Utilization and modeling of satellite gravity data for geohazard assessment in the Yogyakarta area of Java']Java Island, Indonesia

被引:1
|
作者
Pohan, Ahmad F. [1 ]
Sismanto, Sismanto [2 ]
Nurcahya, Budi E. [2 ]
Lewerissa, Richard [3 ]
Koesuma, Sorja [4 ]
Saputro, Sugeng P. [5 ]
Amukti, Rian [6 ]
Saputra, Hijrah [7 ]
Adhi, Mochamad A. [8 ]
机构
[1] Andalas Univ, Fac Math & Sci, Dept Phys, Jl Univ Andalas Limau Manis Pauh, Padang 25163, Indonesia
[2] Univ Gadjah Mada, Fac Math & Nat Sci, Dept Phys, Yogyakarta 55281, Indonesia
[3] Papua Univ, Fac Math & Nat Sci, Dept Phys, Manokwari 98314, Papua Barat, Indonesia
[4] Sebelas Maret Univ, Fac Math & Nat Sci, Dept Phys, Surakarta, Indonesia
[5] Natl Res & Innovat Agcy BRIN, Res Ctr Geol Resources, Bogor, Indonesia
[6] Natl Res & Innovat Agcy BRIN, Ctr Geol Disaster, Bogor, Indonesia
[7] Univ Airlangga, Postgrad Sch, Master Program Disaster Management, Surabaya, Indonesia
[8] Semarang State Univ, Fac Math & Nat Sci, Dept Phys, Semarang, Indonesia
关键词
Aerotropolis; Geohazard assessment; Inversion modeling; Opak fault; Merapi volcano; 3-D INVERSION;
D O I
10.1016/j.kjs.2023.05.016
中图分类号
O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];
学科分类号
07 ; 0710 ; 09 ;
摘要
A geohazard assessment was conducted in the Aerotropolis area of the new Yogyakarta international airport, located in the Yogyakarta special region province, Indonesia. The study involved the analysis and modeling of 3-D inversions of earth gravity anomaly data obtained from the high-resolution of Global Gravity Model (GGM). The main objective of the study was to identify subsurface geological structures such as faults, active volcanoes, and sedimentary layers that may pose potential hazards to the Yogyakarta aerotropolis area. The complete Bouguer anomaly in the study region was calculated using modern terrain correction methods that relied on full-scale topography gravity data from the SRTM2gravity model. A 2-D radial spectrum analysis was then performed on this anomaly data, which revealed that the average thickness of sedimentary layers was estimated to be more than 100 m. The rock density contrast was determined using the residual gravity anomaly inversion, which showed a range of-0.086 g/cm3 to 0.043 g/cm3. The analysis of gravity anomalies and rock density contrast provided results that aligned with the regional geological conditions of the Yogyakarta region, including the pattern of igneous rock intrusion with high density contrast, the presence of the Merapi magma chambers associated with low negative density contrast, and the Opak normal fault path at low and high contrast boundaries, which could lead to natural hazards in the region.
引用
收藏
页码:499 / 511
页数:13
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