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Stratigraphy of study area consists of three litostratigraphic units, those units are Sandstone Unit of Bayah Formation, Mudstone Unit of Batuasih Formation, and Limestone Unit of Rajamandala Formation. There are ten litofacies in study area, those are, conglomeratic sandstone (Sg), cross bedded san...
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| Online Access: | https://digilib.itb.ac.id/gdl/view/13587 |
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| Institution: | Institut Teknologi Bandung |
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id-itb.:135872017-09-27T11:46:45Z#TITLE_ALTERNATIVE# JULI ANDIKA CHANDRA (NIM 12005011), JUAN Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13587 Stratigraphy of study area consists of three litostratigraphic units, those units are Sandstone Unit of Bayah Formation, Mudstone Unit of Batuasih Formation, and Limestone Unit of Rajamandala Formation. There are ten litofacies in study area, those are, conglomeratic sandstone (Sg), cross bedded sandstone (Sp), bioturbated sandstone (Sb), carbonaceous sandstone (Sc), parallel laminated sandstone (Sh), flaser bedded sandstone Sf), wavy bedded sandstone (Sw), lenticular bedded sandstone (Fl), laminated sandstone (Fsc), and bioclastic limestone (Lk). Result of this study shows that Sandstone Unit and Mudstone Unit in this area have deposited in transition environment that have tidal influence, vertical succession is shallowing upward. Sandstone Unit was deposited in tidal sand flat – mixed tidal sand-mud flat that characterized by flaser and wavy bedding. Mudstone Unit was deposited in mixed tidal sand-mud flat – tidal mud flat is characterized by wavy and lenticular bedding. text |
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Stratigraphy of study area consists of three litostratigraphic units, those units are Sandstone Unit of Bayah Formation, Mudstone Unit of Batuasih Formation, and Limestone Unit of Rajamandala Formation. There are ten litofacies in study area, those are, conglomeratic sandstone (Sg), cross bedded sandstone (Sp), bioturbated sandstone (Sb), carbonaceous sandstone (Sc), parallel laminated sandstone (Sh), flaser bedded sandstone Sf), wavy bedded sandstone (Sw), lenticular bedded sandstone (Fl), laminated sandstone (Fsc), and bioclastic limestone (Lk). Result of this study shows that Sandstone Unit and Mudstone Unit in this area have deposited in transition environment that have tidal influence, vertical succession is shallowing upward. Sandstone Unit was deposited in tidal sand flat – mixed tidal sand-mud flat that characterized by flaser and wavy bedding. Mudstone Unit was deposited in mixed tidal sand-mud flat – tidal mud flat is characterized by wavy and lenticular bedding. |
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Final Project |
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JULI ANDIKA CHANDRA (NIM 12005011), JUAN |
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JULI ANDIKA CHANDRA (NIM 12005011), JUAN #TITLE_ALTERNATIVE# |
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JULI ANDIKA CHANDRA (NIM 12005011), JUAN |
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JULI ANDIKA CHANDRA (NIM 12005011), JUAN |
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https://digilib.itb.ac.id/gdl/view/13587 |
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