A APPLICATION OF LINEAMENT DENSITY AND GRAVITY METHODS TO DETECTING FRACTURE AND FAULT LANE IN THE TAMPUSU VOLCANIC FIELD (NORTH SULAWESI, INDONESIA)
Main Article Content
Abstract
Tampusu Mountain (± 1500 m above sea level) is located between two famous geological tourism areas in North Sulawesi, namely Lake Linow and Lake Tondano. The position of Mount Tampusu, as well as the presence of geothermal manifestations in the surrounding area is interesting to study its geological aspects both on the surface and below the surface. This study aims to determine the existence of surface geological structures based on line density, and also to determine the presence and direction of subsurface geological structures based on gravity anomaly data in Tampusu Volcanic area. The fault and fracture density method is used to map the surface geological structure, while the gravity method is used to obtain information about the geological structure of the Tampusu volcanic area between the crater of Lake Linow and the Lake Tondano caldera. The existence of a fault is known to be west of the Lake Tondano caldera which is an extension from east to southeast of the Linow Lake crater. There is a relationship between the distribution map of the bouguer anomaly value and the map of lineament density along the Lake Linow crater to Lake Tondano caldera.
Article Details
Section
References
Abraham, E. M., & Alile, O. M. (2019). Journal of Geophysics and Engineering. Modelling subsurface geologic structures at the Ikogosi geothermal field, southwesterm Nigeria, using gravity, magnetics and seismic interferometry techniques , 729-741.
Andrianaivo, L., & Ramasiariarinoro, V. J. (2010). Relation between Regional Lineament Systems and Geological Structures: Implications for Understanding Structural Controls of Geothermal System in the Volcanic Area of Itasy, Madagascar. World Geothermal Congress 2010. Bali: Université d’Antananarivo.
Atef, H., El-Gawad, A. A., Zaher, M. A., & Farrag, K. (2016). The Contribution of Gravity Method in Geothermal Exploration of Southern Part of the Gulf of Suez-Sinai region, Egypt. National Research Institute of Astronomy and Geophysics NRIAG.
Aziz, K. N., Hartantyo, E., & Niasari, S. W. (2018). The Study of Fault Lineament Pattern of the Lamongan Volcanic Field Using Gravity Data. The International Conference on Theoretical and Applied Physics , 1-5.
Bujung, C. A. (2011). Identifikasi Prospek Panas Bumi Berdasarkan Fault and Fracture Density (FFD) Studi kasus Gunung Patuha, Jawa Barat. Jurnal Lingkungan dan Bencana Geologi, Vol 2 No.1 , 67 - 75.
Hasanah, L., Aminudin, A., Ardi, N. D., Utomo, A. S., Yuwono, H., Kamtono, et al. (2016). International Symposium on Geophysical Issues. Graben Structure Identification Using Gravity Method .
Imam Raharjo, E. S. (2009). “Quick and Dirty” 3-D Gravity Inversion, a case study in Lahendong and its vicinity. Geothermal Pertamina .
Kipkemoi, L. G. (2013). Gravity Survey For Geothermal Exploration in Menengai Area, Kenya. Nairobi: Kenyatta University.
Saepuloh, A., Haeruddin, H., Heriawan, M. N., Kubo, T., Koeike, K., & Malik, D. (2018). Geothermics 72. Application of lineament density extracted from dual orbit of synthetic aperture radar (SAR) images to detecting fluids paths in the Wayang Windu geothermal field (West Java, Indonesia) , 145-155.
Siahaan, E. E., Soemarinda, S., Fauzi, A., Silitonga, T., Azimudin, T., & Raharjo, I. B. (2005). Proceedings World Geothermal Congress 2005. Tectonism and Volcanism Study in the Minahasa Compartment of the North Arm of .
Andrianaivo, L., & Ramasiariarinoro, V. J. (2010). Relation between Regional Lineament Systems and Geological Structures: Implications for Understanding Structural Controls of Geothermal System in the Volcanic Area of Itasy, Madagascar. World Geothermal Congress 2010. Bali: Université d’Antananarivo.
Atef, H., El-Gawad, A. A., Zaher, M. A., & Farrag, K. (2016). The Contribution of Gravity Method in Geothermal Exploration of Southern Part of the Gulf of Suez-Sinai region, Egypt. National Research Institute of Astronomy and Geophysics NRIAG.
Aziz, K. N., Hartantyo, E., & Niasari, S. W. (2018). The Study of Fault Lineament Pattern of the Lamongan Volcanic Field Using Gravity Data. The International Conference on Theoretical and Applied Physics , 1-5.
Bujung, C. A. (2011). Identifikasi Prospek Panas Bumi Berdasarkan Fault and Fracture Density (FFD) Studi kasus Gunung Patuha, Jawa Barat. Jurnal Lingkungan dan Bencana Geologi, Vol 2 No.1 , 67 - 75.
Hasanah, L., Aminudin, A., Ardi, N. D., Utomo, A. S., Yuwono, H., Kamtono, et al. (2016). International Symposium on Geophysical Issues. Graben Structure Identification Using Gravity Method .
Imam Raharjo, E. S. (2009). “Quick and Dirty” 3-D Gravity Inversion, a case study in Lahendong and its vicinity. Geothermal Pertamina .
Kipkemoi, L. G. (2013). Gravity Survey For Geothermal Exploration in Menengai Area, Kenya. Nairobi: Kenyatta University.
Saepuloh, A., Haeruddin, H., Heriawan, M. N., Kubo, T., Koeike, K., & Malik, D. (2018). Geothermics 72. Application of lineament density extracted from dual orbit of synthetic aperture radar (SAR) images to detecting fluids paths in the Wayang Windu geothermal field (West Java, Indonesia) , 145-155.
Siahaan, E. E., Soemarinda, S., Fauzi, A., Silitonga, T., Azimudin, T., & Raharjo, I. B. (2005). Proceedings World Geothermal Congress 2005. Tectonism and Volcanism Study in the Minahasa Compartment of the North Arm of .