1Geological Museum, Geological Agency, Ministry of Energy and Mineral Resources, Jl. Diponegoro 57, Bandung, 40122, Indonesia
2Departement of Geological Engineering, Faculty of Engineering, Universitas Diponegoro, Jl. Prof. Soedarto S.H., Tembalang, Semarang, Indonesia, Indonesia
BibTex Citation Data :
@article{JGT17582, author = {Agustina Djafar and Ifan Suharyogi and Rahajeng Sari and Anita Jayanti and Andhy Sipayung and Indyo Pratomo}, title = {SOUTHERN TASIKMALAYA ANCIENT SUBMARINE VOLCANO: VESTIGES OF ERUPTIONS AND THEIR DIVERSITY AS GEOLOGICAL HERITAGE}, journal = {Jurnal Geosains dan Teknologi}, volume = {6}, number = {2}, year = {2023}, keywords = {basaltic andesite lava; geological heritage; jasper; peperite; southern Tasikmalaya; submarine volcano}, abstract = {In the southern Tasikmalaya area West Java Province, Indonesia, there are Tertiary volcanic rocks, with an east-west trending distribution pattern. Physiographically, this area is included in the southern mountain zone of West Java and is generally composed of tuff and polymic breccias with intercalated of lava and limestone which are grouped into the Jampang Formation and Genteng Members Jampang Formation. The existence of these volcanic and sedimentary rocks of Oligocene – Middle Miocene in the area is an indication of submarine volcano. The purpose of this paper to identify traces of eruptions and submarine volcano products found in the southern Tasikmalaya area, for further assessment of the geological diversity potential as a geological heritage. The method used are field data collection and quantitative data analysis, namely identification of geological heritage based on \"Technical Guidelines for the Assessment of Geological Heritage Resources\". The submarine volcano products which found in this area are peperite, and basaltic andesite lava at Karang Tawulan Beach, traces of alteration, and hydrothermal mineralization like jasper Panca Tengah, and Cipatujah volcanogenic massive sulphide. This shows that volcanic activities in the southern Tasikmalaya took place continuously from Oligocene to Middle Miocene. From the results of the assessment, the geological diversity in this area has a scientific value of \"medium-high\".}, issn = {2620-634X}, pages = {64--72} doi = {10.14710/jgt.6.2.2023.64-72}, url = {https://ejournal2.undip.ac.id/index.php/jgt/article/view/17582} }
Refworks Citation Data :
Article Metrics:
Last update:
The Authors submitting a manuscript do so on the understanding that if accepted for publication, copyright of the article shall be assigned to Jurnal Geosains dan Teknologi and Department of Geological Engineering, Universitas Diponegoro as the publisher of the journal. Copyright encompasses rights to reproduce and deliver the article in all form and media, including reprints, photographs, microfilms, and any other similar reproductions, as well as translations.
Jurnal Geosains dan Teknologi and Department of Geological Engineering, Universitas Diponegoro and the Editors make every effort to ensure that no wrong or misleading data, opinions or statements be published in the journal. In any way, the contents of the articles and advertisements published in Jurnal Geosains dan Teknologi are the sole and exclusive responsibility of their respective authors and advertisers.
The Copyright is officially transfered when the Author has filled and signed the License of Agreement, please do download the file here. The License of Agreement should be signed originally and send to the Editorial Office in the form of original mail or scanned document to :
Dr.rer.nat Thomas Triadi Putranto (Editor-in-Chief)Editorial Office of Jurnal Geosains dan TeknologiGeological Engineering Department, Universitas DiponegoroJl. Prof. Soedarto, Kampus Undip Tembalang, Semarang, Central Java, Indonesia 50275Email: jgt@live.undip.ac.id