#TITLE_ALTERNATIVE#
Stratigraphy units of the study area are divided into seven informally rock units: Claystone-Sandstone and Sandstone unit (Late Oligocene) were deposited in shallow-middle neritik synchronized with Cijengkol Formatiom sandstone member, and then unconformately deposited Tuf-Sandstone Intercalated wit...
Saved in:
| Main Author: | |
|---|---|
| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/13284 |
| Tags: |
Add Tag
No Tags, Be the first to tag this record!
|
| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | Stratigraphy units of the study area are divided into seven informally rock units: Claystone-Sandstone and Sandstone unit (Late Oligocene) were deposited in shallow-middle neritik synchronized with Cijengkol Formatiom sandstone member, and then unconformately deposited Tuf-Sandstone Intercalated with Limestone (Early Miocene) were deposited in shallow-middle neritik synchronized with Citarate Formation tuf member, Limestone (Early Miocene) were deposited in shallow-middle neritik synchronized with Citarate Formation limestone member, Tuf-Sandstone Intercalated with Breccia (Early Miocene) were deposited in middle neritik synchronized with Citarate Formation tuf member, and then unconformately deposited Polymic Breccia (Early Miocene) were deposited in marineun, and Aluvial. The geological structures developed in this area is N-S trend strike slip fault found in Cibunar River and expected formed in Oligocene and reactivated in late of Early Miocene. |
|---|