Print this pageGeochemical Exploration in The Offshore Nile Delta
By
Hany M. Kamel1, Mohmed Sarhan1
(1) Petrobel oil Company, Cairo, Egypt
The major objective of Geochemistry in Exploration phase is to reduce the risk of drilling dry wells by applying geochemical concepts. This paper covers the eastern and central sub-basins in the offshore Nile Delta.
Risk reduction involves selective mapping of quantity, quality and maturity
of petroleum source rocks, identification of the possible 
migration
pathways
from the mature sources to the prospective traps, effectiveness of regional or
local seals and geologic processes, which are controlling all these factors.
Integration of geological studies and geochemical measurements & correlations
help in identifying the charged closures, which exist in the hydrocarbon
migration pathways in the study area.
The Oligocene sequence can be pointed out as the source rock for the most of
the hydrocarbons found in the Nile Delta area. The early Miocene (Qantara
Formation) can be considered as a secondary source rocks. Some Mesozoic
intervals could represent effective sources and co-sources for the hydrocarbons
found towards the north Sinai domain. The migration mainly occurred from the
deepest part of the basin located in the North to Northwest area towards South
to Southeast. Secondary migration along lateral
paths may be quite effective, as
proven along the Abu Madi paleo-valley.