Analytical method of interpreting magnetic anomalies of a horizontal plate at inclined magnetization
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Abstract
Anomalies characteristic of the horizontal plate are most often observed in platform regions. Their sources are usually relatively low thicknesses of terrigenous (sometimes volcanogenic) rocks, the distribution of which in the plan is limited by discontinuities or zones of sharp facies transitions ...
Область исследования:
(Archived) Without section
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None
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