Subsurface diagenetic evolution and porosity evaluation of Middle-Upper Devonian Kee Scarp reef, Norman Wells, Northwest Territories, Canada.

The Middle-Upper Devonian Kee Scarp Formation at Norman Wells consists of a carbonate platform and an overlying reefal buildup. Episodic increases in the rate of sea-level rise produced multiple cycles of reef growth, with a backstepping character. Reservoir porosity of these reefs is mostly represe...

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Main Author: Azmy, Karem.
Format: Master Thesis
Language:English
Published: University of Windsor 1992
Subjects:
Online Access:https://scholar.uwindsor.ca/etd/3664
https://scholar.uwindsor.ca/cgi/viewcontent.cgi?article=4663&context=etd
id ftunivwindsor:oai:scholar.uwindsor.ca:etd-4663
record_format openpolar
spelling ftunivwindsor:oai:scholar.uwindsor.ca:etd-4663 2023-05-15T17:46:43+02:00 Subsurface diagenetic evolution and porosity evaluation of Middle-Upper Devonian Kee Scarp reef, Norman Wells, Northwest Territories, Canada. Azmy, Karem. 1992-01-01T08:00:00Z application/pdf https://scholar.uwindsor.ca/etd/3664 https://scholar.uwindsor.ca/cgi/viewcontent.cgi?article=4663&context=etd eng eng University of Windsor https://scholar.uwindsor.ca/etd/3664 https://scholar.uwindsor.ca/cgi/viewcontent.cgi?article=4663&context=etd info:eu-repo/semantics/openAccess http://creativecommons.org/licenses/by-nc-nd/4.0/ CC-BY-NC-ND Electronic Theses and Dissertations Geology info:eu-repo/semantics/masterThesis 1992 ftunivwindsor 2022-01-17T12:15:26Z The Middle-Upper Devonian Kee Scarp Formation at Norman Wells consists of a carbonate platform and an overlying reefal buildup. Episodic increases in the rate of sea-level rise produced multiple cycles of reef growth, with a backstepping character. Reservoir porosity of these reefs is mostly represented by micropores of various types developed during diagenesis by the action of aggrading neomorphism and dissolution. The microporosity was developed as intercrystalline microvoids within the present low-magnesium calcite (LMC) stromatoporoid, algal and matrix components. SEM studies show that microporosity development responded to neomorphism at various rates. Reef margins, grain shoals and lower, middle and upper foreslope facies have the highest and best developed microporosity compared to lagoon, reef flat and tidal flat facies. The micropores in Kee Scarp limestone can be classified into four categories based on their shapes: (1) stepwise rhombic, about 1$\mu$m to 2$\mu$m in diameter; mainly developed in stromatoporoids; (2) intercrystalline rhombic, about 1$\mu$m in diameter; mainly in algal aggregates; (3) microvugs, 4$\mu$m to 10 $\mu$m in diameter; mainly in algal aggregates; (4) microchannels, 12$\mu$m length and 0.5$\mu$m width; in algal aggregates and stromatoporoids. (Abstract shortened by UMI.)Dept. of Geology and Geological Engineering. Paper copy at Leddy Library: Theses & Major Papers - Basement, West Bldg. / Call Number: Thesis1992 .A958. Source: Masters Abstracts International, Volume: 31-04, page: 1695. Thesis (M.Sc.)--University of Windsor (Canada), 1992. Master Thesis Northwest Territories University of Windsor, Ontario: Scholarship at UWindsor Canada Kee Scarp ENVELOPE(-126.725,-126.725,65.310,65.310) Leddy ENVELOPE(-117.519,-117.519,56.367,56.367) Norman Wells ENVELOPE(-126.833,-126.833,65.282,65.282) Northwest Territories
institution Open Polar
collection University of Windsor, Ontario: Scholarship at UWindsor
op_collection_id ftunivwindsor
language English
topic Geology
spellingShingle Geology
Azmy, Karem.
Subsurface diagenetic evolution and porosity evaluation of Middle-Upper Devonian Kee Scarp reef, Norman Wells, Northwest Territories, Canada.
topic_facet Geology
description The Middle-Upper Devonian Kee Scarp Formation at Norman Wells consists of a carbonate platform and an overlying reefal buildup. Episodic increases in the rate of sea-level rise produced multiple cycles of reef growth, with a backstepping character. Reservoir porosity of these reefs is mostly represented by micropores of various types developed during diagenesis by the action of aggrading neomorphism and dissolution. The microporosity was developed as intercrystalline microvoids within the present low-magnesium calcite (LMC) stromatoporoid, algal and matrix components. SEM studies show that microporosity development responded to neomorphism at various rates. Reef margins, grain shoals and lower, middle and upper foreslope facies have the highest and best developed microporosity compared to lagoon, reef flat and tidal flat facies. The micropores in Kee Scarp limestone can be classified into four categories based on their shapes: (1) stepwise rhombic, about 1$\mu$m to 2$\mu$m in diameter; mainly developed in stromatoporoids; (2) intercrystalline rhombic, about 1$\mu$m in diameter; mainly in algal aggregates; (3) microvugs, 4$\mu$m to 10 $\mu$m in diameter; mainly in algal aggregates; (4) microchannels, 12$\mu$m length and 0.5$\mu$m width; in algal aggregates and stromatoporoids. (Abstract shortened by UMI.)Dept. of Geology and Geological Engineering. Paper copy at Leddy Library: Theses & Major Papers - Basement, West Bldg. / Call Number: Thesis1992 .A958. Source: Masters Abstracts International, Volume: 31-04, page: 1695. Thesis (M.Sc.)--University of Windsor (Canada), 1992.
format Master Thesis
author Azmy, Karem.
author_facet Azmy, Karem.
author_sort Azmy, Karem.
title Subsurface diagenetic evolution and porosity evaluation of Middle-Upper Devonian Kee Scarp reef, Norman Wells, Northwest Territories, Canada.
title_short Subsurface diagenetic evolution and porosity evaluation of Middle-Upper Devonian Kee Scarp reef, Norman Wells, Northwest Territories, Canada.
title_full Subsurface diagenetic evolution and porosity evaluation of Middle-Upper Devonian Kee Scarp reef, Norman Wells, Northwest Territories, Canada.
title_fullStr Subsurface diagenetic evolution and porosity evaluation of Middle-Upper Devonian Kee Scarp reef, Norman Wells, Northwest Territories, Canada.
title_full_unstemmed Subsurface diagenetic evolution and porosity evaluation of Middle-Upper Devonian Kee Scarp reef, Norman Wells, Northwest Territories, Canada.
title_sort subsurface diagenetic evolution and porosity evaluation of middle-upper devonian kee scarp reef, norman wells, northwest territories, canada.
publisher University of Windsor
publishDate 1992
url https://scholar.uwindsor.ca/etd/3664
https://scholar.uwindsor.ca/cgi/viewcontent.cgi?article=4663&context=etd
long_lat ENVELOPE(-126.725,-126.725,65.310,65.310)
ENVELOPE(-117.519,-117.519,56.367,56.367)
ENVELOPE(-126.833,-126.833,65.282,65.282)
geographic Canada
Kee Scarp
Leddy
Norman Wells
Northwest Territories
geographic_facet Canada
Kee Scarp
Leddy
Norman Wells
Northwest Territories
genre Northwest Territories
genre_facet Northwest Territories
op_source Electronic Theses and Dissertations
op_relation https://scholar.uwindsor.ca/etd/3664
https://scholar.uwindsor.ca/cgi/viewcontent.cgi?article=4663&context=etd
op_rights info:eu-repo/semantics/openAccess
http://creativecommons.org/licenses/by-nc-nd/4.0/
op_rightsnorm CC-BY-NC-ND
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