been enhanced by the derivative techniques for the delineation of the structural features. Possible depths of the delineated lineaments have been estimated using Euler deconvolution of the Bouguer gravity data, which indicates maximum clustering over the delineated lineaments. It is observed that most of the lineaments are in the depth range of 1.0 km to 5.5km, which correlate well with the previous seismic studies. The present study reveals that the major lineament trends in the N-S, E-W and NNW-SSE directions followed by NE-SW, NW-SE and ENE-WSW directions. These major lineament trends are due to the tectonic activities occurred during Precambrian and Cretaceous period. Different small circular features, rectangular features and shorter wavelength features have also been identified, which could be the key parameter for mapping potential location for hydrocarbon exploration.  相似文献   

9.
激发极化法是寻找硫化物金属矿床的一种有效方法,被广泛应用于矿产勘查中.在内蒙古阿荣旗矿产远景调查中,运用时间域激发极化法,通过激电中梯扫面测量后,绘制视电阻率与视极化率等值线平面图,迅速地圈定激电异常.依据地质与化探调查结果,选择其中3个激电异常区做激电测深.通过对激电测深数据反演,得到极化率与电阻率断面图,确定了潜在矿(化)体的形态.  相似文献   

10.
The research site is the whole landmass of the Federal College of Education, Zaria, seated on basement complex of north-central Nigeria. Direct current resistivity geophysical method was employed to characterise parameters such as the basement depth and topography, aquifer depth and thickness, weathered basement distribution as well as mapping of orientations of fractures and faults present in the premises using radial sounding technique. The conventional vertical electrical sounding (VES) Schlumberger array was carried out at 40 stations, and eight of which were radial stations. Radial sounding was used to establish resistivity anisotropy which gives clue for the choice of consistent VES profile direction used throughout the fieldwork. Results from the resistivity interpretation suggest three layers in most parts of the premises with some minor occurrence of two and four layers. The first layer (topsoil) has its thickness ranging between 3.5 and 14.0 m; second layer (weathered basement) thickness ranges between 9.0 and 36.5 m, while the third layer (fresh basement) is deepest (40.1 m) towards the eastern corner of the area. The aquifer depth ranges from 1.5 to 4.0 m with a thickness range of 5.0 to 14.0 m. The thickest aquifer occurs around the centre to the west in the area. Results from radial sounding show presence of resistivity anisotropy, an insight to fracturing and faulting; this is more pronounced around the west-central part of the premises.  相似文献   

11.
通过收集和研究莱芜富铁矿区早期的地面磁测资料,结合近几年在铁矿深部找矿中的理论及找矿实践,经过数据处理获得地面磁测ΔZ垂向二次导数异常,用以分解磁异常和圈定深部磁铁矿体的大致分布范围,在莱芜市石家泉地区找到了厚度较大的隐伏富铁矿体,初步估算铁矿石资源量在千万吨以上,取得了良好的找矿效果,同时对该地区深部铁矿找矿起到一定的借鉴。  相似文献   

12.
The present study is an approach to detect the sea/freshwater interface in Sidi Abdel Rahman area, northwestern coast of Egypt using both vertical electrical sounding and time domain electromagnetic. The measured vertical electrical soundings are interpreted in 1D and 2D manner. The 1D inversion is carried out using the commercial software (RESIST), whereas 2D resistivity nonlinear iterative inversion scheme based on the finite element technique and regularization method was used. The time domain electromagnetic stations are interpreted using Temixxl-4 software by Interpex Ltd. To have the advantages of the vertical electrical sounding in shallow depths and time domain electromagnetic in deep depths, a joint inversion algorithm is applied for the electric profile and the nearby electromagnetic profile. Very low resistivity values have been observed near the coast as well as a considerable salt/fresh water interface. The tip-top portion of the interface lies approximately 1,000 m from the shore line.  相似文献   

13.
阳山金矿自1997年发现以来,进行了不间断的勘查和科研工作,矿床规模不断扩大。其中阳山矿段发现23条金矿脉,以2号脉和13号脉为主,估算金资源量12957kg。前期激电中梯度测量高极化率异常显示较强,说明阳山矿段矿脉群还有继续研究的潜力。本文将衍生指数法应用于激电测深工作中,对13号脉群西延段进行研究,掌握了其空间分布规律,经钻孔验证,取得了很好的效果,对本区浅部矿产勘查具有指导意义。  相似文献   

14.
The proposed site for a new solid waste disposal facility was identified by a municipal government in a north Florida area characterized by Miocene Hawthorn Group sedimentary sequences and active karst development. An evaluation of the sinkhole potential and subsurface stability was conducted with a total of 300 electrical resistivity Wenner array sounding traverses with electrode spacings extending to 30 m. Data were interpreted to identify vertical sequences of the Hawthorn Group confining layer, and the underlying Ocala Limestone. Electrical evidence identified an intermediate, discontinuous limestone layer present in limited areas, but absent in much of the area investigated. No evidence was detected to identify breeches within the confining layer over the Floridan Aquifer within the Ocala Limestone. The data were combined with lithologic logs from deep boreholes to prepare a series of continuous and interconnecting fence diagrams to portray the geologic configuration throughout the proposed site. The results demonstrate the value of electrical resistivity measurements to augment borehole data in economical investigations of sinkhole potential in karstic terrains.  相似文献   

15.
从原理上分析了音频大地电磁阻抗相位在静位移和垂向电性异常体影响下的变化特性,并采用二维有限元方法进行了正演模拟。考虑到阻抗相位在静位移和真实垂向异常中的响应差异,认为利用阻抗相位开展综合解释对于识别二维垂向电性异常具有十分积极的意义。理论模型计算和工程实例表明,基于阻抗相位的综合解释方法对于识别二维垂向电性异常具有较好的应用效果。  相似文献   

16.
曲潭测区内地形较平坦,多为第四系覆盖,表层土质较均匀,接地条件较好,选择五极纵轴电测深法在区内寻找岩溶地下水,通过视电阻率及激电二次场的测量,对物探异常的解译和深部钻孔验证,成功找到日出水量达千吨以上的岩溶地下水,为今后在灰岩地区寻找岩溶地下水提供借鉴意义。采用物探方法寻找岩溶地下水是一种不可替代的勘查方法,可以减少单纯钻探成井的盲目性,提高找水的成功率。  相似文献   

17.
面向21世纪的海洋测深(改正)新技术   总被引:7,自引:0,他引:7  
首次提出了随船一体化测深改正新概念及新方法。GPS的应用已使海洋测量的主要矛盾转移到高精度的测深方面。传统的方法已同精度测图的需要。为此在测深改正新技术基础上提出了研制海洋三维测量仪的新设想。这对于海洋测量由2+1维过渡到真3维具有重要理论意义,对海底地形测量来说具有重大应用价值。  相似文献   

18.
一维层状介质大地电磁模拟退火反演法   总被引:17,自引:0,他引:17       下载免费PDF全文
师学明  王家映 《地球科学》1998,23(5):542-546
大地电磁模拟退火反演法是一种最优化的非线性反演方法,与传统的线性反演方法相比该方法具有:(1)不依赖于初始模型的选择;(2)能寻找全局最小点而不陷入局部极小;(3)在反演过程中不用计算雅可比偏数矩阵等优点;通过对各种类型的大地电磁测深理论曲线试算,结果表明模拟退火法能准确地自动反演地电参数(地层电阻率,厚度)最后对实际资料进行了处理,取得了较好的效果。  相似文献   

19.
自Pelton等发表第一篇直接电测深数据的二维反演文章以来,电测深数据的二维反演解释已广泛应用于资源勘探和环境监测,并取得一定效果。然而,由于该方法中加入了人为确定的平滑约束,其反演解释结果具有很大不确定性,使其在实际生产中普及应用受到限制。因此,如何在现有方法的基础上进一步改进完善成为该方法普及应用的关键。为了使反演解释结果既忠于实测数据,又合理地反映地下介质的变化,作者在本文中讨论了基于最大熵谱原理的剩余信息量最小准则实现电测深数据的二维自动反演。作者在文中还介绍了正演计算和偏导数求取中,提高精度和计算效率的技巧。用三个数值模式算例对本文的自动反演方法进行了验证。数值模拟结果表明,基于剩余信息量电小准则的二维自动反演给出的解释结果基本不受人为因素影响,能反映地下介质电阻率的详细变化。  相似文献   

20.
CSAMT法在西北深部探矿中的应用研究   总被引:3,自引:0,他引:3  
可控源音频大地电磁法(英文简称CSAMT)是20世纪80年代中期兴起的一种测量卡尼亚电阻率和相位的电磁测深技术。由于它探测深度大、横向分辨率高、抗干扰性能强,因此在深部找矿的勘探中有着重要指导意义。笔者使用美国ZONGE公司生产的GDP-16大地电磁测量系统,利用的工作频率为1-4096Hz,对西北某矿区的外围和深部进行了实际勘探。证明该方法在矿区深部及外围找矿(主要是铁矿)具有有效性。  相似文献   

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