Abstract
When salt is buried under heavier rocks, it rises buoyantly in vast sheets and fingers; it may even fountain aboveground and flow like a glacier. Laboratory models reveal the patterns of salt upwelling.
Cite
CITATION STYLE
APA
Talbot, C. J., & Jackson, M. P. A. (1987). SALT TECTONICS. Scientific American, 257(2), 70–79. https://doi.org/10.1038/scientificamerican0887-70
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