GEOLOGIC ASPECTS CONTROLLING MACERAL AND MINERAL MATTER CONTENT OF SATUI COALS- SOUTH KALIMANTAN
| Main Author: | SANTOSO, BINARKO; R & D Centre for Mineral and Coal Technology |
|---|---|
| Format: | Article info application/pdf eJournal |
| Bahasa: | eng |
| Terbitan: |
Puslitbang tekMIRA
, 2017
|
| Subjects: | |
| Online Access: |
http://jurnal.tekmira.esdm.go.id/index.php/imj/article/view/494 http://jurnal.tekmira.esdm.go.id/index.php/imj/article/view/494/358 |
| ctrlnum |
article-494 |
|---|---|
| fullrecord |
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<dc schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd"><title lang="en-US">GEOLOGIC ASPECTS CONTROLLING MACERAL AND MINERAL MATTER CONTENT OF SATUI COALS- SOUTH KALIMANTAN</title><creator>SANTOSO, BINARKO; R & D Centre for Mineral and Coal Technology</creator><subject lang="en-US">maceral, mineral matter, coal, geologic aspects</subject><subject lang="en-US"/><description lang="en-US">Coal deposits were formed in Tertiary sequexnces in Satui area of Asem-Asem Basin, South Kalimantan. The coals were deposited in paralic to neritic environments. Lithotype of Satui coals is dominated by bright- banded and banded. Petrographically, vitrinite and liptinite are the dominant macerals in the Eocene coals. Inertinite is a minor component. Mineral content is relatively high in most of the coals. There is a significant relationship between lithotype and petrographic observations; the brighter coal is in association with the vitrinite-rich coal. The differences in the coal type are due to the interaction of geologic factors. There is a good correlation among lithotype, petrographic composition and geologic aspects that clearly influence the characteristics of the coals. The ranks of the Eocene coals ranging from brown coal to high volatile bitumi- nous indicate a normal regional coalification.</description><publisher lang="en-US">Puslitbang tekMIRA</publisher><contributor lang="en-US"/><date>2017-11-18</date><type>Journal:Article</type><type>Other:info:eu-repo/semantics/publishedVersion</type><type>Other:</type><type>Other:</type><type>File:application/pdf</type><identifier>http://jurnal.tekmira.esdm.go.id/index.php/imj/article/view/494</identifier><source lang="en-US">Indonesian Mining Journal; Vol 14, No 2 (2011): INDONESIAN MINING JOURNAL Vol. 14 No. 2 June 2011; 63 - 73</source><source lang="id-ID">Indonesian Mining Journal; Vol 14, No 2 (2011): INDONESIAN MINING JOURNAL Vol. 14 No. 2 June 2011; 63 - 73</source><source>2527-8797</source><source>0854-9931</source><language>eng</language><relation>http://jurnal.tekmira.esdm.go.id/index.php/imj/article/view/494/358</relation><rights lang="en-US">Copyright (c) 2017 Indonesian Mining Journal</rights><rights lang="en-US">http://creativecommons.org/licenses/by-nc/4.0</rights><recordID>article-494</recordID></dc>
|
| language |
eng |
| format |
Journal:Article Journal Other:info:eu-repo/semantics/publishedVersion Other Other: File:application/pdf File Journal:eJournal |
| author |
SANTOSO, BINARKO; R & D Centre for Mineral and Coal Technology |
| title |
GEOLOGIC ASPECTS CONTROLLING MACERAL AND MINERAL MATTER CONTENT OF SATUI COALS- SOUTH KALIMANTAN |
| publisher |
Puslitbang tekMIRA |
| publishDate |
2017 |
| topic |
maceral mineral matter coal geologic aspects |
| url |
http://jurnal.tekmira.esdm.go.id/index.php/imj/article/view/494 http://jurnal.tekmira.esdm.go.id/index.php/imj/article/view/494/358 |
| contents |
Coal deposits were formed in Tertiary sequexnces in Satui area of Asem-Asem Basin, South Kalimantan. The coals were deposited in paralic to neritic environments. Lithotype of Satui coals is dominated by bright- banded and banded. Petrographically, vitrinite and liptinite are the dominant macerals in the Eocene coals. Inertinite is a minor component. Mineral content is relatively high in most of the coals. There is a significant relationship between lithotype and petrographic observations; the brighter coal is in association with the vitrinite-rich coal. The differences in the coal type are due to the interaction of geologic factors. There is a good correlation among lithotype, petrographic composition and geologic aspects that clearly influence the characteristics of the coals. The ranks of the Eocene coals ranging from brown coal to high volatile bitumi- nous indicate a normal regional coalification. |
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IOS4265.article-494 |
| institution |
Kementerian Energi dan Sumber Daya Mineral |
| institution_id |
105 |
| institution_type |
library:special library |
| library |
Pusat Penelitian dan Pengembangan Teknologi Mineral dan Batubara |
| library_id |
974 |
| collection |
Indonesian Mining Journal |
| repository_id |
4265 |
| subject_area |
Mining and Related Operations/Teknik Tambang dan Teknik Pertambangan Minerals of Indonesia/Mineral di Indonesia Chemistry and Allied Science/Kimia dan Ilmu yang Berhubungan Metallurgy/Metal, Metalurgi |
| city |
BANDUNG |
| province |
JAWA BARAT |
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1 |
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IOS4265 |
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2017-12-01T01:44:19Z |
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2017-12-01T01:44:19Z |
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1686103520576536577 |
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17.538404 |