About This Item
- Full text of this item is not available.
- Abstract PDFAbstract PDF(no subscription required)
Share This Item
The AAPG/Datapages Combined Publications Database
Houston Geological Society Bulletin
Abstract
Abstract: Plate Tectonics, Organic-Matter Type, and
Basin Evaluation for Petroleum Potential
By
The concepts of plate tectonics have been used to classify
sedimentary basins in terms of physical characteristics, such
as location on the plate and geothermal gradient. A complete classification must
include the amount, type, and distribution of organic matter because this is the
material that generates
petroleum. Organic matter can be divided into that which
grows on the land surface (terrestrial) and that which grows in
water (aquatic). This is an economically important
because aquatic materials produce normal crudes whereas
terrestrially derived materials produce gas and waxy oil. Transport of terrestrial organic
matter to areas of deposition
depends on surface relief because this controls drainage
patterns. The association of transported terrestrial organic
matter with clastic sediments makes deltas the most gas-prone
depositional environment. Organic materials are not
distributed uniformly in deltas because terrestrial organic
matter has its highest concentration nearshore and aquatic
material is produced in large amounts offshore. This separation
and distribution lead to gas fields near paleoshorelines
and oil farther out. As the delta progrades, terrestrial organic
matter is deposited over the previously deposited aquatic
organic matter, producing a vertical sequence from gas to oil
in the delta. Sediments on subducting plates should show the
same vertical sequence of terrestrial over aquatic material
because the slow transport of sediments toward the source of
terrestrial organic matter causes its concentration to increase
as the subduction zone is approached. The opposite trend
(i.e., aquatic over terrestrial) is found on pull-apart margins
where the oldest sediments were formed in a continental rift
rich in terrestrial organic matter and were overlain by
sediments containing increasing amounts of aquatic organic
matter. The distribution of organic-matter types exercises
primary control over the distribution of oil and gas. End_Pages 1 and 2---------------