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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