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Cited by 425

The DOI matches its Crossref record; 9 of the 9 references it cites were found in a registry or an index.

Dolomitization by Seepage Refluxion

John Emery Adams (2), Mary Louise R·1960·AAPG Bulletin

Abstract

ABSTRACT Bedded dolomites in the Permian Basin were formed by the alteration of metastable limestones by hypersaline brines refluxing from evaporite lagoons. The hot, heavy, highly alkaline, carbon dioxide-free, magnesium-supercharged brines displaced connate waters to provide both a chemically favorable environment for magnesium-calcium exchange and a vehicle for removing displaced calcium. Fossil lagoonal brines and fillings of halite and anhydrite in the dolomite pores offer proof of the brine invasion. Sedimentary dolomites in other areas are commonly associated with evaporites, and for these dolomites a similar origin is postulated.

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Crossref · 10.1306/0bda6263-16bd-11d7-8645000102c1865d

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Metadata

Authors
John Emery Adams (2), M. L. R.
Venue
AAPG Bulletin
Published
1960
Volume
44
Issue
12
Pages
1912-1920
ISSN
0149-1423 (ISSN-L)
OpenAlex
W1998984266
Cited by
425
References
9
FWCI
6.41
Type
journal article
Language
en
Open access
closed

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CoChat. (2026). Citation check: Dolomitization by Seepage Refluxion. https://app.cochat.ai/papers/10.1306/0bda6263-16bd-11d7-8645000102c1865d
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John Emery Adams (2), M. L. R. (1960). Dolomitization by Seepage Refluxion. AAPG Bulletin. https://doi.org/10.1306/0bda6263-16bd-11d7-8645000102c1865d

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Bibliographic data: Semantic Scholar, OpenAlex, Crossref.

Contains information from the Semantic Scholar Academic Graph Datasets, made available under the ODC Attribution License (ODC-BY 1.0).

Semantic Scholar’s data is described in: Kinney, R., et al. (2023). The Semantic Scholar Open Data Platform. arXiv:2301.10140.