#TITLE_ALTERNATIVE#
This research area is divided into two geomorphological units: Complex Mountain Unit and Coastal Plain Unit. Stratigraphy in research area is divided into four units: Middle Eocene Conglomeratic Sandstone Unit, Late Oligocene Sandstone Unit, Early Pliocene Conglomerate Unit, and Recent Aluvial-Coast...
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/13788 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | This research area is divided into two geomorphological units: Complex Mountain Unit and Coastal Plain Unit. Stratigraphy in research area is divided into four units: Middle Eocene Conglomeratic Sandstone Unit, Late Oligocene Sandstone Unit, Early Pliocene Conglomerate Unit, and Recent Aluvial-Coastal Deposit. Geological structures formed in the research area are reverse faults, strike slip faults, and folds. Research area is a part of fold-thrust belt which has formed by compressive tectonic. Reverse fault is the main structure in the research area, with strike slip faults and folds as accompaniment structures. Strike slip faults were formed by each block ability differences to accommodate compressive force. |
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