Type and rank variation of selected Sumateran (Ombilin and Bukit Asam) Tertiary coals were as- sessed by petrographic examination of 170 samples. The coals are dominated by vitrinite, common liptinite and rare inertinite and mineral matter. Vitrinite macerals are dominated by detrovitrinite and telovitrinite. Resinite, cutinite and suberinite are the dominant liptinite macerals in the coals. Inertinite macerals in the coals consist of semifusinite, sclerotinite and inertodetrinite. The higher vitrinite re- flectance of some coals is a result of the local and variable effects of igneous intrusions in both areas. Similarities in the type and rank characteristics in the coals reflect their geological setting, climatic influence and peat condit...
Coal deposits were formed in Tertiary sequexnces in Satui area of Asem-Asem Basin, South Kalimantan....
Abundant coal seams of Miocene age with thickness of up to 4.7 metres occur in Kutai Basin, East Kal...
Coal seams D and E belong to the Muara Enim Formation in South Sumatra Basin, which includes to the ...
Type and rank variation of selected Sumateran (Ombilin and Bukit Asam) Tertiary coals were as- sesse...
Selected Tertiary coals from the western part of Indonesia (Sumatera, Kalimantan and Java) indicate ...
Type and rank variation within Tertiary Barito coals of Tanjung Formation were analyzed by petro- gr...
Similarities and differences in rank characteristics in the Bukit Asam coals within the South Sumate...
Rank and type variations of the Ombilin coals were studied by petrographic examination of thirty-six...
Petrographic composition of the Neogene Tenggarong coals in the Kutai Basin-East Kalimantan indicate...
Similarities and differences in type and rank characteristics in Tertiary coals of the western part ...
Genesis of the coal macerals in the studied area depends particularly on the tectonic and geologic s...
Two coalfields have been contrasted and compared on the basis of qualitative and quantitative stud- ...
Type and rank variations of Lebak coals were derived from twenty-eight samples of Palaeogene coalfie...
Geological setting of the Cigudeg and Bojongmanik areas gives rise to the coal characteristics, par-...
Tertiary coals of Nagaland are found within the Barail group of rocks belonging to Oligocene age and...
Coal deposits were formed in Tertiary sequexnces in Satui area of Asem-Asem Basin, South Kalimantan....
Abundant coal seams of Miocene age with thickness of up to 4.7 metres occur in Kutai Basin, East Kal...
Coal seams D and E belong to the Muara Enim Formation in South Sumatra Basin, which includes to the ...
Type and rank variation of selected Sumateran (Ombilin and Bukit Asam) Tertiary coals were as- sesse...
Selected Tertiary coals from the western part of Indonesia (Sumatera, Kalimantan and Java) indicate ...
Type and rank variation within Tertiary Barito coals of Tanjung Formation were analyzed by petro- gr...
Similarities and differences in rank characteristics in the Bukit Asam coals within the South Sumate...
Rank and type variations of the Ombilin coals were studied by petrographic examination of thirty-six...
Petrographic composition of the Neogene Tenggarong coals in the Kutai Basin-East Kalimantan indicate...
Similarities and differences in type and rank characteristics in Tertiary coals of the western part ...
Genesis of the coal macerals in the studied area depends particularly on the tectonic and geologic s...
Two coalfields have been contrasted and compared on the basis of qualitative and quantitative stud- ...
Type and rank variations of Lebak coals were derived from twenty-eight samples of Palaeogene coalfie...
Geological setting of the Cigudeg and Bojongmanik areas gives rise to the coal characteristics, par-...
Tertiary coals of Nagaland are found within the Barail group of rocks belonging to Oligocene age and...
Coal deposits were formed in Tertiary sequexnces in Satui area of Asem-Asem Basin, South Kalimantan....
Abundant coal seams of Miocene age with thickness of up to 4.7 metres occur in Kutai Basin, East Kal...
Coal seams D and E belong to the Muara Enim Formation in South Sumatra Basin, which includes to the ...