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Geomorphology of research area consists of three geomorphology units: Anticline Valley Unit, Lava Dome Unit and Alluvial Plain Unit. Historical geology of research area starts from Middle Miocene Epoch while deposition of Claystone-Sandstone Unit in Middle Neritic environment, then regression and co...
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/14551 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | Geomorphology of research area consists of three geomorphology units: Anticline Valley Unit, Lava Dome Unit and Alluvial Plain Unit. Historical geology of research area starts from Middle Miocene Epoch while deposition of Claystone-Sandstone Unit in Middle Neritic environment, then regression and continued conformably by deposition of Sandstone Unit in delta environment. This unit is depositioned at Late Miocene and contains coal intercalation. Plio-Pleistocene tectonic activity results deformation in research area such as Lematang Anticline and Kanti Fault. Andesite Unit is formed at Pleistocene in terrestrial environment and unconformably covers the older units. The younger unit in research area is Alluvial Unit and its deposition working until now. |
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