• 提出一种新的基于统计推断联合反演方法

    A novel gravity magnetic seismic combination inversion method based on statistical inference was proposed.

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  • 本文采用磁力联合反演方法计算民和盆地基底深度磁化强度

    In this paper, combined gravity and magnetic inversion method of potential field is applied to the calculation of the basement depth and apparent magnetization in the Minghe basin.

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  • 反演基于波动方程走时反演(WT反演)波形反演联合反演方法

    WTW inversion is a hybrid inversion method of wave-equation traveltime inversion (WT) and waveform inversion.

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  • 反演基于波动方程走时反演WT反演波形反演联合反演方法

    Wave function is used to calculate the traveltime and its derivative(perturbation of traveltime with respect to velocity) in WT inversion.

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  • 方法通过引入加权最小平方目标泛函层状介质中的重力地震资料联合反演问题转化成具体优化问题。

    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.

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  • 联合反演优点就是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问题解性。

    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.

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  • 现场实测结果为基础利用数值模拟反演方法分析煤层联合开采底板破坏范围

    Based on the site actual measurements, the inversion analysis on the destroy range of roof and floor by the combined mining of thin seams was made by using numerical modeling.

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  • 方法利用动校正CMPCCP全部建立参数联合反演方程,进而求解出目的层段岩性参数

    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.

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  • 研究了电偶源频率电磁测深单分量电阻率—相位联合反演实施方法,并论述了实际应用效果

    The joint-inversion method of three kinds of one-component apparent resistivity-phase is studied. Morever, the practical applied results are expounded.

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  • 另外采用阻尼最小二乘方法利用全球地震层析成像资料大地水准面异常资料联合反演全球地幔密度异常。

    Moreover, The authors inverted three dimensional global mantle density (anomaly) combining geoid data and seismic tomography data by means of damping least square method.

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  • 介绍利用反射走时联合反演地震界面起伏形态速度横向分布方法。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

    This paper describes a joint inversion method of the topography of seismic interfaces and lateral velocity distribution using travel times of reflections.

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  • 介绍利用反射走时联合反演地震界面起伏形态速度横向分布方法。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

    This paper describes a joint inversion method of the topography of seismic interfaces and lateral velocity distribution using travel times of reflections.

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