Genesis of natural hydraulic fractures as an indicator of basin inversion
Satin spar (fibrous gypsum) veins, which occur in evaporite basins worldwide, provide significant insights into host rock deformation and fluid flow, although the genetic mechanism remains obscure. Satin spar veins in the red marls of the Triassic Mercia Mudstone of the Bristol Channel Basin were ch...
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| Format: | Journal article |
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Elsevier
2017
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