Differential dissolution of a Pleistocene reef in the groundwater mixing zone of coastal Yucatan, Mexico
Geology
By: W. Back, B.B. Hanshaw, J.S. Herman, and J. N. Van Driel
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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.
Suggested Citation
Back, W., Hanshaw, B., Herman, J., and Van Driel, J., 1986, Differential dissolution of a Pleistocene reef in the groundwater mixing zone of coastal Yucatan, Mexico: Geology, v. 14, no. 2, p. 137-140, https://doi.org/10.1130/0091-7613(1986)14<137:DDOAPR>2.0.CO;2.
| 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 |
| DOI | 10.1130/0091-7613(1986)14<137:DDOAPR>2.0.CO;2 |
| Volume | 14 |
| Issue | 2 |
| Year Published | 1986 |
| Language | English |
| Publisher | GeoScienceWorld |
| Description | 4 p. |
| First page | 137 |
| Last page | 140 |