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Sedimentation study of the units in Cantayan Formation shows that the units were deposited by the turbidite and sub-marine fan system at upper bathyal environment. There are few facies of turbidite that are found in this study, those are: facies of classical tubidite (thin-bedded and thick-bedded),...
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/13503 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | Sedimentation study of the units in Cantayan Formation shows that the units were deposited by the turbidite and sub-marine fan system at upper bathyal environment. There are few facies of turbidite that are found in this study, those are: facies of classical tubidite (thin-bedded and thick-bedded), facies of massive sandstone, facies of conglomerate, and facies of debris flow. |
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