Digital computation of gravitational and magnetic anomalies and their derivatives for two-dimensional bodies of arbitrary shape-Reference-Cited by-同舟云学术

Digital computation of gravitational and magnetic anomalies and their derivatives for two-dimensional bodies of arbitrary shape

Published:1966 Issue:1 Volume:64 Page:14-18
ISSN:0033-4553
Container-title:Pure and Applied Geophysics PAGEOPH
language:en
Short-container-title:PAGEOPH

Author:

Vallabh Sharma P.

Publisher

Springer Science and Business Media LLC

Subject

Geochemistry and Petrology,Geophysics

Link

http://link.springer.com/content/pdf/10.1007/BF00875526.pdf

Reference4 articles.

1. F. Gassmann,Graphical evaluation of the anomalies of gravity and of the magnetic field, caused by three-dimensional bodies, Proc. Third World Petrol. Congress, Sec.,1 (1951), 613.

2. N. A. Morgan andF. S. Grant,High speed calculation of gravity and magnetic profiles across two-dimensional bodies having an arbitrary cross-section, Geophysical Prospecting11 (1963), 10.

3. M. Talwani, J. L. Worzel andM. Landisman,Rapid gravity computations for two-dimensional bodies with application to the Mendocino submarine fracture zone. J. Geophys. Res.64 (1959), 49.

4. M. Talwani andJ. R. Heirtzler,Computation of magnetic anomalies caused by two-dimensional structures of arbitrary shape: Computers in the mineral industries, Part 1, Stanford Univ. Publ., Geol. Sciences9 (1964), 464.

Cited by 4 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Tectonic Development of the Bismarck Sea Based on Gravity and Magnetic Modelling;Geophysical Journal International;1976-07-01

2. A structural interpretation of magnetometer and seismic profiler records in the Bismarck Sea, Melanesian Archipelago;Journal of the Geological Society of Australia;1974-12

3. Solution of the direct problem in gravimetry by means of the Monte Carlo method;Geoexploration;1968-12

4. High speed gravity and magnetic calculations of uniform cylindrical bodies of arbitrary cross-section and finite length;Pure and Applied Geophysics PAGEOPH;1966