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Late Holocene seismic uplift events depicted by coastal karst formations in Bali, Indonesia

Datos Bibliográficos

ID14972755
AutoresMiklós Kázmér (0000-0003-1092-1316), Rikza Nahar, Krzysztof Gaidzik (0000-0003-3286-0833)
Año2024
Volumen712
Páginas109577
Fecha de publicación2024-12-01
Peer ReviewedSí
Open AccessSí
TipoARTICLE
RevistaQuaternary International (JOURNAL)
Identificadores de la revistaISSN: 1040-6182 • E-ISSN: 1873-4553
EditorialElsevier BV (PUBLISHER)
DOI10.1016/j.quaint.2024.10.009
OpenAlexW4403940302
IdiomaEN
Citas recibidas1
Referencias citadas47

Limestone shores record earthquake-related uplift and subsidence worldwide. While comprehensive investigations exist for the Mediterranean and Japan, only limited studies are available in other regions. In this study, we analyze the carbonate shore of the Sunda Arc on Bali Island, Indonesia, in terms of tectonic uplift/subsidence. We surveyed coastal profiles of terraces and notches, identifying coastal karst features and bioerosion traces and determining their position relative to sea level. We found a set of marine terraces at Suluban Beach: Level A (lowest) – the active reef pavement with occasional surf potholes; Level B – 0.5–0.7 m above level A, with surf potholes and channels; Level C – 0.8 m above level B , heavily pitted by flat-bottomed pans, separated by heavily karstified ridges; Level D – 2 m above level C, karstified surface, with several decimetres deep karren. The increasing depth of coastal karst features marks a longer time of exposure to the sea, both in the intertidal and the supratidal zone. Holocene sea level reached its present-day position about 5000–6000 years ago; therefore, all coastal features, which require the action of the sea, salt water, and wave action to develop, formed following this period. Bali is on the front of the overriding plate in the Sunda arc. Seismicity is expressed by the uplift of the coastal zone. We propose that seismic events of moment magnitude 6.5–7, with a few hundred years return period, can produce the observed repeated surface uplift of 0.5–2 m in Bali

Geomorphology · Holocene · Karst · Seismology · earthquake and tectonic studies · Geological and Geophysical Studies · Geology and Paleoclimatology Research · Geology · Paleontology

  • Millennial paleo-landscape reconstructions of coastal areas

    Open Access•Claudia Caporizzo, Ana Novak et al.•Quaternary International•2025

  • New empirical relationships among magnitude, rupture length, rupture width, rupture area, and surface displacement

    Donald L Wells, Donald Wells et al.•Bulletin of the Seismological…•1994

  • Holocene sea levels along the Andaman Sea coast of Thailand

    Open Access•Anja Scheffers, Dominik Brill et al.•The Holocene•2012

  • Late-Holocene shoreline changes related to palaeoseismic events in the Ionian Islands, Greece

    Open Access•Paolo A Pirazzoli, Stathis C Stiros et al.•The Holocene•1994

  • Archaeological Evidence for Modern Coastal Uplift at Diu, Saurashtra Peninsula, India

    Open Access•Miklós Kázmér, Nilesh Bhatt et al.•Geoarchaeology•2016

Obras citantes distintas1
Citas por año1
Intervalo de citas2025 - 2025 (1)
Velocidad de citaciónrecent
Altamente citadoNo
Tipos de citaNeutras: 1
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