SUMMARY: Rock-Eval and pyrolysis GC data show that coals from various origins generate on thermal cracking up to 30070 weight in form of hydrocarbons. Most of them consist of oil-type components (C6 + hydrocarbons) upto about 1.5070 vitrinite rellectance maturity. Therefore fair quantities of oil should be generated during maturation of such samples. Paradoxically, coal-rich sediments contain only minute amounts of oil, whatever their maturity rank. This is interpreted by an easy expulsion of hydrocarbons from coals during burial. Moreover, trapping of oil in the 'microporosity ' of coals, or due to their 'plastic ' behaviour isunlikely. Therefore coals should have a fair potential for oil generation and expulsion and th...
Coal quality indicators Coal is formed from the decomposition products of organic residues of plants...
Abundant oil prone coal (Type III kerogen) deposits are preserved within the high latitude, middle P...
The New Zealand coal covering the complete maturity range from peat to high volatile bituminous, thu...
Although it was for many years believed that coals could not act as source rocks for commercial oil ...
A visual technique has been developed using a diamond anvil cell to characterize oil-prone vs. gas-p...
The oil generation potential of coals in the southern Sydney Basin has been examined using organic p...
Potential of hydrocarbon generation of coals as an oil-generating source has been discussed by sever...
Oil expulsion efficiencies from different lithologies have been investigated and compared employing ...
Hydrous pyrolysis of immature Longyear coal samples was done to assess the source of bitumen found i...
Confined pyrolysis experiments (gold capsules) were performed to determine the yields and kinetic fe...
A unique Upper Permian coal, Leping coal, is widely distributed in South China. The coal samples stu...
The Central Graben in the North Sea is a mature petroleum province with Upper Jurassic – lowermost C...
Some oil and gas wells relate to coals and coaly mudstones have been found in some Jurassic coal-bea...
Coal quality indicators Coal is formed from the decomposition products of organic residues of plants...
The present thesis investigates terrestrial organic matter, i.e. lacustrine shales and coals to furt...
Coal quality indicators Coal is formed from the decomposition products of organic residues of plants...
Abundant oil prone coal (Type III kerogen) deposits are preserved within the high latitude, middle P...
The New Zealand coal covering the complete maturity range from peat to high volatile bituminous, thu...
Although it was for many years believed that coals could not act as source rocks for commercial oil ...
A visual technique has been developed using a diamond anvil cell to characterize oil-prone vs. gas-p...
The oil generation potential of coals in the southern Sydney Basin has been examined using organic p...
Potential of hydrocarbon generation of coals as an oil-generating source has been discussed by sever...
Oil expulsion efficiencies from different lithologies have been investigated and compared employing ...
Hydrous pyrolysis of immature Longyear coal samples was done to assess the source of bitumen found i...
Confined pyrolysis experiments (gold capsules) were performed to determine the yields and kinetic fe...
A unique Upper Permian coal, Leping coal, is widely distributed in South China. The coal samples stu...
The Central Graben in the North Sea is a mature petroleum province with Upper Jurassic – lowermost C...
Some oil and gas wells relate to coals and coaly mudstones have been found in some Jurassic coal-bea...
Coal quality indicators Coal is formed from the decomposition products of organic residues of plants...
The present thesis investigates terrestrial organic matter, i.e. lacustrine shales and coals to furt...
Coal quality indicators Coal is formed from the decomposition products of organic residues of plants...
Abundant oil prone coal (Type III kerogen) deposits are preserved within the high latitude, middle P...
The New Zealand coal covering the complete maturity range from peat to high volatile bituminous, thu...