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Physiographically, studied area is belong to lowland and hills zone (van Bemmelen, 1949). Geomorphological unit of studied area consist of Anticlinal Ridge and Homoclinal Valley. Rocks in studied area is divided (from the oldest up to the youngest) to claystone with upper delta plain depositinal env...
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Format: | Final Project |
Language: | Indonesia |
Online Access: | https://digilib.itb.ac.id/gdl/view/13473 |
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Institution: | Institut Teknologi Bandung |
Language: | Indonesia |