Thermal alteration of organic matter in the contact of a rift-related basaltic dyke: an example from the black limestone, Wadi Matulla, West central Sinai, Egypt
Journal Publication ResearchOnline@JCUAbstract
In the Wadi Matulla area, central Sinai, Egypt, an asymmetric baked zone having an average width of 103 m was formed on both sides of a sub-aerial rift-related Oligocene basaltic dyke cross-cutting organic matter-bearing chalky limestone of the Upper Cretaceous Sudr Formation. Advection was the significant heat transfer mechanism. Very narrow metamorphic and metasomatic zones are developed in the country rock at the immediate contact with the dyke. The change in the thermal maturation of organic matter is reflected in the di�erences in values of the total organic carbon (TOC) within the baked zone. Such di�erences account for the color variation of the snow-white limestone from shades of brown, in the mature to barren samples, to black, in the totally carbonized overmature metamorphic ones. This study presents for the first time the thermal e�ect of mafic dykes on some exposed organic matter-bearing rocks in the Gulf of Suez (GOS) region, and turns attention to the local maturation of source rocks in contact with rift-related intrusives at a relatively greater burial depth in the rift basin.
Journal
Minerals
Publication Name
N/A
Volume
9
ISBN/ISSN
2075-163X
Edition
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Issue
5
Pages Count
26
Location
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Publisher
MDPI AG
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EISSN
N/A
DOI
10.3390/min9050279