Petrology, Geochemistry, and Magma Evolution Of Basaltic Rocks Of Baturraden Area, Central Java, Indonesia.

Authors

  • Yogi Adi Prasetya Department of Geological Engineering, Faculty of Engineering, Universitas Jenderal Soedirman Jln. Mayjen Sungkono Km.5, Purbalingga, Indonesia
  • Akhmad Khahlil Gibran Department of Geological Engineering, Faculty of Engineering, Universitas Jenderal Soedirman Jln. Mayjen Sungkono Km.5, Purbalingga, Indonesia
  • Mochammad Aziz Department of Geological Engineering, Faculty of Engineering, Universitas Jenderal Soedirman Jln. Mayjen Sungkono Km.5, Purbalingga, Indonesia
  • Siswandi Department of Geological Engineering, Faculty of Engineering, Universitas Jenderal Soedirman Jln. Mayjen Sungkono Km.5, Purbalingga, Indonesia

DOI:

https://doi.org/10.25299/jgeet.2024.9.04.17882

Keywords:

Slamet Volcano, Baturraden, Magma Evolution, Magma Mixing

Abstract

Slamet volcano is the second highest active stratovolcano in Java Island, it has a long volcanic history eruption event, the Baturraden Area is a tourism area in southern part of Slamet Volcano. Baturraden area is the part of Banyumas Regency and it took 30-60 minutes riding motorcycle from Purwokerto city. Our research is focused on studying the petrology, geochemistry, and geological history of basaltic lava on Baturraden Area mainly that formed a waterfall on its location, because there is no a researcher that study basaltic lava on Baturraden, we focus on petrology, and petrography and geochemistry of basaltic lava on Baturraden using XRF methods and focused on magma evolution of basaltic lava rocks on Baturraden Area. Stratigraphically basaltic rocks in Baturraden Area are a part of Slamet Lava 1(SL 1) and Slamet Lava 2 (SL 2). The mineral composition of SL 1 and SL 2 are including the phenocryst of plagioclase, K-feldspar, olivine, clinopyroxene, and opaque minerals, with plagioclase microlites and volcanic glass as groundmass. Plagioclase shows zoning and sieve texture. Seven rock samples are prepared for whole-rock major element compositions of the study, the SiO2 contents range from 48.13 – 49.17 wt.%. The K2O contents in all rock samples range from 0.78 – 1.56 wt.%. Geochemical data confirm that SL 1 and SL 2 are from same magma type that magma of SL  1 and SL 1 are influenced by fractional crystallization and magma mixing from new injection of more basaltic magma, as evidenced by the frequent changes in SiO2 content.

Downloads

Download data is not yet available.

References

Barber, N. D., Baldwin, S. L., Edmonds, M., Boschetty, F. O., Wibowo, H. E., & Harijoko, A. (2023). Monogenetic volcanoes as windows into transcrustal mush: A case study of Slamet and Loyang volcanoes, Central Java. Journal of Volcanology and Geothermal Research.

Djuri , M., Samodra, H., Amin, T. C., & Gafoer, S. (1996). Peta Geologi Lembar Purwokerto - Tegal Skala 1:100.000. Bandung: Pusat Penelitian dan Pengembangan Geologi.

Global Volcanism Program. (2013). ( National Museum Of Natural History Smithsonian Institution) Retrieved April 05, 2022,

Handley,, H. K., Blichert-Toft, J., Gertisser, R., Macpherson, C. G., Turner, S. P., Zaennudin, A., & Abdurrachman,, M. (2014). Insight from Pb and O isotopes into along arc variation in subduction inputs and crustal assimilation for volcanic rocks in Java, Sunda arc, Indonesia. Geochimica et Cosmochimica Acta, 205-226.

Harijoko, A., Alifcanta, M. L., Moktikanana, M. L., & Abdillah, M. Y. (2022). Magma Evolution of Lasem and Senjong Volcanic Complex: High-K Magmatism in Sunda Arc, Indonesia. Indonesian Journal on Geoscience, Vol. 9(1), 131-145.

Harijoko, A., Milla, A., Wibowo, H. E., & Setiawan, N. I. (2020). Magma evolution of Slamet Volcano, Central Java, Indonesia based on lava characteristic. The 3rd Environmental Resources Management in Global Region.

Harijoko, A., Sari, S. A., Wibowo, H. E., Setiawan, N. I., & Moktikanana, M. L. (2021). Stratigraphy, chronology, and magma evolution of Holocene volcanic products from Mt. Slamet deposited in the Guci Valley, Central Java, Indonesia. Journal of Volcanology and Geothermal Research.

Iswahyudi, S., Permanajati, I., Setijadi, R., Zaenurrohman, J. A., & Pamungkas, M. A. (2020). Origin of Geothermal Water Around Slamet Volcano,Paguyangan,Cipari, Central Java, Indonesia. Journal of Geoscience, Engineering, Environment, and Technology, 181-184.

Le Bas, M., Le Maitre, R., Streckeisen, A., & Zanettin, B. (1986). A Chemical Classification of Volcanic Rocks Based on the Total Alkali Silica Diagram. Journal of Petrology, 745-750.

Le Maitre, R. W. (2002). Igneous Rocks a Classification and Glossary of Terms 2nd Edition Recommendations of the International Union of Geological Science Subcommision on the systematics of igneous rocks. University Press Cambridge.

Mulyaningsih, S., Bronto, S., Kusniadi, A., Apriyanti, L., Budiyanto, L., & Wiloso, D. A. (2022). The Petrology and Volcano-Stratigraphyof The Muria-Peninsula High-K Volcanic Rocks, Central Java, Indonesia. Journal of Geoscience, Engineering, Environment, and Technology, 69-80.

Peccerillo, A., & Taylor, S. (1976). Geochemistry of Eocene calc-alkaline volcanic rocks in Turkey. Contrib. Mineral. Petrology, 68, 63-81.

Prasetya, Y. A., & Gibran, A. K. (2024). Geologi Gunung Slamet Tua Dan Gunung Slamet Muda : Kajian Geomorfologi, Petrologi, Geowisata, Dan Bencana Geologi. Jurnal Geosaintek, 71-84.

Prasetya, Y. A., & Toramaru, A. (2022). Petrology and Geochemical Comparation of Pumice and Scoria Rocks of Slamet Volcano, Central Java. Journal of Applied Sciences, Management and Engineering Technology, Vol 3(1), 19-28.

Reubi,, O., & Nicholls, I. A. (2004). Magmatic evolution at Batur volcanic field, Bali, Indonesia: petrological evidence for polybaric fractional crystallization and implication for caldera forming eruption. Journal of Volcanology and Geothermal Research, 345-369.

Sendjaja,, Y. A., Kimura, J. I., & Sunardy, E. (2009). Across-arc geochemical variation of Quatenary lavas in West Java, Indonesia: Mass-balance elucidation using arc basalt simulator model. Island Arc, 18, 201-224.

Sutawidjaja, I. S., & Sukhyar, R. (2009). Cinder cones of Mount Slamet, Central Java, Indonesia. Journal Geologi Indonesia, Vol. 4(No 1), 57-75.

Sutawidjaja, I. S., Aswin, D., & Sitorus, K. (1985). Geology Map Of Slamet Volcano, Central Java. Bandung: Volcanology Survey of Indonesia.

Vukadinovic, D., & Nicholls, I. A. (1989). The Petrogenesis of Island arc basalt from Gunung Slamet Volcano, Indonesia: Trace element and 87Sr/86Sr Constrain. Geochimica et Chosmochimica, 53, 2349 - 2362.

Vukadinovic, D., & Sutawidjaja , I. (1995). Geology, Mineralogy and Magma Evolution of Gunung Slamet Volcano. Journal Southeast Asian Earth Science, 11(2), 135 - 164.

Wibowo, H. E., Nakagawa, M., Kuritani , T., Furukawa , R., Prambada, O., & Haraijoko, A. (2022). Petrological and geochemical study of Sundoro Volcano, Central Java, Indonesia: temporal variations in differentiation and source processes during the growth of an individual Volcano. Journal of Petrology, 1-22.

Winter, J. (2013). Principle of Igneous and Metamorphic Petrology. London: Pearson Education Limited.

Yudiantoro, D. F., Haty, I. P., Pambudi, S., Magdalena, E., Putri, A., Takashima, I., & Abdurrachman, M. (2022). Evolution Magmatism of Nagasari Volcano Dieng, Central Java, Indonesia. Journal of Geoscience, Engineering, Environment, and Technology, 140-150

Downloads

Published

2024-11-26 — Updated on 2024-12-27

Versions