(Table 1) Chronology of sediment core GeoB10065-9

  • The 210Pbxs data of MUC-A and MUC-B reveal the existence of a 10-cm thick sequence of repeated young sediment above 14 cm corrected depth. This can likely be attributed to small-scale deformation and/or sliding processes due to seismic activity that can often occur in an earthquake prone region like Indonesia.
DOI https://doi.org/10.1594/PANGAEA.832464
Related Identifier https://doi.org/10.1594/PANGAEA.832475
Related Identifier https://doi.org/10.1016/j.quascirev.2014.04.006
Metadata Access https://ws.pangaea.de/oai/provider?verb=GetRecord&metadataPrefix=datacite4&identifier=oai:pangaea.de:doi:10.1594/PANGAEA.832464
Creator Steinke, Stephan; Mohtadi, Mahyar ; Prange, Matthias (ORCID: 0000-0001-5874-756X); Varma, Vidya ; Pittauerova, Daniela (ORCID: 0000-0002-3643-333X); Fischer, Helmut W
Publisher PANGAEA
Publication Year 2014
Rights Creative Commons Attribution 3.0 Unported; https://creativecommons.org/licenses/by/3.0/
OpenAccess true
Language English
Resource Type Dataset
Format text/tab-separated-values
Size 218 data points
Discipline Earth System Research
Spatial Coverage (118.892 LON, -9.223 LAT)