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Differential dissolution of a Pleistocene reef in the groundwater mixing zone of coastal Yucatan, Mexico.

Geology

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, , ,

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Abstract

Mixing of fresh groundwater with subterranean Caribbean seawater generates a highly reactive geochemical zone that enhances aragonite and calcite dissolution and permits neomorphism of aragonite.-from Authors

Additional Publication Details

Publication type:
Article
Publication Subtype:
Journal Article
Title:
Differential dissolution of a Pleistocene reef in the groundwater mixing zone of coastal Yucatan, Mexico.
Series title:
Geology
Volume
14
Issue:
2
Year Published:
1986
Language:
English
Larger Work Type:
Article
Larger Work Subtype:
Journal Article
Larger Work Title:
Geology
First page:
137
Last page:
140
Number of Pages:
4