Search engine for discovering works of Art, research articles, and books related to Art and Culture
ShareThis
Javascript must be enabled to continue!

SOURCE POTENTIAL OF UPPER TRIASSIC FLUVIO-DELTAIC SYSTEMS OF THE EXMOUTH PLATEAU

View through CrossRef
The fluvio-deltaic rocks of the Upper Triassic Mungaroo Formation of the Exmouth Plateau contain abundant organic material in the form of both coal seams and dispersed fragments. Several thousand metres of these sediments lie within the oil generation window (0.5 to 1.3 per cent R̅O max vitrinite), but they have commonly not been considered as source rocks for oil because the organic matter is of terrestrial origin. Increasing acceptance of plant material as a source for oil warrants an assessment of the oil generating potential of the Mungaroo Formation. The maceral composition of organic matter is dependent on the depositional environment. The large-scale uniformity of environments (mostly lower delta plain) in the Mungaroo Formation leads to a similarity in the organic matter, with an approximate composition of 90 per cent vitrinite in the coals and 50 per cent vitrinite, 20 per cent exinite and 30 per cent inertinite for the dispersed organic matter (DOM). The exception to this is organic material from the alluvial plain environment, where the coal has a vitrinite content of 60 per cent and the dispersed organic matter has a composition of 20 per cent vitrinite, 20 per cent exinite and 60 per cent inertinite. A quantitative assessment of the oil-generating potential of the organic matter based on maceral composition, vitrinite reflectance and volume of coal and dispersed organic matter was made for a range of time-rock units. On this basis, the Carnian-Ladinian and Carnian sequences have the best source potentials. On the basis of vitrinite reflectance measurements, it appears that the Mungaroo Formation has been generating oil since late in the Triassic or early in the Jurassic, through to the Tertiary. Lack of suitable seals during the early generative phase may have permitted some oil to escape. However, significant oil generation has occurred subsequent to the deposition of the younger Mesozoic sequences, when trapping and sealing were more effective.
Title: SOURCE POTENTIAL OF UPPER TRIASSIC FLUVIO-DELTAIC SYSTEMS OF THE EXMOUTH PLATEAU
Description:
The fluvio-deltaic rocks of the Upper Triassic Mungaroo Formation of the Exmouth Plateau contain abundant organic material in the form of both coal seams and dispersed fragments.
Several thousand metres of these sediments lie within the oil generation window (0.
5 to 1.
3 per cent R̅O max vitrinite), but they have commonly not been considered as source rocks for oil because the organic matter is of terrestrial origin.
Increasing acceptance of plant material as a source for oil warrants an assessment of the oil generating potential of the Mungaroo Formation.
The maceral composition of organic matter is dependent on the depositional environment.
The large-scale uniformity of environments (mostly lower delta plain) in the Mungaroo Formation leads to a similarity in the organic matter, with an approximate composition of 90 per cent vitrinite in the coals and 50 per cent vitrinite, 20 per cent exinite and 30 per cent inertinite for the dispersed organic matter (DOM).
The exception to this is organic material from the alluvial plain environment, where the coal has a vitrinite content of 60 per cent and the dispersed organic matter has a composition of 20 per cent vitrinite, 20 per cent exinite and 60 per cent inertinite.
A quantitative assessment of the oil-generating potential of the organic matter based on maceral composition, vitrinite reflectance and volume of coal and dispersed organic matter was made for a range of time-rock units.
On this basis, the Carnian-Ladinian and Carnian sequences have the best source potentials.
On the basis of vitrinite reflectance measurements, it appears that the Mungaroo Formation has been generating oil since late in the Triassic or early in the Jurassic, through to the Tertiary.
Lack of suitable seals during the early generative phase may have permitted some oil to escape.
However, significant oil generation has occurred subsequent to the deposition of the younger Mesozoic sequences, when trapping and sealing were more effective.

Related Results

Organic Geochemical Characteristic Of Crude Oils From Orange Graben, South Sumatra Basin
Organic Geochemical Characteristic Of Crude Oils From Orange Graben, South Sumatra Basin
Lemat Formation in the Orange Graben in the South Sumatra basin has been considered as syn-rift sediments consist of fluvio-lacustrine sediments, create source rock with fluvio-lac...
Proximal Tibial Epiphysiodesis in a Growing Dog
Proximal Tibial Epiphysiodesis in a Growing Dog
 Background: It is believed that the inclined tibial plateau angle to be a major cause of cranial cruciate ligament (CCL) rupture, and the treatment of this disease is the tibial p...
EXPLORATION IN SENSITIVE AREAS: CONVINCING THE COMMUNITY
EXPLORATION IN SENSITIVE AREAS: CONVINCING THE COMMUNITY
Hadson Carnarvon Pty Ltd (Hadson), on behalf of the Joint Venture Partners, operates permits EP342 and TP/9 located at the northern end of Exmouth gulf, to the east of Cape Range p...
Triassic stratigraphy of northern Yukon Territory
Triassic stratigraphy of northern Yukon Territory
This report presents a general outline of the Triassic stratigraphy based on field work carried out on a reconnaissance geologic study of the northern part of Yukon Territory. Tria...
The rise of ginkgoalean plants in the early Mesozoic: a data analysis
The rise of ginkgoalean plants in the early Mesozoic: a data analysis
AbstractIn the present article, ginkgoalean fossil records are analysed and the data are incorporated into a sketched, ‘epoch‐by‐epoch’ framework (e.g. late Triassic, early Jurassi...
Complex evolution and the Triassic Tethyan‐type sedimentation in the Qinling Orogen
Complex evolution and the Triassic Tethyan‐type sedimentation in the Qinling Orogen
The evolution of the Tethys Ocean is a significant geological event in global evolution history. However, although the hinterland of China has Tethyan sedimentary formations, the o...
Global carbon isotope signal in the Middle Triassic on Svalbard
Global carbon isotope signal in the Middle Triassic on Svalbard
<p>Several carbon isotope curves were recently published for the Early and Middle Triassic in Tethys. Recent work has also been done on the Early Triassic of Svalbard...

Back to Top