Dolomite overgrowths suggest a primary origin of cone-in-cone
A long-debated aspect of cone-in-cone structures is whether the mineral aggregates composing the structure precipitated with their conical form (primary cone-in-cone), or whether the cones formed after precipitation (secondary cone-in-cone). A calcite deposit from the Cretaceous of Jordan bears all...
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| Format: | Journal article |
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Cambridge University Press
2016
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