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Journal : Journal of Geoscience, Engineering, Environment, and Technology

Quantifying hydrothermal alteration Derived by remote sensing technique in Tompaso Geothermal Field (North Sulawesi Indonesia) Bariadi, Laode; Saepuloh, Asep
Journal of Geoscience, Engineering, Environment, and Technology Vol. 10 No. 1 (2025): JGEET Vol 10 No 01 : March (2025)
Publisher : UIR PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25299/jgeet.2025.10.1.19515

Abstract

Quantifying hydrothermal alteration is important for geothermal system modeling, which aims to understand fluid dynamics, soil distribution, and energy production potential in the geothermal exploration areas as well as the economic mineral potential at the Tompaso area, North Sulawesi. Alteration processes can result in weathering degradation of rock strength. The Sentinel-2 color composite of band ratio R,G,B for band (4/2), band (8A/11), and band (11/12) reveals the distribution of iron oxides, ferromagnesian silicates, and clay minerals. These alteration minerals are characterized by the presence of clay minerals such as chlorite (Chl), epidote (Ep), quartz (Qs), sericite (Sr), alunite (Al), and illite (ill), which formed at temperatures of 110-300⁰C and fluid pH ranging from 3-5 (acidic in nature). The process of geological phenomena in the form of structures that open fluid pathways affects changes in the physical and chemical composition of the host rocks. The host rock and hydrothermal interactions influence to the fertility as well as vegetation conditions. Therefore, the soil and vegetation conditions were used to trace the occurrence of hydrothermal alteration minerals. A band ratio of the chlorophyll spectrum captured by the red edge vegetation index (REVI) is used as a basis for mapping vegetation stress related to the occurrence of the alteration minerals. The insitu chlorophyll measurements of ferns were used to verify the REVI in the study area. The REVI image shows anomalous vegetation stress corresponding to alteration minerals. To quantify the detection correctness, the SPAD soil measurements were conducted to pinpoint vegetation stress caused by the existence of hydrothermal alteration minerals. Correlation between alteration minerals to these two variables REVI and fern SPAD. The determination coefficient (R2) between REVI and alteration minerals then the alteration minerals and SPAD chlorophyll measurements were archived linearly about 0.7. We have also obtained a linear correlation with positively gradient between alteration zones of argillic and propylitic presented by occurrences of kaolinite, sericite, chlorite, epidote, and quartz minerals in rock samples, to stressed vegetations.
Co-Authors Abdul Fatah Hassanudin Adawiyah, Sulistia Nursyamsiyah Adelia Adiningsih, Cinde Adi Firmansyah Adriansyah, David Agus Handoyo Harsolumakso, Agus Handoyo Agustiningtyas, Lestari Alkusani, Alkusani Ananda Bagus Satria Andhinna Yunniekasari Andri Muhammad Nuroni Andri Sukmaindrayana Awit Marwati Sakinah Awwaliyah, Nurul Aini Al Bambang Handoko Bariadi, Laode Budiyono Pristyadi Butet Oyong Nurasiah D. Nurfajrin Ningsih Damar Nandiwardhana, Damar Damayanti, Mila Aisilia Daru Maliki Destya Forcsa Dewantoro, Ahmad Qoni Dewi, Rosiana Dhatu Kamajati, Dhatu Diningsih, Cinde Adia Dodo Eka Pristianti S Elis Homsini Maolida Elkin Rilvani Estu Kriswati Fadila Siti Nuraeni Fahmi, Raizal Fajar Yunawwirudin febriani, ermila Febriyana, Karisman Fitri Syakinah Frederikus Dian Indrastomo, Frederikus Dian Ghazali, Mochamad Firman Gumilar, Irfan Rizki Hadi Ismanto Hadi Supratikta Halimah Halimah Halimah Hapid Burhanudin Haryanto Lukmana, Allen Hassanudin, Abdul Fatah HENDRA GUNAWAN B11211055 Hendra Suwardana Heru Baskoro I Gde Sukadana Ida Nuraida Imel Aura Agustin Iskandar, Risda Alena Jauhar Helmie Kahfi, Martin Ketut Wikantika Komala, Ela Kurniawan, Rajab Lucky Anggara Melsandi Mila Salbiyah Mirani Erliana S Nadila Elsa Nailah Sayyidatii Hayaa Nia Kurniawati Ningsih, Dinni Nurfajrin Nugraha, Agus Ramdhani Nugraha, Sukma Nugraha, Yudhistira Adika Nur Fauziah Putri Nuraeni, Intan Nurfajrin Ningsih, Dini Nurfitria Khoirunisa Nurhayati Halimatu Sya'diah, Siti Nurjaman Panji Anwar Sanusi Perwito, Perwito Pina Aulia M Prayoga, Ardy Setya Prihadi Sumintadireja, Prihadi Primadipta, Indira Wido Purnamasari, Heruningtyas Desi Rahmanto, Ridwan Ramadhani, Siva Malika Putri Ratnawati, Yeli Restiani Ria Zulfiana Rima Rachmayani, Rima Rizqi, Maulidyah Amalina Rohaeni, Anie Rudyana, Ikhsan Saepuloh Sahana, Muhammad Irham Salsabila, Vina Aini Sarip Hidayatulloh Setianto, Nasrul Setiawan, Rahyuniati Setiawati, Wawat Siti Mardiana Siti Maryam Slamet Rahayu Sofyan Primulyana Sukaris Sulistiyani, Adinda Sungkawa, Muhamad Guntur Gaos Suyono, Annisa Maharani Syahla Mutia Aini Syamsi, Wuri Arianty Taufan Abdurrachman Taufiqurrahman, Moh. Tiaradia Ihsan Tri Herdiawan Apandi Tri Muji Susantoro, Tri Muji Veronika Simanjutak Very Susanto vina andriani Vina Nurviyani Wenti Krisnawati Wijaya, P. Hadi Yeni Suryani Yoga Sampurna Yulia Nur Annisa Yundani Irmala Zaki Hilman Zuber