Http://dx.doi.org/10.17014/ijog.vol1no1.20063aA geological research was performed in the Berau Basin, to provide a better understanding on the potential and resources of coalbed methane (CBM) in Berau Regency, East Kalimantan Province, particularly in the Lati Coalfield. Field observation conducted in the coalfield, shows that the banded to bright banded Lati coal is dominated by the bright banded one. Petrographically, the coal consists of vitrinite comprising typical telocollinite and desmocollinite; with rare to sparse exinite, and minor inertinite, and mineral matter. Geochemical analysis shows the range of volatile matter content is from 32.65–39.60%, total sulfur from 0.35–3.04%, ash varies between 2.78–14.50%, and moisture from 12.23...
Geological setting of the Cigudeg and Bojongmanik areas gives rise to the coal characteristics, par-...
Petrographic composition of the Neogene Tenggarong coals in the Kutai Basin-East Kalimantan indicate...
Coal deposits were formed in Tertiary sequexnces in Satui area of Asem-Asem Basin, South Kalimantan....
A geological research was performed in the Berau Basin, to provide a better understanding on the pot...
A geological research was performed in the Berau Basin, to provide a better understanding on the pot...
Increasing world oil prices have a huge impact on national energy needs. Indonesia's economic growth...
Coal has ability to store gas in large quantities, because the surface has ability to adsorb gas. Th...
Abundant coal seams of Miocene age with thickness of up to 4.7 metres occur in Kutai Basin, East Kal...
Muaraenim coalbeds in Rambutan Field have typically high vitrinitic coal geochemical features that i...
Nowadays, conventional energy production has decreased, so it is necessary to develop unconventional...
The location of research is located in the North Muara Tiga Besar Area, East Merapi Sub-District, La...
Administratively, the research is located in the concession area of PT. Berau Coal Site Binungan Blo...
Coal Bed Methane (CBM) is one of unconventional resource that shows great promise forfuture energy n...
Abstract: The coal seams of Sajau Formation in Berau basin, Indonesia are lignite to sub-bituminous ...
The location of research is located in the Tanjung Baru Area, Lahat Regency, South Sumatera. The Geo...
Geological setting of the Cigudeg and Bojongmanik areas gives rise to the coal characteristics, par-...
Petrographic composition of the Neogene Tenggarong coals in the Kutai Basin-East Kalimantan indicate...
Coal deposits were formed in Tertiary sequexnces in Satui area of Asem-Asem Basin, South Kalimantan....
A geological research was performed in the Berau Basin, to provide a better understanding on the pot...
A geological research was performed in the Berau Basin, to provide a better understanding on the pot...
Increasing world oil prices have a huge impact on national energy needs. Indonesia's economic growth...
Coal has ability to store gas in large quantities, because the surface has ability to adsorb gas. Th...
Abundant coal seams of Miocene age with thickness of up to 4.7 metres occur in Kutai Basin, East Kal...
Muaraenim coalbeds in Rambutan Field have typically high vitrinitic coal geochemical features that i...
Nowadays, conventional energy production has decreased, so it is necessary to develop unconventional...
The location of research is located in the North Muara Tiga Besar Area, East Merapi Sub-District, La...
Administratively, the research is located in the concession area of PT. Berau Coal Site Binungan Blo...
Coal Bed Methane (CBM) is one of unconventional resource that shows great promise forfuture energy n...
Abstract: The coal seams of Sajau Formation in Berau basin, Indonesia are lignite to sub-bituminous ...
The location of research is located in the Tanjung Baru Area, Lahat Regency, South Sumatera. The Geo...
Geological setting of the Cigudeg and Bojongmanik areas gives rise to the coal characteristics, par-...
Petrographic composition of the Neogene Tenggarong coals in the Kutai Basin-East Kalimantan indicate...
Coal deposits were formed in Tertiary sequexnces in Satui area of Asem-Asem Basin, South Kalimantan....