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Analisis Kematangan Batuan Induk Hidrokarbon di Formasi Naintupo, Sub-Cekungan Tarakan, Provinsi Kalimantan Utara

*FX Anjar Tri Laksono orcid scopus  -  Teknik Geologi, Fakultas Teknik, Universitas Jenderal Soedirman, Indonesia
Fendy Kusdiantoro  -  Divisi Eksplorasi, Medco E&P Indonesia, Indonesia
János Kovács  -  Department of Geology and Meteorology, Faculty of Sciences, University of Pecs, Hungary
Widhiatmoko Herry Purnomo  -  Departemen Teknik Elektro, Fakultas Teknik, Universitas Jenderal Soedirman,, Indonesia
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Abstract

Sub-Cekungan Tarakan yang terletak di Provinsi Kalimantan Utara diperkirakan memiliki potensi hidrokarbon sekitar dua miliar barel oil equivalent (BOE). Tujuan dari penelitian ini adalah menganalisis kematangan batuan induk dan potensi hidrokarbon di Formasi Naintupo, Sub-Cekungan Tarakan. Metode yang digunakan dalam kajian ini adalah analisis Total Organic Carbon (TOC), Vitrinite Reflectance (Ro), Hydrogen Index (HI), Tmax, Potential Yield (PY), S1, Oxygen Index (OI), dan Oil Production Index (OPI). Hasil kajian ini adalah Formasi Naintupo merupakan batuan induk efektif menghasilkan hidrokarbon dengan nilai TOC antara 1,02-5,92 wt.%, HI 52-115 mgHC/gr TOC, Ro 0,62%-1,84%, Tmax 436oC-468oC, S1 0,17-0,32, dan OPI sebesar 0,15-0,4. Jenis hidrokarbon dengan potensi terbesar adalah gas bumi. Potensi gas bumi terbesar berada di Sumur South Sembakung-1, Tanjung Bimau-1, Sesayap E-1, dan Tanjung Kramat-1. Hasil analisis menunjukkan bahwa Formasi Naintupo berpotensi menghasilkan gas bumi di Sub-Cekungan Tarakan.

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Keywords: TOC;Ro; formasi Naintupo; hidrokarbon; sub-cekungan Tarakan

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