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The geomorphological of research area divided into three units, there are Homoklin Hills Unit, Volcanic Hills Unit, and Alluvial Plain Unit. Classification of three units based on morphology and geological condition. The stratigraphy of research area divided into four unformal units, there is Clayst...
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id-itb.:138052017-09-27T11:46:39Z#TITLE_ALTERNATIVE# (NIM 12006039), RONALD Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13805 The geomorphological of research area divided into three units, there are Homoklin Hills Unit, Volcanic Hills Unit, and Alluvial Plain Unit. Classification of three units based on morphology and geological condition. The stratigraphy of research area divided into four unformal units, there is Claystone Unit (Middle Miocene), Sandstone-claystone Unit (Middle Miocene), Volcanic Breccia Unit (Pleistocene), and Alluvial Unit (Recent). Based on the equal of lithological features, Claystone Unit and Sandstone-claystone Unit be equal with Formasi Bantargadung. The deformation of research area happened during Plio-Pleistocene with the main force in north-south direction resulted reverse fault in west-east direction and then strike-slip fault in north-south direction. text |
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The geomorphological of research area divided into three units, there are Homoklin Hills Unit, Volcanic Hills Unit, and Alluvial Plain Unit. Classification of three units based on morphology and geological condition. The stratigraphy of research area divided into four unformal units, there is Claystone Unit (Middle Miocene), Sandstone-claystone Unit (Middle Miocene), Volcanic Breccia Unit (Pleistocene), and Alluvial Unit (Recent). Based on the equal of lithological features, Claystone Unit and Sandstone-claystone Unit be equal with Formasi Bantargadung. The deformation of research area happened during Plio-Pleistocene with the main force in north-south direction resulted reverse fault in west-east direction and then strike-slip fault in north-south direction. |
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