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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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id-itb.:133492017-09-27T11:46:44Z#TITLE_ALTERNATIVE# NURWANI (NIM 12006018), CITRA Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13349 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. text |
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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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Final Project |
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NURWANI (NIM 12006018), CITRA |
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NURWANI (NIM 12006018), CITRA #TITLE_ALTERNATIVE# |
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NURWANI (NIM 12006018), CITRA |
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NURWANI (NIM 12006018), CITRA |
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https://digilib.itb.ac.id/gdl/view/13349 |
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