Impact of facies and diagenetic variability on permeability and fluid flow in an oolitic grainstone—Pleistocene Miami Oolite-Reference-Cited by-同舟云学术

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Impact of facies and diagenetic variability on permeability and fluid flow in an oolitic grainstone—Pleistocene Miami Oolite

Published:2020-02-10 Issue:2 Volume:6 Page:459-470
ISSN:2055-4877
Container-title:The Depositional Record
language:en
Short-container-title:Depositional Rec

Author:

Harris Paul (Mitch)¹^ORCID,Purkis Sam¹

Affiliation:

1. CSL – Center for Carbonate Research Department of Marine Geosciences University of Miami Miami FL USA

Publisher

Wiley

Subject

Paleontology,Stratigraphy,Geology,Environmental Science (miscellaneous),Oceanography

Link

https://onlinelibrary.wiley.com/doi/pdf/10.1002/dep2.104

Reference65 articles.

1. Matrix permeability of the confined Floridan Aquifer;Budd D.A.;Hydrology Journal,2004

2. The caves of Dade County, Florida;Cressler A.;Georgia Underground,1993

3. Co‐existence of skeletal and ooid shoals as a result of antecedent topography—Cat cay shoal complex, Bahamas

4. Application of ground-penetrating radar, digital optical borehole images, and cores for characterization of porosity hydraulic conductivity and paleokarst in the Biscayne aquifer, southeastern Florida, USA

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