HYDROCARDO S IN COAL DEPOSITS FROM LO G TUTOR, BARAM AND MERIT PILLA. KAPIT OF SARAWAK ABSTRACT The coal samples obtained from Long Tutoh coalfield, Baram and Merit Pilla coalfield, Kapit, Sarawak were studied to determine their hydrocarbon composition. The objectives of this study are (1) to characterize the organic components in two Sarawakian coal samples, (2) to predict the source of organic matters and (3) to evaluate maturity degree of coal samples through biomarker evaluation. The geolipid from the coal sample was extracted using Soxhlet extractor and subsequently being separated into aliphatic fraction and polyaromatic fraction on activated silica gel chromatography. The analysis of organic components In the coal samples were per...
The distribution of hopanoids and alkanes in bitumen extracts of coals, coaly shales, and shales fro...
Organic geochemical studies on brown coal (lignite) located in Inul area were carried out, an area t...
The purpose of this study was to reconstruct the depositional environment, the genesis and the compo...
The coal samples obtained from Long Tutoh coalfield, Baram and Merit Pilla coalfield, Kapit, Sarawak...
Coal samples Merit pilla, Sungai Mas and Mukah-Balingian were studied qualitatively and quantitativ...
Characteristic of organic geochemistry (biomarker) gives information about environment of coal. Coal...
Potential of hydrocarbon generation of coals as an oil-generating source has been discussed by sever...
The Tertiary Tanjong Formation coals exposed in the west middle block of the Pinangah Coalfield, cen...
AbstractMuaraWahau coal belongs to Wahau Formation which was deposited during Early Miocene in terre...
DOI: 10.17014/ijog.5.2.107-116The Middle to Late Miocene brown coal extracted from Inul area, Sangat...
Balingan and Mukah coals were investigated for their organic geochemical contents. The coal samples...
Tertiary coal from Merit-Pila coalfield, Central Sarawak, Malaysia were analysed their regional ran...
Coal from the Cenozoic period takes a large proportion of world coal reservoirs. The information on ...
Ten coal seams in Upper Shihezi Formation, Lower Shihezi Formation, and Shanxi Formation from the Zh...
Pyrolysis-gas chromatography-mass spectrometry (Py-GC–MS) and thermally assisted hydrolysis and meth...
The distribution of hopanoids and alkanes in bitumen extracts of coals, coaly shales, and shales fro...
Organic geochemical studies on brown coal (lignite) located in Inul area were carried out, an area t...
The purpose of this study was to reconstruct the depositional environment, the genesis and the compo...
The coal samples obtained from Long Tutoh coalfield, Baram and Merit Pilla coalfield, Kapit, Sarawak...
Coal samples Merit pilla, Sungai Mas and Mukah-Balingian were studied qualitatively and quantitativ...
Characteristic of organic geochemistry (biomarker) gives information about environment of coal. Coal...
Potential of hydrocarbon generation of coals as an oil-generating source has been discussed by sever...
The Tertiary Tanjong Formation coals exposed in the west middle block of the Pinangah Coalfield, cen...
AbstractMuaraWahau coal belongs to Wahau Formation which was deposited during Early Miocene in terre...
DOI: 10.17014/ijog.5.2.107-116The Middle to Late Miocene brown coal extracted from Inul area, Sangat...
Balingan and Mukah coals were investigated for their organic geochemical contents. The coal samples...
Tertiary coal from Merit-Pila coalfield, Central Sarawak, Malaysia were analysed their regional ran...
Coal from the Cenozoic period takes a large proportion of world coal reservoirs. The information on ...
Ten coal seams in Upper Shihezi Formation, Lower Shihezi Formation, and Shanxi Formation from the Zh...
Pyrolysis-gas chromatography-mass spectrometry (Py-GC–MS) and thermally assisted hydrolysis and meth...
The distribution of hopanoids and alkanes in bitumen extracts of coals, coaly shales, and shales fro...
Organic geochemical studies on brown coal (lignite) located in Inul area were carried out, an area t...
The purpose of this study was to reconstruct the depositional environment, the genesis and the compo...