The effects of anisotropy of marine magnetic anomalies on the Curie point depth estimates from spectral analysis
Author:
Funder
National Natural Science Foundation of China
Publisher
Springer Science and Business Media LLC
Subject
Geophysics
Link
http://link.springer.com/article/10.1007/s11600-018-0197-z/fulltext.html
Reference47 articles.
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2. Bansal AR, Gabriel G, Dimri VP et al (2011) Estimation of depth to the bottom of magnetic sources by a modified centroid method for fractal distribution of sources: an application to aeromagnetic data in Germany. Geophysics 76(3):L11–L22. https://doi.org/10.1190/1.3560017
3. Bansal AR, Anand SP, Rajaram M et al (2013) Depth to the bottom of magnetic sources (DBMS) from aeromagnetic data of Central India using modified centroid method for fractal distribution of sources. Tectonophysics 603(5):155–161. https://doi.org/10.1016/j.tecto.2013.05.024
4. Bhattacharyya BK, Leu LK (1975) Analysis of magnetic anomalies over Yellowstone National Park: mapping of Curie point isothermal surface for geothermal reconnaissance. J Geophys Res 80(32):4461–4465. https://doi.org/10.1029/JB080i032p04461
5. Blakely RJ (1976) An age-dependent, two-layer model for marine magnetic anomalies. Geophy Pac Ocean Basin Marg. https://doi.org/10.1029/GM019p0227
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