最大熵功率谱计算磁源深度方法应用初探

全文: PDF(699 KB)
输出: BibTeX | EndNote (RIS)

摘要

本文介绍了应用最大熵功率谱计算磁源深度的方法原理、理论模型试算结果及在方法应用方面的改进措施,肯定了利用磁场水平导数的最大熵功率谱计算深度的效果。

	服务

	把本文推荐给朋友
	加入引用管理器
	E-mail Alert
	RSS
	作者相关文章

Abstract：

This paper deals with the method for calculating the depth of magnetic body by applying maximum entropy power spectrum and describes its basic principle, tentative calculation on theoretical model and the measures for im provement of its application. The calculation of the depth according to maxi mum power spectrum of horizontal derivative of the magnetic field is proved to be effective.

出版日期: 1989-02-24

引用本文:

张培琴, 朱兆芳. 最大熵功率谱计算磁源深度方法应用初探[J]. 物探与化探, 1989, 13(1): 44-52.
Zhang Peiqin, Zhu Zhaofang. THE METHOD FOR CALCULATING THE DEPTH OFMAGNETIC BODY ON THE BASIS OF MAXIMUM ENTROPYPOWER SPECTRUM AND ITS APPLCATION. Geophysical and Geochemical Exploration, 1989, 13(1): 44-52.

链接本文:

https://www.wutanyuhuatan.com/CN/ 或 https://www.wutanyuhuatan.com/CN/Y1989/V13/I1/44

［1］张培琴:最大摘谱分析法及其在物探中的应用,物化探汁算技术,Vol. 9, No. 9, 1987.
［2］侯重初、施志群:利用位场转换解释异常,物化探电子计算技术,1982年,第1期,总13期。
［3］熊光楚:磁铁矿床上磁异常的解释推断,中国工业出版社,1961.
［4］侯重初、李保国:直接计算磁性下界面深度的功率谱法,物化探计算技术,Vol. 7, No. 3, 1985.
［5］ Blahely R. J.and Hassanzadch S. Estimation of depth to magnetic Source using maximum entrory rower spectra, with application to the Peru-Chile trench, Geo. soc. of America Memoir, 154,1981.
［6］ Blakely R. and cox A. Identification of short polarity events by transfomring marine magnetic rrofilcs to the Pole,Journal of Geophysical Research, Vol. 77, No. 23, 1972.