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dc.rights.licenseopenen_US
dc.contributor.authorSANTOSO, Arianto Budi
dc.contributor.authorWILS, Katleen
dc.contributor.authorDARYONO, Mudrik
dc.contributor.authorPRAET, Nore
dc.contributor.authorSANTOSO, Arianto
dc.contributor.authorDIANTO, Aan
hal.structure.identifierEnvironnements et Paléoenvironnements OCéaniques [EPOC]
dc.contributor.authorSCHMIDT, Sabine
dc.contributor.authorVERVOORT, Morgan
dc.contributor.authorHUANG, Jyh-Jaan Steven
dc.contributor.authorKUSMANTO, Edi
dc.contributor.authorSUANDHI, Purnama
dc.contributor.authorNATAWIDJAJA, Danny
dc.contributor.authorDE BATIST, Marc
dc.date.accessioned2024-03-11T11:53:44Z
dc.date.available2024-03-11T11:53:44Z
dc.date.issued2021-04
dc.identifier.issn0037-0738en_US
dc.identifier.urihttps://oskar-bordeaux.fr/handle/20.500.12278/188665
dc.description.abstractEnNatural hazards such as earthquakes, volcanic activity, and heavy rainfall causing floods and debris avalanches are common phenomena in many tropical settings, including the island of Sumatra, located in the Indonesian archipelago. To enhance our understanding of the recurrence of these often destructive events, we studied the sedimentary infill of two lakes in the Padang highlands, West Sumatra. This includes Lake Singkarak, a tectonically-formed lake located on a step-over of a major strike-slip fault system (the Sumatran Fault), and Lake Maninjau, a caldera lake. Both lakes are located -300 km from the Sunda subduction trench and surrounded by steep slopes and a chain of active volcanoes. Hence, considering their unique tectonic setting, these lakes may potentially record a wide range of natural hazards that affect the region. A combination of seismic-reflection pro¬files and short sediment cores revealed that both lakes indeed record various types of natural hazards, each with their own sedimentary response to a specific type of event. Lake Singkarak can be used to study past floods and major debris avalanches in addition to high-magnitude megathrust earthquakes, while traces of past intraplate earthquakes have been identified in both lakes. Furthermore, we argue that Lake Singkarak is an ideal recorder of volcanic activity in the region, while Lake Maninjau itself can pose a volcanic hazard toits surroundings as demonstrated by potential activity of the volcano below the lake
dc.language.isoENen_US
dc.subject.enIndonesia
dc.subject.enNatural hazards
dc.subject.enTurbidite
dc.subject.enVolcanic activity
dc.subject.enLacustrine paleoseismology
dc.subject.enEarthquake
dc.subject.enIndonesia
dc.title.enThe sediments of Lake Singkarak and Lake Maninjau in West Sumatra reveal their earthquake, volcanic and rainfall history
dc.title.alternativeSediment. Geolen_US
dc.typeArticle de revueen_US
dc.identifier.doi10.1016/j.sedgeo.2021.105863en_US
dc.subject.halPlanète et Univers [physics]/Interfaces continentales, environnementen_US
bordeaux.journalSedimentary Geologyen_US
bordeaux.page105863en_US
bordeaux.volume416en_US
bordeaux.hal.laboratoriesEPOC : Environnements et Paléoenvironnements Océaniques et Continentaux - UMR 5805en_US
bordeaux.institutionUniversité de Bordeauxen_US
bordeaux.institutionCNRSen_US
bordeaux.teamSEDIMen_US
bordeaux.peerReviewedouien_US
bordeaux.inpressnonen_US
bordeaux.import.sourcehal
hal.identifierhal-03337026
hal.version1
hal.popularnonen_US
hal.audienceInternationaleen_US
hal.exportfalse
workflow.import.sourcehal
dc.rights.ccPas de Licence CCen_US
bordeaux.COinSctx_ver=Z39.88-2004&rft_val_fmt=info:ofi/fmt:kev:mtx:journal&rft.jtitle=Sedimentary%20Geology&rft.date=2021-04&rft.volume=416&rft.spage=105863&rft.epage=105863&rft.eissn=0037-0738&rft.issn=0037-0738&rft.au=SANTOSO,%20Arianto%20Budi&WILS,%20Katleen&DARYONO,%20Mudrik&PRAET,%20Nore&SANTOSO,%20Arianto&rft.genre=article


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