#TITLE_ALTERNATIVE#
Depending on morfological shape and process in research area, this area devide into four geomorfological units, which is Anticline Mountain Unit, Fault Scarp Unit, Fold Limb Mountain Unit, and Flood Plain Unit. Stratigraphy units in research area consist of Massive Sandstone Unit, Bedding Sandstone...
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/13925 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | Depending on morfological shape and process in research area, this area devide into four geomorfological units, which is Anticline Mountain Unit, Fault Scarp Unit, Fold Limb Mountain Unit, and Flood Plain Unit. Stratigraphy units in research area consist of Massive Sandstone Unit, Bedding Sandstone Unit, Claystone Unit, and Alluvium Unit. That stratigraphy units equal with three formation, Batupasir Haloq in Late Eocene, Batu Ayau Formation in Late Eocene, and Ujoh Bilang Formation in Early Oligosen (Abidin, et al., 1993). Structures in research area consist of fault and fold, Leng Normal Fault with N-S direction, Merah Strike Slip Fault with NW-SE direction, and Leng Anticline with NE-SW fold axis. |
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