#TITLE_ALTERNATIVE#
Physiographycally, research area is included in Bogor Zone. Geomorphologically research area consist of 3 units, are Homoclinal Ridge unit, Homoclinal Mountain unit, Low Peneplain, and the river show dendritic-subdendritic pattern Stratigrafically, there are 6 informal rocks unit in the research are...
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/13349 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | Physiographycally, research area is included in Bogor Zone. Geomorphologically research area consist of 3 units, are Homoclinal Ridge unit, Homoclinal Mountain unit, Low Peneplain, and the river show dendritic-subdendritic pattern Stratigrafically, there are 6 informal rocks unit in the research area, : Claystone, Limestone, Tuff-Sandstone, Breccia, Andesite Intrution, and Laharik Breccia. The oldest informal unit is Claystone Which aged Middle Miocene (N12-N13). In the research area, there are two thrust fault and one fault which have a direction Northeast-Southwest. It causes by tectonic process which happened in Late Miocene until Early Plistocene. |
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