The Miocene Sangatta coals indicate similarities and differences in type and rank characteristics. The phenomena express the geological setting that includes the stratigraphic aspect and the pres- ence of intrusive body. The stratigraphic aspect relates to geologic age and cover thickness; the lower coal seam having a thicker cover has a higher rank than the upper coal seam. The intrusive body changes the rank of the coal up to semi-anthracite. The coals that are not affected by the intrusion have rank of brown coal to subbituminous. The rank of the coals increases from east to west toward the Meratus Range due to the cover thickness, where the western part has a thicker cover than the eastern part. These geological phenomena could be an ex...
The Palaeogene coal deposits occur in three coalfields in the Banten Province, which are distributed...
Geologic aspects, particularly geologic history and depositional environment, have a main role in th...
Coal seams D and E belong to the Muara Enim Formation in South Sumatra Basin, which includes to the ...
The Miocene Sangatta coals indicate similarities and differences in type and rank characteristics. T...
The Asem-Asem Basin has cratonic and back-arc settings containing coal deposits that were formed in ...
Coal deposits were formed in Tertiary sequexnces in Satui area of Asem-Asem Basin, South Kalimantan....
Selected Tertiary coals from the western part of Indonesia (Sumatera, Kalimantan and Java) indicate ...
Geological setting of the Cigudeg and Bojongmanik areas gives rise to the coal characteristics, par-...
Eastern Kalimantan has the second largest coal resources in Indonesia after Bukit Asam and Ombilin C...
A carbonate complex in the Mangkalihat area, East Kalimantan, has been selected for this study, beca...
Petrographic composition of the Neogene Tenggarong coals in the Kutai Basin-East Kalimantan indicate...
Eight samples of Eocene Kuaro Formation were taken from Pasir area, East Kalimantan to be examined t...
Type and rank variation of selected Sumateran (Ombilin and Bukit Asam) Tertiary coals were as- sesse...
Abundant coal seams of Miocene age with thickness of up to 4.7 metres occur in Kutai Basin, East Kal...
The South Palembang Sub-basin, in the southern part of the South Sumatra Basin, is an important area...
The Palaeogene coal deposits occur in three coalfields in the Banten Province, which are distributed...
Geologic aspects, particularly geologic history and depositional environment, have a main role in th...
Coal seams D and E belong to the Muara Enim Formation in South Sumatra Basin, which includes to the ...
The Miocene Sangatta coals indicate similarities and differences in type and rank characteristics. T...
The Asem-Asem Basin has cratonic and back-arc settings containing coal deposits that were formed in ...
Coal deposits were formed in Tertiary sequexnces in Satui area of Asem-Asem Basin, South Kalimantan....
Selected Tertiary coals from the western part of Indonesia (Sumatera, Kalimantan and Java) indicate ...
Geological setting of the Cigudeg and Bojongmanik areas gives rise to the coal characteristics, par-...
Eastern Kalimantan has the second largest coal resources in Indonesia after Bukit Asam and Ombilin C...
A carbonate complex in the Mangkalihat area, East Kalimantan, has been selected for this study, beca...
Petrographic composition of the Neogene Tenggarong coals in the Kutai Basin-East Kalimantan indicate...
Eight samples of Eocene Kuaro Formation were taken from Pasir area, East Kalimantan to be examined t...
Type and rank variation of selected Sumateran (Ombilin and Bukit Asam) Tertiary coals were as- sesse...
Abundant coal seams of Miocene age with thickness of up to 4.7 metres occur in Kutai Basin, East Kal...
The South Palembang Sub-basin, in the southern part of the South Sumatra Basin, is an important area...
The Palaeogene coal deposits occur in three coalfields in the Banten Province, which are distributed...
Geologic aspects, particularly geologic history and depositional environment, have a main role in th...
Coal seams D and E belong to the Muara Enim Formation in South Sumatra Basin, which includes to the ...