Jurnal Geologi dan Sumberdaya Mineral
https://jgsm.geologi.esdm.go.id/index.php/JGSM
<p><strong>Jurnal Geologi dan Sumberdaya Mineral (Journal of Geology and Mineral Resources)</strong> is an Indonesian scientific journal published by the Center for Geological Survey, Geological Agency, Ministry of Energy and Mineral Resources. The journal receives Indonesian or English articles. Those articles are selected and reviewed by our professional editors and peer reviewers.</p> <p>JGSM has been assigned as an Accredited Scientific Periodical Magazine by the Indonesian Institute of Sciences (LIPI) No. 596/Akred/P2MI-LIPI/03/2015 in 2015, followed by Kementerian Riset dan Teknologi / Badan Riset dan Inovasi Nasional No. 200/M/KPT/2020 in 2020. The journal is indexed in <a title="portal_garuda_IPI" href="http://id.portalgaruda.org/?ref=browse&mod=viewjournal&journal=10104" target="_blank" rel="noopener">Indonesian Publication Index (IPI)</a>, <a title="isjd" href="http://isjd.pdii.lipi.go.id/index.php/public_no_login/index_direktori" target="_blank" rel="noopener">Indonesian Scientific Journal Database (ISJD)</a>, <a href="http://dx.doi.org/10.33332">Digital Object Identifier (DOI)</a> and <a title="google_scholar" href="https://scholar.google.co.id/citations?user=nXMHIYUAAAAJ&hl=en" target="_blank" rel="noopener">Google Scholar</a>, the contents are freely available in electronic version. JGSM is published quarterly in February, May, August, and November.</p> <p><a title="issn" href="http://issn.pdii.lipi.go.id/issn.cgi?daftar&1402376294&1&&" target="_blank" rel="noopener"><strong>ISSN : 0853-9634 (print)</strong></a></p> <p><a title="eissn" href="http://issn.pdii.lipi.go.id/issn.cgi?daftar&1485227549&1&&" target="_blank" rel="noopener"><strong>e-ISSN : 2549-4759 (online)</strong></a></p> <p><strong><em><strong>DOI Prefix: </strong></em><a title="JGSM" href="https://doi.org/10.33332">https://doi.org/10.33332</a><br /></strong></p>
Pusat Survei Geologi
en-US
Jurnal Geologi dan Sumberdaya Mineral
0853-9634
<p>Authors who publish articles in <strong>Jurnal Geologi dan Sumberdaya Mineral (JGSM.Geologi)</strong> agree to the following terms:</p><ol><li>Authors retain copyright of the article and grant the journal right of first publication with the work simultaneously licensed under a <strong>CC-BY-NC</strong> or <strong>The Creative Commons Attribution–ShareAlike License.</strong></li><li>Authors are able to enter into separate, additional contractual arrangements for the non-exclusive distribution of the journal's published version of the work (e.g., post it to an institutional repository or publish it in a book), with an acknowledgment of its initial publication in this journal.</li><li>Authors are permitted and encouraged to post their work online (e.g., in institutional repositories or on their website) prior to and during the submission process, as it can lead to productive exchanges, as well as earlier and greater citation of published work (See <a href="http://opcit.eprints.org/oacitation-biblio.html" target="_blank">The Effect of Open Access</a>)</li></ol>
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Karakteristik Jenis dan Geokimia Batugamping Formasi Wapulaka untuk Bahan Baku Industri di Kecamatan Sampolawa, Kabupaten Buton Selatan, Provinsi Sulawesi Tenggara
https://jgsm.geologi.esdm.go.id/index.php/JGSM/article/view/857
<p>© JGSM. This is an open access article<br />under the CC-BY-NC license (https://creativecommons.org/licenses/by-nc/4.0/)<br />Jurnal Geologi dan Sumberdaya Mineral Vol. 26 No. 2 Mei 2025 hal. 77-85<br />Abstrak- Daerah Buton Selatan memiliki prospek bahan<br />galian batugamping yang cukup besar, hal ini ditunjukan<br />dari peta geologi lembar Buton bahwa daerah Buton<br />Selatan terdapat Formasi Wapulaka yang merupakan<br />formasi batugamping selain itu beberapa lokasi di Buton<br />Selatan terdapat penambangan batugamping yang belum<br />berkembang aktif. Penambangan batugamping masih<br />membutuhkan data-data eksplorasi dan pengembangan<br />infrastruktur di daerah tersebut. Oleh karena itu data tentang<br />potensi batugamping di Buton Selatan perlu ditingkatkan<br />untuk mendukung kebutuhan pemerintah dan masyarakat.<br />Daerah penelitian berada di Kecamatan Sampolawa,<br />Kabupaten Buton Selatan, Provinsi Sulawesi Selatan.<br />Penelitian ini bertujuan untuk mengetahui karakteristik<br />jenis dan geokimia batugamping formasi Wapulaka sebagai<br />acuan karakteristik batugamping untuk bahan baku industri.<br />Karakteristik jenis batugamping di daerah penelitian terdiri<br />dari jenis wackestone dan jenis packstone. Jenis yang<br />berkembang di daerah penelitian terdiri grain: bioklas, mud:<br />kalsit, pure: vug dan channel. Berdasarkan analisis geokimia<br />batugamping di daerah penelitian memiliki Kandungan<br />CaO hingga 99%, hal ini dipengaruhi oleh adanya cangkang-<br />cangkang atau fosil pada batugamping. Karakteristik fasies<br />dan geokimia menunjukan karakteristik batugamping yang<br />akan digunakan sebagai bahan baku industri seperti: semen,<br />bahan bangunan, industri peleburan dan pemurnian baja.</p>
Citra Aulian Chalik
Rezki Reyditha Januar
Mubdiana Arifin
Copyright (c) 2025 Citra Aulian Chalik, Rezki Reyditha Januar, Mubdiana Arifin
http://creativecommons.org/licenses/by-nc/4.0
2025-06-23
2025-06-23
26 2
77
85
10.33332/jgsm.geologi.v16i2.857
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Identifikasi Karakteristik Erupsi Gunung Patuha Berdasarkan Stratigrafi Batuan di Kawah Putih Ciwidey
https://jgsm.geologi.esdm.go.id/index.php/JGSM/article/view/964
<p>Gunung Patuha terletak di Jawa Barat dan<br />memiliki kondisi tektonik yang dipengaruhi oleh aktivitas<br />subduksi di bagian selatan Pulau Jawa. Aktivitas vulkanik<br />yang menghasilkan berbagai jenis batuan, termasuk tuf,<br />lapili, breksi vulkanik, skoria, dan aglomerat. Penelitian<br />ini bertujuan untuk mengidentifikasi karakteristik erupsi<br />Gunung Patuha berdasarkan analisis stratigrafi batuan<br />di Kawah Putih. Metode yang digunakan adalah metode<br />deskriptif kualitatif, dengan data primer diperoleh melalui<br />observasi lapangan dan wawancara, serta data sekunder dari<br />studi literatur. Hasil penelitian menunjukkan bahwa kawasan<br />ini mencerminkan dinamika vulkanisme yang kompleks,<br />dengan berbagai fase erupsi, dari eksplosif hingga efusif.<br />Batuan tuf dan lapili mengindikasikan erupsi eksplosif<br />yang berulang, sementara keberadaan skoria dan aglomerat<br />mencerminkan aktivitas efusif dengan pelepasan gas yang<br />signifikan. Namun, erupsi Gunung Patuha belum mencapai<br />intensitas erupsi Plinian, sebagaimana ditunjukkan oleh<br />tidak adanya deposit pumis yang signifikan dan distribusi<br />material yang cenderung lokal. Penelitian ini diharapkan<br />dapat memberikan pemahaman mendalam tentang proses<br />vulkanisme Gunung Patuha. Temuan ini juga diharapkan<br />dapat berkontribusi pada upaya mitigasi bencana vulkanik<br />di kawasan tersebut.</p> <p><strong>Kata kunci:</strong> Gunung Patuha, stratigrafi, vulkanisme, erupsi.</p> <p> </p> <p><strong><em>Abstract</em></strong></p> <p><em>Mount Patuha is located in West Java and has</em><br /><em>tectonic conditions influenced by subduction activity in the</em><br /><em>southern part of Java Island. Volcanic activity produced a</em><br /><em>variety of rock types, including tuff, lapilli, volcanic breccia,</em><br /><em>scoria, and agglomerate. This research aims to identify the</em><br /><em>eruption characteristics of Mount Patuha based on the</em><br /><em>analysis of rock stratigraphy in Kawah Putih. The method</em><br /><em>used is a descriptive qualitative method, with primary data</em><br /><em>obtained through field observations and interviews, and</em><br /><em>secondary data from literature studies. The results showed</em><br /><em>that the area reflects complex volcanism dynamics, with</em><br /><em>various eruption phases, from explosive to effusive. Tuff and</em><br /><em>lapilli rocks indicate repeated explosive eruptions, while</em><br /><em>the presence of scoria and agglomerate reflects effusive</em><br /><em>activity with significant gas release. However, the eruption</em><br /><em>of Mount Patuha has not reached the intensity of a Plinian</em><br /><em>eruption, as indicated by the absence of significant pumice</em><br /><em>deposits and the localized distribution of materials. This</em><br /><em>research is expected to provide an in-depth understanding</em><br /><em>of the volcanism process of Mount Patuha. The findings are</em><br /><em>also expected to contribute to volcanic disaster mitigation</em><br /><em>efforts in the region.</em></p> <p><em><strong>Keywords:</strong> Mount Patuha, stratigraphy, volcanism,</em><br /><em>eruption.</em></p>
Kurnia Maulidi Noviantoro
Dwi Novitasari
Ayu Firnanda
Agung Dwi Firmansyah
Ahmad Wildan Nanda Febry
Faiza Amalia
Fir Atiyatul Mu’awwanah
Wahyu Susanti
Devia Liza Rahmadani
Copyright (c) 2025 Kurnia Maulidi Noviantoro, Dwi Novitasari, Ayu Firnanda, Agung Dwi Firmansyah, Ahmad Wildan Nanda Febry, Faiza Amalia, Fir Atiyatul Mu’awwanah, Wahyu Susanti, Devia Liza Rahmadani
http://creativecommons.org/licenses/by-nc/4.0
2025-06-23
2025-06-23
26 2
87
96
10.33332/jgsm.geologi.v26i2.964