DETAIL KOLEKSI

Rocktyping Pada Reservoir Batupasir A Dan B Berdasarkan Data Well Log Dan Core Di Lapangan X, Formasi Telisa Cekungan Sumatera Selatan


Oleh : Yansa Destrian

Info Katalog

Nomor Panggil : 970/TG/2018

Penerbit : FTKE - Usakti

Kota Terbit : Jakarta

Tahun Terbit : 2018

Pembimbing 1 : M. Ali Jambak

Pembimbing 2 : Benyamin S.

Subyek : Rocks;Geology

Kata Kunci : rocktyping, petrophysical analysis, flow zone indicator


File Repositori
No. Nama File Ukuran (KB) Status
1. 2018_TA_GL_072001300109_Halaman-judul.pdf 5033.74
2. 2018_TA_GL_072001300109_Bab-1.pdf 5675.63
3. 2018_TA_GL_072001300109_Bab-2.pdf 6158.75
4. 2018_TA_GL_072001300109_Bab-3.pdf 5697.79
5. 2018_TA_GL_072001300109_Bab-4.pdf 6131.55
6. 2018_TA_GL_072001300109_Bab-5.pdf 5675.73
7. 2018_TA_GL_072001300109_Daftar-Pustaka.pdf 5676.22
8. 2018_TA_GL_072001300109_Lampiran.pdf 6227.41

D Daerah penelitian berada pada lapangan “X”, yaitu terletak pada Cekungan Sumatera Selatan, Provinsi Sumatera Selatan. Dalam penelitian ini dilakukanbeberapa analisa menggunakan data log yang dipadukan dengan data batuan inti,yaitu analisa fasies, analisa petrofisika, dan unit rock type yang berada pada Formasi Telisa dari sumur 1, sumur 2, Sumur 3, Sumur 4 dan Sumur 5.Pada penelitian ini dilakukan pada lapisan reservoir batupasir A dan B pada formasiTelisa. Berdasarkan data struktur sedimen daerah penelitian yang ada pada sumur1, lapisan “A” pada lapangan "X" diendapkan lingkungan pengendapan mouthbar, channel dan prodelta. Berdasarkan hasil perhitungan analisa petrofisika danmembagi rock type pada daerah penelitian menggunakan metode Flow ZoneIndicator (FZI). Berdasarkan hasil penelitian menunjukan bahwa terdapat 4 tipe batuan (rock type) dari daerah penelitian berdasarkan harga FZI yang diperolehserta setiap rock type memiliki perbedaan kemampuan dalam mengalirkan fluida.

T The research area is located on the "X" field, which is located in the SouthSumatera Basin, South Sumatera Province. In this research, some analyzes usedwireline log and combined with core data, such as facies analysis, petrophysicalanalysis, and rock type unit located in Telisa Formation from well 1, well 2, well3, well 4 and well 5. In research this has done in the sandstone reservoir layer Aand B on the Telisa formation. Based on the data of the sediment structure of theresearch area present in well 1, the "A" layer in the "X" field deposite in themouth bar, channel and prodelta deposition environment. Based on thecalculation of petrophysical analysis and divide the rock type in the research areausing the method of Flow Zone Indicator (FZI). The results showed that there are4 rock types of the study area, based on FZI values each rock type has differentability in fluid flow.

T The research area is located on the "X" field, which is located in the SouthSumatera Basin, South Sumatera Province. In this research, some analyzes usedwireline log and combined with core data, such as facies analysis, petrophysicalanalysis, and rock type unit located in Telisa Formation from well 1, well 2, well3, well 4 and well 5. In research this has done in the sandstone reservoir layer Aand B on the Telisa formation. Based on the data of the sediment structure of theresearch area present in well 1, the "A" layer in the "X" field deposite in themouth bar, channel and prodelta deposition environment. Based on thecalculation of petrophysical analysis and divide the rock type in the research areausing the method of Flow Zone Indicator (FZI). The results showed that there are4 rock types of the study area, based on FZI values each rock type has differentability in fluid flow.

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