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Hasil Pencarian

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Vira Yunita
"Cekungan Banggai merupakan salah satu cekungan yang memiliki potensi hidrokarbon dan terletak di Sulawesi Tengah. Formasi Lower Kintom B yang terendapkan pada masa Pliosen Awal diinterpretasikan dapat menjadi reservoir hidrokarbon di Cekungan Banggai. Formasi ini terbentuk saat terjadinya kolisi antara Banggai-Sula dengan sabuk ofiolit Sulawesi Timur sehingga membentuk endapan molasse. Penelitian ini dilakukan untuk mengevaluasi sifat-sifat petrofisika batuan yang terdapat di Cekungan Banggai berdasarkan data log sumur yang terdapat pada sumur VR-3, VR-14, dan VR-15. Sifat-sifat petrofisika yang dihasilkan dari perhitungan ketiga log sumur, seperti nilai volume shale, porositas, dan saturasi air digunakan untuk penentuan kandidat reservoir yang juga didukung oleh data petrografi dan data mud log untuk mengetahui jenis litologi yang terdapat di zona reservoir. Berdasarkan hasil yang diperoleh, Formasi Lower Kintom B didominasi batulempung yang berasosiasi dengan batupasir dan batugamping di bagian atasnya. Batugamping tersebut diperkirakan sebagai zona reservoir Formasi Lower Kintom B, yaitu berupa batugamping mudstone hingga wackestone dan wackestone hingga packstone. Hasil perhitungan petrofisika pada zona reservoir Formasi Lower Kintom B didapatkan bahwa nilai volume shale berkisar antara 28-40%, nilai porositas efektif berkisar antara 14-36%, dan nilai saturasi air berkisar antara 29-40%.

The Banggai Basin is one of the basins that has potential for hydrocarbons and is located in Central Sulawesi. The Lower Kintom B Formation which was deposited in the Early Pliocene is interpreted to be a reservoir of hydrocarbons in the Banggai Basin. This formation was formed during a collision between Banggai-Sula micro-continent and the ophiolite belt of East Sulawesi which formed molasses deposits. This research was conducted to evaluate the petrophysical properties of the rocks in the Banggai Basin on well log data in the VR-3, VR-14, and VR-15 wells. Petrophysical resulting from the calculation of the three well logs, such as shale volume, porosity, and water saturation values are used to determine reservoir candidates which are also supported by petrographic and mud log data to determine the type of lithology in the reservoir zone. Based on the result obtained, the Lower Kintom B Formation is dominated by claystone associated with sandstone and limestone at the top. The limestone is interpreted to be a reservoir zone for the Lower Kintom B Formation, namely mudstone towackestone and wackestone to packstone. The result of petrophysics calculations in the reservoir zone of the Lower Kintom B Formation found that shale volume values ranged from 28-40%, effective porosity values ranged from 14-36%, and water saturation values ranged from 29-40%."
Depok: Fakultas Matematika dan Ilmu Pengetahuan Alam Universitas Indonesia, 2022
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UI - Skripsi Membership  Universitas Indonesia Library
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Rizka Novita Syahruddin
"Daerah penelitian terletak di Formasi Tomori Blok “X” Cekungan Banggai yang berada di wilayah Kabupaten Banggai, Provinsi Sulawesi Tengah. Formasi Tomori terendapkan pada masa Miosen Awal hingga Miosen Tengah dan diinterpretasikan dapat menjadi reservoir hidrokarbon di Cekungan Banggai. Formasi ini disusun oleh dominan batugamping bioklastik, terbentuk saat terjadinya proses syn-rift ketika aktivitas tektonik relatif tenang. Penelitian ini bertujuan untuk mengetahui karakteristik reservoir dengan mengevaluasi sifat-sifat petrofisika batuan yang terdapat di Formasi Tomori, Cekungan Banggai berdasarkan data log sumur R3 dan R2ST. Sifat-sifat petrofisika yang dihasilkan dari perhitungan ketiga log sumur, seperti nilai volume shale, porositas, dan saturasi air digunakan untuk rekomendasi reservoir yang didukung oleh data petrografi, serta data mudlog guna mengetahui jenis litologi di zona reservoir. Berdasarkan hasil yang diperoleh, Formasi Tomori tersusun atas batugamping mudstone, batugamping wackestone, dan batugamping packstone yang di beberapa interval ditemukan sisipan batubara dan batulempung. Hasil perhitungan petrofisika pada zona reservoir Formasi Tomori didapatkan nilai volume shale berkisar 38%-40%, porositas efektif 7%-0%, dan saturasi air 23%-34%.

The research area is located in the Tomori Formation Block "X" of the Banggai Basin in the Banggai Regency, Central Sulawesi Province. The Tomori Formation was deposited during the Early Miocene to Middle Miocene and is interpreted to be a hydrocarbon reservoir in the Banggai Basin. This formation is composed of predominantly bioclastic limestones, formed during syn-rift processes when tectonic activity is relatively calm. This study aims to determine the characteristics of the reservoir by evaluating the petrophysical properties of the rocks in the Tomori Formation, Banggai Basin based on well log data R3 and R2ST. Petrophysical properties resulting from the calculation of the three well logs, such as shale volume, porosity, and water saturation values are used for reservoir recommendations supported by petrographic data, as well as mudlog data to determine the type of lithology in the reservoir zone. Based on the results obtained, the Tomori Formation is composed of mudstone limestone, wackestone limestone, and packstone limestone which at some intervals was found intercalated with coal and claystone. The results of petrophysics calculations in the reservoir zone of the Tomori Formation obtained shale volume values ranging from 38%-40%, effective porosity 7%-10%, and water saturation 23%-34%."
Depok: Fakultas Matematika dan Ilmu Pengetahuan Alam Universitas Indonesia, 2022
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UI - Skripsi Membership  Universitas Indonesia Library