Geological structure identification in geothermal manifestation of Lamongan Volcano Complex: A magnetic data analysis approach

The Tiris area in the Lamongan Volcano Complex, Probolinggo, East Java, is estimated to be an area with geothermal potential in Indonesia. This is indicated by the existence of several hot springs along the Tancak River, forming a continuous line with a distance about 20-50 m between each h...

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Main Authors: Ulumuddin Faqih, Fajar Miftakhul Haris M., Warnana Dwa Desa, Rafi Muhammad Erfand Dzulfiqar, Rahayu K Helda usuma
Format: Article
Language:English
Published: Faculty of Mining and Geology, Belgrade 2024-01-01
Series:Geološki Anali Balkanskoga Poluostrva
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Online Access:https://doiserbia.nb.rs/img/doi/0350-0608/2024/0350-06082400013U.pdf
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author Ulumuddin Faqih
Fajar Miftakhul Haris M.
Warnana Dwa Desa
Rafi Muhammad Erfand Dzulfiqar
Rahayu K Helda usuma
author_facet Ulumuddin Faqih
Fajar Miftakhul Haris M.
Warnana Dwa Desa
Rafi Muhammad Erfand Dzulfiqar
Rahayu K Helda usuma
author_sort Ulumuddin Faqih
collection DOAJ
description The Tiris area in the Lamongan Volcano Complex, Probolinggo, East Java, is estimated to be an area with geothermal potential in Indonesia. This is indicated by the existence of several hot springs along the Tancak River, forming a continuous line with a distance about 20-50 m between each hot spring. Segaran hot springs are one of the hydrothermal manifestations that can indicate the presence of geothermal potential in this location. Some previous research has shown the existence of subsurface geological structures around Segaran hot springs in a northwest-southeast direction. However, the identification of geo - thermal manifestations in this location is limited, so magnetic data can help identify subsurface geological structures to confirm the geo thermal potential in this area. A significant contrast in horizontal magnetic anomalies indicates the existence of subsurface geological structures. To delineate the boundaries of the magnetic anomaly, the first horizontal derivative and second vertical derivative were applied. To determine the depth of the magnetic anomaly, located Euler deconvolution was used. The integration of these three transformations on the magnetic data is sufficient to interpret the position, direction, and depth of subsurface structures in the research area. The results show the position of dominant lineament in the Lamongan Volcano Complex through Segaran hot springs is a northwest-southeast orientation. These results align with the dominant orientation from the density lineaments analysis performed based on the Digital Elevation Model Nasional (DEMNAS). Building from previous research, the existence of fault structures correlated with Segaranhot springs can improve the indication of geothermal potential in the Lamongan Volcano Complex, especially in the Tiris area.
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institution Kabale University
issn 0350-0608
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language English
publishDate 2024-01-01
publisher Faculty of Mining and Geology, Belgrade
record_format Article
series Geološki Anali Balkanskoga Poluostrva
spelling doaj-art-c2e64df7787140b9b9ae3c2f1458323f2025-01-30T06:45:17ZengFaculty of Mining and Geology, BelgradeGeološki Anali Balkanskoga Poluostrva0350-06082406-07472024-01-01852657810.2298/GABP240321013U0350-06082400013UGeological structure identification in geothermal manifestation of Lamongan Volcano Complex: A magnetic data analysis approachUlumuddin Faqih0https://orcid.org/0009-0005-8687-6402Fajar Miftakhul Haris M.1https://orcid.org/0009-0001-8043-9261Warnana Dwa Desa2https://orcid.org/0000-0001-6145-0265Rafi Muhammad Erfand Dzulfiqar3https://orcid.org/0009-0003-6716-0084Rahayu K Helda usuma4https://orcid.org/0009-0006-8655-5366Geophysical Engineering Department, Sepuluh Nopember Institute of Technology, Surabaya, IndonesiaGeophysical Engineering Department, Sepuluh Nopember Institute of Technology, Surabaya, IndonesiaGeophysical Engineering Department, Sepuluh Nopember Institute of Technology, Surabaya, IndonesiaGeophysical Engineering Department, Sepuluh Nopember Institute of Technology, Surabaya, IndonesiaGeophysical Engineering Department, Sepuluh Nopember Institute of Technology, Surabaya, IndonesiaThe Tiris area in the Lamongan Volcano Complex, Probolinggo, East Java, is estimated to be an area with geothermal potential in Indonesia. This is indicated by the existence of several hot springs along the Tancak River, forming a continuous line with a distance about 20-50 m between each hot spring. Segaran hot springs are one of the hydrothermal manifestations that can indicate the presence of geothermal potential in this location. Some previous research has shown the existence of subsurface geological structures around Segaran hot springs in a northwest-southeast direction. However, the identification of geo - thermal manifestations in this location is limited, so magnetic data can help identify subsurface geological structures to confirm the geo thermal potential in this area. A significant contrast in horizontal magnetic anomalies indicates the existence of subsurface geological structures. To delineate the boundaries of the magnetic anomaly, the first horizontal derivative and second vertical derivative were applied. To determine the depth of the magnetic anomaly, located Euler deconvolution was used. The integration of these three transformations on the magnetic data is sufficient to interpret the position, direction, and depth of subsurface structures in the research area. The results show the position of dominant lineament in the Lamongan Volcano Complex through Segaran hot springs is a northwest-southeast orientation. These results align with the dominant orientation from the density lineaments analysis performed based on the Digital Elevation Model Nasional (DEMNAS). Building from previous research, the existence of fault structures correlated with Segaranhot springs can improve the indication of geothermal potential in the Lamongan Volcano Complex, especially in the Tiris area.https://doiserbia.nb.rs/img/doi/0350-0608/2024/0350-06082400013U.pdfderivative analysiseuler deconvolutionfault structuresegaran hot springseast java
spellingShingle Ulumuddin Faqih
Fajar Miftakhul Haris M.
Warnana Dwa Desa
Rafi Muhammad Erfand Dzulfiqar
Rahayu K Helda usuma
Geological structure identification in geothermal manifestation of Lamongan Volcano Complex: A magnetic data analysis approach
Geološki Anali Balkanskoga Poluostrva
derivative analysis
euler deconvolution
fault structure
segaran hot springs
east java
title Geological structure identification in geothermal manifestation of Lamongan Volcano Complex: A magnetic data analysis approach
title_full Geological structure identification in geothermal manifestation of Lamongan Volcano Complex: A magnetic data analysis approach
title_fullStr Geological structure identification in geothermal manifestation of Lamongan Volcano Complex: A magnetic data analysis approach
title_full_unstemmed Geological structure identification in geothermal manifestation of Lamongan Volcano Complex: A magnetic data analysis approach
title_short Geological structure identification in geothermal manifestation of Lamongan Volcano Complex: A magnetic data analysis approach
title_sort geological structure identification in geothermal manifestation of lamongan volcano complex a magnetic data analysis approach
topic derivative analysis
euler deconvolution
fault structure
segaran hot springs
east java
url https://doiserbia.nb.rs/img/doi/0350-0608/2024/0350-06082400013U.pdf
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AT warnanadwadesa geologicalstructureidentificationingeothermalmanifestationoflamonganvolcanocomplexamagneticdataanalysisapproach
AT rafimuhammaderfanddzulfiqar geologicalstructureidentificationingeothermalmanifestationoflamonganvolcanocomplexamagneticdataanalysisapproach
AT rahayukheldausuma geologicalstructureidentificationingeothermalmanifestationoflamonganvolcanocomplexamagneticdataanalysisapproach