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All Journal Jurnal Pengelolaan Sumberdaya Alam dan Lingkungan (Journal of Natural Resources and Environmental Management) Journal of Applied Geospatial Information JRST (Jurnal Riset Sains dan Teknologi) SELAPARANG: Jurnal Pengabdian Masyarakat Berkemajuan Jurnal GEOSAPTA Jambura Geoscience Review Geodika: Jurnal Kajian Ilmu dan Pendidikan Geografi Jurnal Sibermas (Sinergi Pemberdayaan Masyarakat) Lamahu: Jurnal Pengabdian Masyarakat Terintegrasi Journal of Earth Energy Science, Engineering, and Technology Panrita Inovasi: Jurnal Pengabdian Kepada Masyarakat Geographica: Science and Education Journal
Muh Kasim
Universiitas Negeri Gorontalo
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Diagenesis Analysis of Padengo Limestone Area, Gorontalo Regency Based on Petrographic Method Fikri Boften; Aang Panji Permana; Muhammmad Kasim
Journal of Applied Geospatial Information Vol 7 No 2 (2023): Journal of Applied Geospatial Information (JAGI)
Publisher : Politeknik Negeri Batam

Show Abstract | Download Original | Original Source | Check in Google Scholar | DOI: 10.30871/jagi.v7i2.5074

Abstract

Carbonate rocks are rocks composed of carbonate minerals that are chemically formed in the form of solutions, and there are organisms involved in their formation. The limestone found around Lake Limboto is very interesting, because the water in the lake is freshwater while the limestone is characteristic of a marine environment. Diagenesis is a natural process in sedimentary rocks that occurs from the initial deposition until it reaches the limit of metamorphism will be formed. The research area is located in Padengo Village, West Limboto Subdistrict, Gorontalo Regency with a research area of 7.72 Km2. This research aims to analyze the diagenesis of limestone in the Padengo area of Gorontalo Regency using the petrographic method. The methods used are field geological survey and petrographic analysis. The results showed that the geology of the Padengo area is composed of a wackestone limestone facies unit, a crystalline limestone facies unit, and an alluvial sediment unit. The diagenesis type of the study area consists of neomorphism, micritization, dissolution, cementation, and dolomitization. From the type of diagenesis, it can be determined that the limestone diagenesis environment of the study area starts from the marine phreatic zone, then the burial zone, and ends at the meteoric vadose zone.
Co-Authors Abd. Rahman Maloho Aditya Prasetyo Mangkat Ahmad Iryanto Rompo Ahmad Zainuri Akbar, La Ode Juni Anggun Farwati M Abdullah Aulia Fitrah Ramadhani Daud Yusuf Delta Jexica Sianturi Destira Handayani Eksan Fajri Kurniawan Mamonto Fikri Boften Fitrianingsih Antula Fitryane Lihawa Irene Ester Wowiling Irmawati Irmawati Joni Djakun M. Iqbal Liayong Pratama Moh. Nazer Ismail Mohamad Adrian Saputra Mohamad Dio Pangulu Mohammad Noorhidayat Baruadi Muhlis Ali Mutiara Nonsi Nani Mardiani Noviar Akase Nurfaika Nurfaika Nurmuhniyanti M. Hubaib Permana, Aang Panji Rachmat Ramadhan Nur Syamsuri Rahmia Rahman Riski I. Pidu Ronal Hutagalung Siti Chusnul Chatimah Nurrahmah Sri Maryati Sutriyono sutriyono Umar Zulkarnain Bakkar Widya Candra Mooduto