The Acid Zone Delineation In Tangkuban Parahu Geothermal Working Area

Authors

  • Arsyi Hadyan PT PLN (Persero), Jalan Trunojoyo Blok M-1 No. 135, Jakarta, Indonesia
  • Suryantini Suryantini Geothermal Engineering Master’s Program – Faculty of Mining and Petroleum Engineering (FTTM), Institut Teknologi Bandung (ITB), Jl. Ganesha 10, Bandung 40132, Indonesia

Keywords:

Tangkuban Parahu, geothermal, Acid zones, magnetotelluric, total conductance

Abstract

The Tangkuban Parahu Geothermal Working Area is located in West Java, Indonesia, and is dominated by volcanic products from Mt. Sunda and Mt. Tangkuban Parahu. Mt. Tangkuban Parahu was generated after Mt. Sunda eruption which produced large caldera. Acid zone in Tangkuban Parahu GWA becomes important to be studied regarding its origin which associated with intensive volcanic activity up to present days. The study applying the magnetotelluric data to determine the total conductance numbers for identifying anomalies corresponding acid zones. Total conductance with specific amount tied with acid manifestations in some locations to acquire approximate number of acid zones. The acid zone map delivered from total conductance data further calibrated with aleration zones and comprimising structure data. From preceding processes, the study has obtained the 2D distribution map of acid zone in Tangkuban Parahu GWA. The acid zone spread from the Kawah Ratu and Kawah Domas northward to Cijalu, northeastward to Ciater, and southward to Kancah. While Cikole and Amblongan estimated to be area which consist more benign fluids with near-neutral pH.

Downloads

Download data is not yet available.

References

Pratomo, I. (2006). Klasifikasi Gunung Api Aktif Indonesia,Studi Kasus Dari Beberapa Letusan Gunung Api Dalam Sejarah. Jurnal Geologi Indonesia.

Nasution, A., Kartadinata, M. N., Kobayashi, T., Siregar, D., Sutaningsih, E., Hadisantono, R., & Kadarstia, E. (2004). Geology, Age Dating and Geochemistry of the Tangkuban Parahu Geothermal Area, West Java, Indonesia. J. Geothermal Resource Soc. Japan.

Boedihardi, M., Suranto, & Sudarman, S. (1991). Evaluation Of The Dieng Geothermal Held; Review Of Development Strategy. IPA 20th Annual Convention Proceedings.

Ohm, G. S. (1827). The Galvanic Circuit Investigated Mathematically (T. D. Lockwood (trans.)). Kraus Reprint Co.

Sunardi, E. and Kimura, J. (1998) Temporal chemical variation in Late Cenozoic volcanic rocks around the Bandung Basin, West Java, Indonesia. J. Min. Petr. Econ. Geol.,vol. 93, 103-128.

Sutoyo and Hadisantono, R. (1992) Geological map of Tangkuban Parahu volcano, West Java. Bandung, Indonesia.

Stoffregen, R. (1987). Genesis of acid-sulfate alteration and Au-Cu-Ag mineralisation at Summitville, Colorado. Economic Geology, vol. 82, 1575-1591.

Nasution, A., and Nasution M. P. (2021). Geochemical Modeling of Acid Fluid from Volcanic Geothermal Areas, Case Study of Indonesian Geothermal Prospects. Proceedings World Geothermal Congress 2020+1

Chave, A. D., & Jones, A. G. (2012). The Magnetotelluric Method: Theory and Practice. Cambridge University Press

Downloads

Published

2025-01-20

How to Cite

Hadyan, A., & Suryantini, S. (2025). The Acid Zone Delineation In Tangkuban Parahu Geothermal Working Area. ITB Graduate School Conference, 4(1). Retrieved from https://gcs.itb.ac.id/proceeding-igsc/index.php/igsc/article/view/437

Issue

Section

Articles