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Journal : Journal of Geosciences and Applied Geology

PETROGENESIS OF PASIR CUPU DIORITE, PLERED DISTRICT, PURWAKARTA, WEST JAVA Fachrudin, Kurnia Arfiansyah; Aini, Hana Nur; Syafri, Ildrem; Luthfi, Ahmad; Amitama, Emilia Bunga
Journal of Geological Sciences and Applied Geology Vol 2, No 5 (2018): Journal of Geological Sciences and Applied Geology
Publisher : Faculty of Geological Engineering, Universitas Padjadjaran

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.24198/gsag.v2i5.20316

Abstract

Pasir Cupu located in the area of Plered and Sukatani, Purwakarta, West Java. It is geographically on 107o 26 '25.2' - 107o 27 '16.8' Easternmost and 6o 37 '22.8' - 6o 37 '03 "Southtermost. The Pasir Cupu is a formally formed intrusion, and classified into diorite (Streckeisen, 1978 in Gillespic and Styles, 1999). The method used is petroloogy, petrographic, and geochemical analysis using the XRF and CIPW methods. The megascopic appearance shows gray-colored rocks - in fresh, black-brown gray - in weathered ones; masive; very hard; fanheritic porphyritic textures; contains dark and bright minerals, dark minerals estimated to be amphibol, and pyroxene, and minerals that are bright feldspar; and masasaras are gray. Microscopic observations of 3 thin section of rock samples (CP 1, CP2 and CP3), showed porphyritic-afanitic texture, hypocrystalline, hypidiomorphic; composed of phenocryst plagioclase, amphibol, pyroxene, biotite, with mineral sizes between 0.1 mm - 4 mm; there are also small amounts of opaque, K-feldspar, quartz and carbonate minerals; with medium-coarse-grained bottom, consisting of plagioclase microlite, amphibole microlite, pyroxene and biotite microlite, carbonate minerals, chlorite and clay minerals. Based on geochemical analysis, Pasir Cupu is composed by diorite according to the Total Alkali Silica diagram. The magmatic series is included in the Calc-Alkaline and Thoeliitic series, the types of magma include the High-K and Medium-K (Calc-Alkaline Series) groups, as long as magma interacts with continental crust (continent), as long as the magma is based on the Island Arc Calc -Alkaline Basalt, the origin of magma origin ranged ± 140 Km - ± 185 Km in the Benioff zone and formed at temperatures of 1016 ̊ – 1062 ̊ C with rock specific gravity of 2.82 - 2.89 gram / cm3.
Co-Authors Abdul Aziz Achmad Yusuf Agung Firmansyah, Rico AHMAD FAISOL Aini, Hana Nur Amali, Adityal Chisabul Amitama, Emilia Bunga Anggraini, Friska Apriyani, Mirna Ariwibisono, FX Bambang Sugiantoro Bin Wallang, Muslimin Dedy Afrizal Denny Vitasari Dewa, Chandra Kusuma Dhomas Hatta Fudholi diana, ros Didik Sudyana Dila Erlianti Ekareesakul, Kittipan Eko Yuli Handoko Erinaldi, Erinaldi Fachrudin, Kurnia Arfiansyah Fawzan, Ihsan fFaizal, Arif Fiasari, Sinta Nur Hafrida, Lis Halim, Muhammad Yusuf Hananfajri, Muhammad Hardika Dwi Hermawan Hijeriah, E. Maznah Hildawati Hildawati, Hildawati I Made Arie Widyasthana Wartana Putra Ildrem Syafri Imam Riadi Indriasari, Ratna Kasnelly, Sri Khair, Otti Ilham Kholid Haryono Kurniawan, Andang Kusuma Dewa, Chandra Latif Syaipudin Lian Agustina Setiyaningsih M. Said Marisa Permatasari, Marisa Maulana, Bagus Andrai Mawarni, Dinda Iga Meutia, Adinda Muhammad, Aldila Syariz Munawwaroh, Nasywa Zunaibatul Munjayyanah, Munjayyanah Mustikarini, Monika Grace Nilma, Nilma Nur Widiyasono, Nur Nurhalisa, Sabrina Nuril Anwar, Nuril Pakkaja, Ryan Alghazali Paputungan, Irving Vitra Poespitohadi, Wibisono Pratama, Syahrul Pravitasari, Norma Prayoga, Diki Priwibowo, Aqge Purnamasari, Rika Afriyanti Putra, I Made Arie Widyasthana Wartana Ramadani, Erika Ramadiniyati, Suci Rika Handayani Rike Nursafitri Rizky Achmad Almayda Almayda Rosa, Nauviana Pita Salwa, Nikmatus Shaleha, Annisa Amalia Sopaheluwakan, Ardhasena Sri Widayati Sumarni Sumarni Suroningsih Suroningsih, Suroningsih susi susi Tuharea, Ibnu Rohan Wahyuzi, Zikri Widarta, Agung Eka Yosika, Diana Rosa Yudi prayudi Zainul’ID, Ahmad Bagus Zubizaretta, Zaid Dzulkarnain