Modeling Kaligarang fault base on gravity data 2020
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F67985530%3A_____%2F23%3A00574231" target="_blank" >RIV/67985530:_____/23:00574231 - isvavai.cz</a>
Výsledek na webu
<a href="https://pubs.aip.org/aip/acp/article-abstract/2738/1/030037/2894312/Modeling-Kaligarang-fault-based-on-gravity-data?redirectedFrom=PDF" target="_blank" >https://pubs.aip.org/aip/acp/article-abstract/2738/1/030037/2894312/Modeling-Kaligarang-fault-based-on-gravity-data?redirectedFrom=PDF</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1063/5.0140955" target="_blank" >10.1063/5.0140955</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
Modeling Kaligarang fault base on gravity data 2020
Popis výsledku v původním jazyce
The Kaligarang river in Semarang City flows from south to north. Kaligarang river divides Semarang city to be 2 regions. Kaligarang river was formed by the Kaligarang fault. Kaligarang Fault is an active fault that divides young rock in the south of Semarang City to the Java Sea. The activity of fault can trigger earthquakes. Semarang is a crowded city that causes a lot of human activity so the possibility of an earthquake due to fault activity in the future needs to be studied. The research objective is to describe mass distribution beneath Semarang using new gravity data in 2020. The gravity data is 50 data, which focus around the Kaligarang area from south to north. The processing used basic calculation and correction in gravity as latitude, Bouguer, and terrain. The average density was 2.4 g/cc. The inverse modeling in 3-dimensional used Grablox. The research results are a density model beneath Semarang city. The modeling described a fault model beneath The Kaligarang area. The direction of the fault layer is on the north-south and east-west. The density distribution is 2 - 2.85 g/cc. The rock layers are clay and sand rocks above the breccia, lava, and andesite rocks. The density distribution indicates a basin in the central area of the research area to the west and south. the South-West part of the research area has a maximum density. The maximum density on the center area also indicates two faults. The Kaligarang fault is a transform fault. The Kaligarang fault has a South-North direction and turns to the north-west. Gombel fault (east-west normal Fault) become cut and shift to the north.
Název v anglickém jazyce
Modeling Kaligarang fault base on gravity data 2020
Popis výsledku anglicky
The Kaligarang river in Semarang City flows from south to north. Kaligarang river divides Semarang city to be 2 regions. Kaligarang river was formed by the Kaligarang fault. Kaligarang Fault is an active fault that divides young rock in the south of Semarang City to the Java Sea. The activity of fault can trigger earthquakes. Semarang is a crowded city that causes a lot of human activity so the possibility of an earthquake due to fault activity in the future needs to be studied. The research objective is to describe mass distribution beneath Semarang using new gravity data in 2020. The gravity data is 50 data, which focus around the Kaligarang area from south to north. The processing used basic calculation and correction in gravity as latitude, Bouguer, and terrain. The average density was 2.4 g/cc. The inverse modeling in 3-dimensional used Grablox. The research results are a density model beneath Semarang city. The modeling described a fault model beneath The Kaligarang area. The direction of the fault layer is on the north-south and east-west. The density distribution is 2 - 2.85 g/cc. The rock layers are clay and sand rocks above the breccia, lava, and andesite rocks. The density distribution indicates a basin in the central area of the research area to the west and south. the South-West part of the research area has a maximum density. The maximum density on the center area also indicates two faults. The Kaligarang fault is a transform fault. The Kaligarang fault has a South-North direction and turns to the north-west. Gombel fault (east-west normal Fault) become cut and shift to the north.
Klasifikace
Druh
D - Stať ve sborníku
CEP obor
—
OECD FORD obor
10508 - Physical geography
Návaznosti výsledku
Projekt
—
Návaznosti
I - Institucionalni podpora na dlouhodoby koncepcni rozvoj vyzkumne organizace
Ostatní
Rok uplatnění
2023
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název statě ve sborníku
AIP Conference Proceedings
ISBN
—
ISSN
0094-243X
e-ISSN
1551-7616
Počet stran výsledku
7
Strana od-do
030037
Název nakladatele
American Institute of Physics
Místo vydání
Melville
Místo konání akce
Semarang
Datum konání akce
14. 10. 2021
Typ akce podle státní příslušnosti
WRD - Celosvětová akce
Kód UT WoS článku
—