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THERMAL MATURITY DEVELOPMENT AND SOURCE‐ROCK OCCURRENCE IN THE RED SEA AND GULF OF ADEN
Author(s) -
Barnard P. C.,
Thompson S.,
Bastow M. A.,
Ducreux C.,
Mathurin G.
Publication year - 1992
Publication title -
journal of petroleum geology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 0.725
H-Index - 42
eISSN - 1747-5457
pISSN - 0141-6421
DOI - 10.1111/j.1747-5457.1992.tb00961.x
Subject(s) - geology , source rock , rift , sedimentary rock , maturity (psychological) , structural basin , context (archaeology) , facies , tectonics , geothermal gradient , geochemistry , rift zone , plate tectonics , paleontology , psychology , developmental psychology
Detailed geochemical and geothermal studies have been carried out in the Red Sea and Gulf of Aden in order to understand the regional distribution of source rocks through time, and the effects of changing heat flow through time. These studies have shown the presence of generally thin developments of fair to very good quality source rocks. Most of the identified source rocks occur in syn‐rift sediments throughout the Red Sea area, but pre‐rift source‐rock occurrences have been identified in Yemen (Gulf of Aden). Somalia, and to a lesser extent in Egypt. Isolated occurrences of post‐rift source rocks have also been identified. The data can be interpreted in the regional context of the sedimentary facies of the region in order to predict possible geographic distribution of source rocks. Maturity gradients determined using vitrinite reflectivity and spore coloration range from low (often in post‐rift sections) to high (often in syn‐ and pre‐rift sections). The maturity gradients in many of the sections analysed show intersecting bi‐linear trends, suggesting very high palaeogeothermal gradients in sediments close to the rifting centres. In such areas, the oil and gas “windows” are relatively shallow and thin. In areas where crustal thickening has reduced heat flux. hydrocarbon generation may have occurred in the past, but has since ceased. The models derived during this project for source‐rock distribution and heat‐flow variations are consistent with the tectonic evolution of the basin, and show that there is good potential in parts of the study area for oil generation, accumulation and preservation in pre‐rift, syn‐rift as well as in post‐rift sediments.