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The research area is divided into three geomorphologic units. Those geomorphologic units are Folded Mountains unit, Homoclinal ridge unit and the Alluvial plain unit. All the stages of the research area are situated on medium and mature stage. The stratigraphy of research area is equal to Meliat For...
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| Institution: | Institut Teknologi Bandung |
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id-itb.:134222017-09-27T11:46:45Z#TITLE_ALTERNATIVE# MUJIONO (NIM 12005060), EKO Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13422 The research area is divided into three geomorphologic units. Those geomorphologic units are Folded Mountains unit, Homoclinal ridge unit and the Alluvial plain unit. All the stages of the research area are situated on medium and mature stage. The stratigraphy of research area is equal to Meliat Formation, Tabul Formation and Tarakan Formation. Those Formations are divided into four informal units which are formed since Late Miocene up to recent. These units are: Quartz Sandstone, Sandstone-Claystone, Sandstone and Alluvial deposits The geological structure which is dominated in the research area can be determine from the lineament, topographic map and SRTM image. Geological structure which is grown in this research area is fold with NW-SE trend and fault. Fault in research area into boundary between Quarts Sandstone and Sandstone-Claystone. Generally, the depositional environments of the research area have shown the influence of river procces. text |
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The research area is divided into three geomorphologic units. Those geomorphologic units are Folded Mountains unit, Homoclinal ridge unit and the Alluvial plain unit. All the stages of the research area are situated on medium and mature stage. The stratigraphy of research area is equal to Meliat Formation, Tabul Formation and Tarakan Formation. Those Formations are divided into four informal units which are formed since Late Miocene up to recent. These units are: Quartz Sandstone, Sandstone-Claystone, Sandstone and Alluvial deposits The geological structure which is dominated in the research area can be determine from the lineament, topographic map and SRTM image. Geological structure which is grown in this research area is fold with NW-SE trend and fault. Fault in research area into boundary between Quarts Sandstone and Sandstone-Claystone. Generally, the depositional environments of the research area have shown the influence of river procces. |
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Final Project |
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MUJIONO (NIM 12005060), EKO |
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MUJIONO (NIM 12005060), EKO #TITLE_ALTERNATIVE# |
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MUJIONO (NIM 12005060), EKO |
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MUJIONO (NIM 12005060), EKO |
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https://digilib.itb.ac.id/gdl/view/13422 |
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