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Research area consist of two geomorphology units, there are Wing of Fold Hills Unit and Alluvial Plain Unit. Stratigraphy unit consist of five units. First is Sandstone Unit that was deposited and also Limestone Unit 1 with a relationship between Limestone and Sandstone Unit is fingering, followed b...
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id-itb.:136682017-09-27T11:46:45Z#TITLE_ALTERNATIVE# (NIM 12007011), MUHAJIR Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13668 Research area consist of two geomorphology units, there are Wing of Fold Hills Unit and Alluvial Plain Unit. Stratigraphy unit consist of five units. First is Sandstone Unit that was deposited and also Limestone Unit 1 with a relationship between Limestone and Sandstone Unit is fingering, followed by Sandstone-Mudstone Unit that deposited underlying the Sandstone Unit and also deposited Limestone Unit 2 with the relationship between of them is fingering. Entire unit was deposited in Miocene and out of the tune Alluvial Plain Unit deposited in Resen. Main force formed the geological structure such us fold, that located on the northwest outside the research area and strike slip fault during the Pliocene and Pleistocene. The erosion and mining roads formed the landscape of the research area like case today. In a preliminary survey of this coal area, the authors found no potential coal outcrop to mine. The thickness of coal seams in this study area ranges from ±40-50 cm with class of this coal is lignite. Because of this background, the proximate analysis and more detailed analysis of dispersion coal in this research area. text |
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Research area consist of two geomorphology units, there are Wing of Fold Hills Unit and Alluvial Plain Unit. Stratigraphy unit consist of five units. First is Sandstone Unit that was deposited and also Limestone Unit 1 with a relationship between Limestone and Sandstone Unit is fingering, followed by Sandstone-Mudstone Unit that deposited underlying the Sandstone Unit and also deposited Limestone Unit 2 with the relationship between of them is fingering. Entire unit was deposited in Miocene and out of the tune Alluvial Plain Unit deposited in Resen. Main force formed the geological structure such us fold, that located on the northwest outside the research area and strike slip fault during the Pliocene and Pleistocene. The erosion and mining roads formed the landscape of the research area like case today. In a preliminary survey of this coal area, the authors found no potential coal outcrop to mine. The thickness of coal seams in this study area ranges from ±40-50 cm with class of this coal is lignite. Because of this background, the proximate analysis and more detailed analysis of dispersion coal in this research area. |
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