Ibtehal Abdel Rahman: Early diagenetic features of the scleractinians, pleistocene coral reef, Dahab (Sinai, Egypt). In: Acta mineralogica-petrographica, (40). pp. 161-174. (1999)
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Abstract
Two kms north-east of Dahab, the northernmost remnant of emerged Pleistocene terraces display well preserved coral-reef and associated peri-reefal facies. The Scleractinian corals within the reef sequence display a series of diagenetic features formed by the alteration of the original micro-structures under different diagenetic conditions. Evidence from cement fabrics (aragonite and high-Mg calcite) suggests that the cementation took place exclusively in a phreatic marine environment. Meteoric diagenesis is indicated by traces of minor leaching and sparry calcite cement. Formation of microcrystalline dolomite and halite might take place in a sabkha environment. This suggests under various diagenetic alternation conditions.
Item Type: | Article |
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Journal or Publication Title: | Acta mineralogica-petrographica |
Date: | 1999 |
Volume: | 40 |
ISSN: | 0365-8066 |
Page Range: | pp. 161-174 |
Language: | English |
Publisher: | University of Szeged, Department of Mineralogy, Geochemistry and Petrology |
Place of Publication: | Szeged |
Related URLs: | http://acta.bibl.u-szeged.hu/39419/ |
Uncontrolled Keywords: | Kőzettan, Ásványtan, Földtan |
Additional Information: | Bibliogr.: p. 173-174. ; ill. ; összefoglalás angol nyelven |
Subjects: | 01. Natural sciences 01. Natural sciences > 01.05. Earth and related environmental sciences |
Date Deposited: | 2016. Oct. 17. 09:25 |
Last Modified: | 2022. Jul. 27. 14:53 |
URI: | http://acta.bibl.u-szeged.hu/id/eprint/24886 |
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