The well-logging signal pretreatment is the first requirement for the sake of a better joint inversion of seismic and well-logging data.
为了更好地进行地震测井联合反演，必须首先对测井信号进行预处理，而在此过程中测井信号去噪和测井低频信息提取是非常重要的。
If simultaneously combined with equivalent models and the rapid procedure of ray tracing, the practicability of joint inversion can yet be improved.
如果结合等价模型和快速射线追踪过程的利用，可大大提高联合反演的实用性。
This paper describes a joint inversion method of the topography of seismic interfaces and lateral velocity distribution using travel times of reflections.
介绍了利用反射走时联合反演地震界面起伏形态和速度横向分布的方法。正问题采用了一种简单而有效的二维介质中两点射线追踪方法。
And at the development stage, well log-seismic joint inversion is necessary for detailed reservoir description and identification of thinner layers of interest.
测井与地震联合反演主要用于开发阶段，其结果能分辨薄层目标，适合于精细油藏描述。
Along the profile a joint inversion of gravity with geomagnetism has been carried out and 2-d density structure and 2-d geomagnetic structure have been obtained.
沿剖面完成了重磁联合反演，获得了岩石圈二维密度结构与二维磁性结构。
The joint inversion has better resolution and can more effectively resolve the problem of non-uniqueness than the inversion using only one geophysical method data.
联合反演的优点就是比单一地球物理反演方法具有更高的分辨率，并且在一定程度上抑制了问题的多解性。
The method utilizes all the CMP and CCP angle gathers after NMO to build multi-wave & multi-parameter joint inversion equation and calculate the lithologic parameters of interval.
该方法利用动校正后的CMP及CCP全部角道集，建立多波多参数联合反演方程，进而求解出目的层段的岩性参数。
According to the theory of generalized inversion, we can get the parameters of velocity and thickness in each layer with joint inversion of multilayer reflection wave's travel time.
从广义反演理论出发，对多层反射波的走时联合反演，可以同时获得所有的各层速度及厚度参数。
The joint inversion problem of gravimetric and seismic data in layered medium can be converted into an optimization problem by introducing a weighted least square objective functional.
该方法通过引入加权最小平方目标泛函，将层状介质中的重力、地震资料联合反演问题转化成具体的优化问题。
Joint inversion using different kinds of geophysical data is the important quantitative interpretation tools for integrated geophysics.
因此利用各种地球物理数据的联合反演，是综合地球物理研究的重要定量解释手段。
The joint-inversion method of three kinds of one-component apparent resistivity-phase is studied. Morever, the practical applied results are expounded.
研究了电偶源频率电磁测深中三种单分量视电阻率—相位联合反演的实施方法，并论述了其实际应用效果。
The joint-inversion method of three kinds of one-component apparent resistivity-phase is studied. Morever, the practical applied results are expounded.
研究了电偶源频率电磁测深中三种单分量视电阻率—相位联合反演的实施方法，并论述了其实际应用效果。
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