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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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id-itb.:135032017-09-27T11:46:39Z#TITLE_ALTERNATIVE# MAHAR PAMUNGKAS (NIM 12006002); Pembimbing: Dr. Ir. Yan Rizal R., Dipl. Geol., dan Dr. Asw, GINANJAR Indonesia Final Project INSTITUT TEKNOLOGI BANDUNG https://digilib.itb.ac.id/gdl/view/13503 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. text |
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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), facies of massive sandstone, facies of conglomerate, and facies of debris flow. |
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MAHAR PAMUNGKAS (NIM 12006002); Pembimbing: Dr. Ir. Yan Rizal R., Dipl. Geol., dan Dr. Asw, GINANJAR |
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MAHAR PAMUNGKAS (NIM 12006002); Pembimbing: Dr. Ir. Yan Rizal R., Dipl. Geol., dan Dr. Asw, GINANJAR #TITLE_ALTERNATIVE# |
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MAHAR PAMUNGKAS (NIM 12006002); Pembimbing: Dr. Ir. Yan Rizal R., Dipl. Geol., dan Dr. Asw, GINANJAR |
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MAHAR PAMUNGKAS (NIM 12006002); Pembimbing: Dr. Ir. Yan Rizal R., Dipl. Geol., dan Dr. Asw, GINANJAR |
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https://digilib.itb.ac.id/gdl/view/13503 |
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