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1.
地震-重力联合反演可以降低多解性,针对大勘探范围内岩石波速-密度关系存在较大散布的问题,引入交叉梯度结构约束构建统一的目标函数是一种有效的解决方案。利用台湾海峡南部HX-13测线进行验证:由于火成岩侵入体的存在,部分区域难以拾取可靠的地震初至,常规的走时反演无法准确恢复基底面的形态。搜集研究区的船测重力资料,根据地震地质条件和数据特点设置合适的反演参数,实现基于物性和结构双重约束的重力-地震联合反演。由对反演结果的分析和解释可以看出,该方法可在很大程度上弥补地震数据不完备的缺陷,使反演过程稳定,并提高模型的可靠性。  相似文献   

2.
Full waveform inversion( FWI)is a high resolution inversion method,which can reveal detailed in-formation of the structure and lithology under comPlex geological background. It is limited by many kinds...  相似文献   

3.
青藏东缘三维Moho界面的位场遗传算法反演   总被引:7,自引:5,他引:2  
针对波数域中Parker-Oldenburg位场迭代反演方法中存在向下延拓的问题,提出了利用改进的遗传算法进行三维Moho界面反演的位场遗传反演方法。通过模型试算证明了该方法的有效性和稳定性,并利用该方法反演了青藏高原东缘三维Moho界面的分布。  相似文献   

4.
NMR logging can provide the permeability parameter and abundant stratigraphical information such as total porosity,oil,gas and water saturation,oil viscosity,etc. And these physical parameters can be ob- tained by T2spectrum inversion. NMR inversion is an important part in logging interpretation. The authors de- scribe a multi-exponential inversion algorithm,solid iteration redress technique (SIRT),and apply the algo- rithm in real data and compare the results with those based on singular value decomposition (SVD). It shows that SIRT algorithm is easier to be understood and implemented,and the time spent in SIRT is much shorter than that of SVD algorithm. And the non-negative property of T2spectrum is much easier to be implemented. It can match the results based on SVD very well. SIRT algorithm can be used in T2spectrum inversion for NMR analysis.  相似文献   

5.
论多种数据联合反演的模式及算法   总被引:9,自引:3,他引:6  
针对日益丰富的数据资料,综述了大地测量反演的发展进程,论述了多种数据联合反演的意义和必要性,给出了兼顾权比确定的大地测量、地震和地质三类数据的联合反演模式及采用水准测量、GPS和重力三种数据联合反演断层参数的具体公式,特别介绍了求解优化问题所有全局最优解的区间算法,并给出了基本算例,结果体现了区间算法无可比拟的优越性及其在大地测量反演领域中的应用前景。  相似文献   

6.
Large-scale gravity 3D interpretation depends on efficient and high-resolution 3D inversion processing of massive data.The authors applied the conjugate gradient method with minimum support function and prior model constraint to reduce multi-solutions in gravity inversion.Based on the parallel programming and compu-ting platform NVIDIA CUDA with C++language, we achieve fast 3D gravity inversion by adopting GPU parallel technique into the most time consuming part relating to sensitivity matrix.The results of theoretical model show that the abnormal body can be clearly located and the inversion speed is improved greatly.Comparing with in-version speed of the Matlab program, speed of inversion with GPU parallel technique has improved more than 100 times under the hardware condition of Geforce GTX 1060 graphics card.  相似文献   

7.
With the development of gravity gradient full tensor measurement technique , three-dimensional (3D) inversion based on gravity gradient tensor can provide more accurate information .But the forward calcula-tion of 3D full tensor sensitivity matrix is very time-consuming, which restricts its development and application . According to the symmetry of the kernel function , the authors reconstruct the underground source of geological body to avoid repeat computation of the same value , and work out the corresponding relationship between the re-sponse of geological body to the observation point and the response of reconstructed geological body to the obser -vation point .According to the relationship , rapid calculation of full tensor gravity sensitivity matrix can be achieved .The model calculation shows that this method can increase the speed of 30-45 times compared with the traditional calculation method .The sensitivity matrix is applied to the multi-component inversion of gravity gradient .The application of this method on the measured data provides the basis for the promotion of the meth -od.  相似文献   

8.
There is not much correlation between sand content and P-wave impedance in faulted basins , and the prediction results cannot be guaranteed .Due to sedimentary facies control , there is inconsistency between sand content and low frequency trend of P-wave impedance , causing problems for seismic inversion modeling , which directly affects final seismic inversion results .The acoustic impedance increases with burial depth .When the same layers of sand and shale formation endure different compaction , the acoustic impedance values will be dif-ferent .Therefore , The seismic inversion modeling of faulted basin is different from that of conventional basins . The authors built an inversion model using uncompact sandstone percentage , directly compensating for the low frequency trend of the inversion model .In addition, the model's intermediate frequency is similar to P-wave im-pedance , ensuring that the inversion results are converged correctly .The final results of the inversion can be used directly as sandstone percentage .The aforementioned method was applied to Liaohe Beach in the Bijialing region and obtained optimistic lithology inversion effects:the results were correlated well with the depositional facies map and with lithology in the well borehole .The inversion results can be used to define the sand body horizontally and can separate sand bodies vertically , which is very difficult on conventional seismic section . Therefore the inversion results played an important role in reservoir prediction .  相似文献   

9.
Based on the relationship between the diameter and buried depth of goaf,the authors establish the forward modeling by Res2dmod and inverse the model by Res2dinv. Thus,three kinds of models are obtained:the model of single resistivity anomalous body,model of double different distance resistivity anomalous body,and model of layered resistivity anomalous body. Using forward and inversion,the image of detection is simulated,and the reliability is proved by comparing with the engineering examples.  相似文献   

10.
Focusing inversion is accomplished by the iterative of abnormal source to make the image gradually focused. It can better reflect the underground geological geometry and physical parameters. The model experiments in the study show that gravity focusing inversion allows inversion image stabilization and polymerization, which solves the multiple solutions and instability of inversion and so on. The method is applied to measured gravity data processing of certain region of Changbai Mountain, compared to Euler deconvolution, the results show that the method for determining the horizontal position and depth of underground anomalies has good efforts.  相似文献   

11.
采用正则化平滑因子方法,对重力台站连续观测资料进行处理和讨论,尝试分离同震信号。结果表明,该方法可以有效地分离并获取同震重力效应和地震波信号,且估算的同震重力效应与理论模拟有较好的一致性,可为快速反演地震参数及地震预警提供更多的约束条件。  相似文献   

12.
The processing and interpretation of gravity and gradient data plays an important role in geophysics. The cross gradient joint inversion is usually used for achieving structure coupling of multiple geophysical mod-els.In order to realize the coupling of gravity and gravity tensor data, the authors analyzed each component. The results show that different types of data contain different direction information, and derived the joint inver-sion based on cross gradient function and applied it to model data.The theoretical model results show that the cross gradient method can reduce the multi solution and significantly improve the resolution of the inversion. The method was also applied to inverse the gravity tensor data in Vinton salt dome, showing that this method can get higher resolution results than the separate linear inversion, and be closer to the real density from drilling data.  相似文献   

13.
基于闭锁剪力模式与地震位错理论,提出构造“等效位错”来描述地震的震前“闭锁剪力”,并建立震前地表重力变化与“等效位错”之间的定量化模型。考虑到粗差干扰,采用稳健-贝叶斯最小二乘方法对姚安MS6.0地震的“等效位错”进行反演。结果表明,其孕震源为高倾角走滑型,“孕震矩”与USGS给出的矩震级接近,证明该方法可依据震前重力四象限图像对未来震源特性和孕震强度进行预测。  相似文献   

14.
In the conditions of low Signal-to-Noise Ratio(SNR) of seismic data and a small quality of log information,the consequences of seismic interpretation through the impedance inversion of seismic data could be more precise. Constrained sparse spike inversion(CSSI) has advantage in oil and gas reservoir predication because it does not rely on the original model. By analyzing the specific algorithm of CSSI,the accuracy of inversion is controlled. Oriente Basin in South America has the low amplitude in geological structure and complex lithologic trap. The well predication is obtained by the application of CSSI.  相似文献   

15.
采用重力异常数据,在频率域内通过Parker-Oldenburg反演算法计算南海及邻区的莫霍面深度。通过EGM2008重力场模型联合GOCE重力场模型,计算研究区的自由空气重力异常;通过重力场分离,得到莫霍面起伏引起的重力异常,用于反演莫霍面深度。计算结果与地震剖面计算的莫霍面深度结果平均偏差1.59 km,标准偏差1.9 km。结果表明,南海及邻区的莫霍面深度分布具有明显的区域化构造特征。  相似文献   

16.
Qingchengzi ore concentration area in Liao-Ji rift is an important lead-zinc ore area of China,and the deep prospecting in this area has great prospects.Based on the spatial occurrence of ore bodies the Pb-Zn deposit can be divided into three types:layered,vein-shaped and pinnate.The deep geological conditions in this area are deduced by analyzing the tectonic evolution process and rock mass gravity inversion.The tectonic evolution of Liao-Ji rift can be divided into three stages:Paleoproterozoic extension period,Mesoproterozoic compression period and Mesozoic reactivation period.The magmatic activities in the Indosinian epoch led to the distribution pattern of the present deposits.According to the gravity inversion,Shuangdinggou-and Xinling rock masses on the north and south sides of the mining area are connected in the deep.The connected rock body might be distributed in the entire mining area.Xinling rock mass may be a branch extending from Shuangdinggou rock mass along the northeast trending fault,the connected rocks provide magmatic hydrothermal fluid for the final,folds and faults result in different types of ore body shapes.  相似文献   

17.
重力勘探作为一种快速普查方法,在深部地质构造研究、区域地质构造划分及找矿勘探中均已取得显著的地质效果。自80年代后期,由于在重力测地工作中使用红外测距仪及高精度GPS定位技术,确保了重力测点位置及高程有较高的精度;在重力观测中普遍采用目前世界上精度最高的Lacoste型重力仪进行基点联测,采用对恒温系统改进后的Worden重力仪进行重力测点观测,使得重力测量的质量及精度都有了很大提高,为扩大重力法的应用提供了条件。本文给出的一例是;在我国某含油沉积盆地上,根据对实测1:25000高精度重力资料(布格重力异常总观测均方误差:60×10 ̄-8m/s ̄2)的处理及约束信息下多层界面反演结果,确定有利油气聚集的圈闭范围,推断含油层的大致规模。  相似文献   

18.
The start depth in gravity anomaly inversion is discussed in this paper, and a new method called “test comparing method” is presented to determine the start depth when both boring data and seismic data are not available. Anticline and syncline density interface models are designed to test the method; the calculated result agreed well with the designed value, which proved that the new method can be used to determine the start depth in the gravity anomaly inversion when boring data and seismic data are not available. Contribution No. 3370 from the Institute of Oceanology, Chinese Academy of Sciences. Project 49625609 supported by NSFC, and Young Scientist Lab. of Submarine Hydrothermal Activity Research.  相似文献   

19.
The traditional gravity modelling methods fail to deal with ambiguity zones.These zones are likely to be associated with uncertain boundaries.Source boundaries can be divided into "hard" and "soft" types."Hard" boundary stands for distinguished margin of discontinuity of source distributions.Traditional modelling method is based on this type of boundary.Uncertain boundaries of ambiguity zones belong to"soft" boundary. The authors put forward the uncertainty analysis because lots of uncertainty factors need to be taken into consid-eration.Any powerful system designed to interpret gravity data for a real source distribution must be able to deal with uncertain information.Uncertainty analysis ( UA) is a useful tool to estimate the ambiguity of the data in-terpretation.It is often applied in conjunction with a specific modelling or inversion method.In this study, we use an iterative inversion and its results are evaluated using uncertainty analysis and proved to be effective.  相似文献   

20.
According to the chemical and mineral composition characteristics of the fly ash, alumina can be extracted from fly ash through the calcining method by using sodium carbonate and calcium carbonate additives. The effects on leaching rate of alumina have been investigated. The results showed that the fly ash can be activated effectively and the leaching rate of alumina can be improved to more than 92% through this method. The best process parameters were the ratio of raw materials, i.e. the material weight ratio of fly ash, calcium carbonate and sodium carbonate was 1.0:1.2:0.9. The activating temperature was 850℃-900℃, activating time was 3 h. This process has a potential application prospect and improves the value of comprehensive utilization of fly ash.  相似文献   

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