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

Petrochemistry of Ultramafic Rock in Baula - Pomalaa Ophiolite Complex, Southeast Sulawesi, Indonesia Cendrajaya, Rio Irhan Mais; Juarsan, Laode Ihksan; Masri; Rubaiyn, Al; Syahrul; Neni; Ramadani, Suci; Hasria
Journal of Geoscience, Engineering, Environment, and Technology Vol. 9 No. 1 (2024): JGEET Vol 09 No 01 : March (2024)
Publisher : UIR PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.25299/jgeet.2024.9.1.14491

Abstract

Baula and Pomalaa Ophiolitic Complexes are part of East Sulawesi Ophiolite (ESO). The ultramafic rocks in the Baula and Pomalaa Ophiolite Complex mainly is peridotite and consist of harzburgite, lherzolite and olivine websterite, mostly serpentinized. Chemical and petrological research has focused on minerals, such as olivine, pyroxene, and spinel. This study examines the tectonic setting and temperature of ultramafic rock formation. Twelve ultramafic rock samples were examined using geothermometers made of pyroxene, petrographic examination, and coexisting olivine and spinel analyses. SEM and petrographic analysis of pyroxene lamellae and mylonite-ultramylonite structures allowed for the measurement of the geothermometer of ultramafic rocks. Using SEM-EDS, the coexistence of olivine and spinel was analyzed to determine the type of ultramafic tectonic setting. In the coexistence of olivine and spinel, olivine and spinel oxide compounds as tectonic setting markers in the form of Fo and Cr# values. Ultramafic rocks have different temperature levels, based on pyroxene thermometer, and the first one starts at a high temperature of 1000-1200ºC. It is characterized by thin, elongated augite lamellae. Instead, large lamellae characterize augite at medium temperatures (800–1000ºC). Irregular, anhedral, and broader forms of enstatite lamellae are typical of low temperatures (500–800ºC). Different generations of exsolution lamellae indicate that magma cooling was gradual. The distribution of #Fo ranged from 0.87 to 0.92, and Cr# values ranged from 0.13-0.19. According to coexisting olivine and spinel analysis. On the Olivine-Spinel Mantle Array (OSMA), the Fo and Cr# plot indicates that the peridotites tectonic setting was from the ocean floor and the magmatism was from MORB (Mid Oceanic Ridge Basalt). The Al2O3 vs. TiO2 pattern in spinel lherzolite also similar with Ampana and Kabaena peridotites magmatism.
Assessing the Carbon Sequestration Potential of Ultramafic Rocks in the Kolaka Ophiolite Complex, Southheastern Sulawesi: A Petrographic, Geochemical, and Mineralogical Study Syahrul; La Ode Dzakir; Riska; Rio Irhan Mais Cendra jaya; Masri
Journal of Geoscience, Engineering, Environment, and Technology Vol. 10 No. 1 (2025): Article In Press JGEET Vol 10 No 01 : March (2025)
Publisher : UIR PRESS

Show Abstract | Download Original | Original Source | Check in Google Scholar

Abstract

Climate change has prompted significant global interest in carbon sequestration technologies, particularly using geological formations. This study investigates the potential of ultramafic rocks from the Kolaka Ophiolite Complex in Southeast Sulawesi for carbon sequestration, focusing on the mineralogical, petrographic, and geochemical characteristics that enhance their reactivity with CO₂. The research involved petrographic and mineragraphic analyses of 15 peridotite samples, geochemical measurements via X-ray fluorescence (XRF), and mineral characterization using scanning electron microscopy (SEM). The results revealed that Kolaka's ultramafic rocks, particularly harzburgite and lherzolite, exhibit moderate to high serpentinization, which enhances their reactivity with CO₂. Key minerals such as olivine, pyroxene, and serpentine, rich in magnesium, calcium, and iron oxides, demonstrate significant potential for mineral carbonation. Secondary minerals like magnesite and brucite were identified as products of carbonation, reinforcing the rocks' ability to act as carbon sinks. The discussion highlights that serpentinized peridotites are more effective for carbon sequestration than unaltered ones due to increased mineral reactivity. The presence of magnesite and Cr-Fe-rich carbonates, alongside serpentine veins, indicates that fluid-rock interactions have promoted ongoing carbonation processes. The Kolaka ultramafic rocks, therefore, hold strong potential for long-term carbon storage, offering a promising solution for reducing atmospheric CO₂ levels
Co-Authors Abdal, Nurul Mukhlisa Abdillah, Fardan Abdul Muis Mapalotteng Abdul Muis Mappalotteng Achmad Padil Adhistya Aulia DH afwan, zul Ahmed J. Obaid Aidil Akbar, Farid Aksar, Attariq Dihqan Faza Algazali Alifya NFH Alifya Nurilmi Fony Hasanuddin Ameliati, Sri Aminuddin Bakry Amir Amril Aman Anas Arfandi Andi Akram Nur Risal Andi Satriani Andi Syamsul Alam Bulu Andi Zulfikar Yusuf Aras, Andi Arianti, Annisa Armin, Nurfajrianti ASP, Verdana Islami Asri, Suci Aulia Aulia, Fajri Febrini Ayu Lestari Baso, Fadhlirrahman Bima Fandi Asy’arie Darmi Deperman Kasmora Desi Ramayana Desyana, Gita Dewi Fatmarani Surianto Dirawan, Gufran Darma Djaya, Andi Muhammad Fiqri Muslih Djunaedi Donal Yusuf Hutauruk Dwi ASTUTI Dwi Rezky Anadari Sulaiman Dwi Rezky Anandari Dyah Vitalocca Eka Agustina Elvinda, Rise Fajriani Farida Fathahillah Fauzan Azmi Femmy Angreany Ferry Cahyadi Fikri Vahriza Fithria Fitriah, Reski Habir Hafifah, Nur Hafsah, Hafni Hamdillah, Andi Hamzah, Muh. Qardawi Harlina Harlina Harlina Hasria Hendra Jaya Heri Hermawan Hokama, Naoki I Made Nuarsa I Made Suartika I.D.K. Okariawan Ibnumal Ida Bagus Alit Ilham Habinsaran Imran Imran, Andi Ahmad Ali Indah Wulandari Irwansya Irwansyah Suwahyu Ishak, Suryadi Ismail Qadri Iwan Suhardi Izu, Cynthia C. Jamal, Karmila Jamaluddin, Norliza Binti Jaya, Rio Irhan Mais Cendra Juanda Astarani Juarsan, Laode Ihksan Jumadi Mabe Parenreng Jumadin Kalsum Kamal, Annisa Septiani Kamaruddin Kintani, Aulia Ratu Kurnia Prima Putra La Ode Dzakir Labusab Lu'mu M. Akmal Fauzan M. Syahid Nur Wahid Mahbub Humaidi Aziz Mahmud Mustapa Maisura Mansyur Marwan Ramdhany Edy Masfufah Masri Masri Mayyani, Hidayatul Melanni, Melyan Miftahul Janna Mochamad Tito Julianto Moh. Buny Andaru Bahy Muh. Jaelani Suwardy Muhammad Asriadi Muhammad Fajar B. Muhammad Ilhan Muhammad Kamran Muhammad Nur Muhammad Rais Muhammad Yahya Muhammad Yasin Muhammad, Fadhil Muliadi Mutia Sofiani N. Papalan, Alriomesta Nasruddin NENI Ninik Rahayu Ashadi Noer Chadijah L Sam Nur Aisyah Nur Alam, Eka Nur Auliyah Syahruni Syam Nurcahyo, Edy Nurchalis, Nurfadillah Nurdin Nurdin Nurmi Nursinah Amir, Nursinah Nurul Nurul Mukhlisah Abdal Nurzamzam Prapto Tri Supriyo Putri, Ulfhi Aliyandha Rahmat Makmur, Azharu Rahmatul Rizky Ramadani, Suci Ria Sakinah Waji Riana T. Mangesa Ridwan Daud Mahande Rise Elvinda Riska Riska, Muhammad RR. Ella Evrita Hestiandari Rubaiyn, Al Rustam Sabaria, Sabaria Sabrianil Safia Maulida Safitri, Loli Safrin Salam Saharuna Saito, Ruka Saltanat Meiramova Sari, Rizki Mustika Sato, Mayumi Satriani Seprina Aulia Putri Septianto, Fendy Shabrina Syntha Dewi Siswandi Solly Aryza Sugimoto, Hiroshi SUWARTI Syafitri, Widya Syahrul Ramadana Syamsurijal Syarfi Aziz Syarifaturrahmatullah Syntha Dewi, Shabrina Tahir, Mufti Hatur Rahmi Takril Tang, Beddu Tantut Susanto Tonny, Fajrin Veronika Asri Tandirerung Vivi Keumala Mutiawati Wahyuramadan Wan Muhammad Fariq willyansah, willyansah Wilyansyah Zahrawati B., Fawziah Zahrina, Nisa Afra Zakaria, H.M. Yusuf