#TITLE_ALTERNATIVE#
Analysis of sequence units in Talangakar Bawah Formation obtained a sequence boundary (sequence boundary) and five flooding surfaces (FS). Sequence consists of TST sediments which were composed by retrogradation of conglomerates braided river sediments and retrogradation tide sediments (tidal mud fl...
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| Format: | Final Project |
| Language: | Indonesia |
| Online Access: | https://digilib.itb.ac.id/gdl/view/13234 |
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| Institution: | Institut Teknologi Bandung |
| Language: | Indonesia |
| Summary: | Analysis of sequence units in Talangakar Bawah Formation obtained a sequence boundary (sequence boundary) and five flooding surfaces (FS). Sequence consists of TST sediments which were composed by retrogradation of conglomerates braided river sediments and retrogradation tide sediments (tidal mud flat, tidal mixed tidal flat, tidal sand flat), followed by retrogradation of neritic sediments (middle shorface and lower shorface). Talangakar Bawah Formation consists of two reservoirs which are : reservoir 1 and reservoir 2. Reservoir 1 at interval FS 3-FS 4 is a tidal sand flat deposits which consisting of sandstone with maximum thickness 14 meters and maximum effective porosity 14%.While reservoir 2 at interval SB-FS is braided stream deposits which consisting of breccia with maximum thickness 60 meters and maximum effective porosity 20%. |
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