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具有已知深度点的条件下解二度单一密度界面反问题的方法
引用本文:林振民,阳明.具有已知深度点的条件下解二度单一密度界面反问题的方法[J].地球物理学报,1985,28(3):311-321.
作者姓名:林振民  阳明
作者单位:地质矿产部地球物理地球化学勘查研究所
摘    要:本文假定密度界面上有若干点的深度为已知,制订了一种迭代方法。它不要求事先经过区域异常和局部异常的划分,而直接利用布格异常求解。此方法假定了一个基准面,但解的结果不依赖于它。本文还探讨了一种加速收敛的方法,提供了用本迭代法计算的若干理论模型及实际例子。试验表明,本方法可在袖珍计算机上实现。

关 键 词:密度界面  区域异常  深度点  已知点  反演计算  反问题  下解  无限平板  基准面深度  异常曲线  
收稿时间:1983-10-05

A COMPUTER METHOD FOR GRAVITY INTERPRETATIONOF TWO-DIMENSIONAL DENSITY CONTRASTINTERFACE WITH SOME KNOWN DEPTHS
LIN ZHEN-MIN,YANG MING.A COMPUTER METHOD FOR GRAVITY INTERPRETATIONOF TWO-DIMENSIONAL DENSITY CONTRASTINTERFACE WITH SOME KNOWN DEPTHS[J].Chinese Journal of Geophysics,1985,28(3):311-321.
Authors:LIN ZHEN-MIN  YANG MING
Institution:Institute of Geophysical and Geochemical Exploration, Ministry of Geology and Mineral Resources
Abstract:In most of the current methods for gravity interpretation of density contrast interface, a preliminary regional-residual correction is required and the interpretation is carried on with local anomalies; a mean datum plane is assumed and the interface is determined relative to this plane, or a known flat bottom or top is assumed. We suggest a new iteration method, assuming that there are some known depths on the Interface. Thus a preliminary regional-residual correction is not required and interpretation is carried on directly with Bouguer anomalies. Though a datum plane is assumed also, the solution does not depend on it.
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