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(Fig. 6) Decarbonated grain size mass frequencies of sediment core GeoB130206-1
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(Fig. 5) Decarbonated grain size mass frequencies of sediment core GeoB13071-1
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(Fig. 6) Bulk grain size mass frequencies of sediment core GeoB130206-1
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(Fig. 5) Bulk grain size mass frequencies of sediment core GeoB13071-1
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(Fig. 6) Lithology of sediment core GeoB130206-1
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(Fig. 5) Lithology of sediment core GeoB13071-1
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(Fig. 3) Inter-core correlation of Ca/Fe ratios and magnetic susceptibility o...
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(Fig. 3) Inter-core correlation of Ca/Fe ratios and magnetic susceptibility o...
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(Table 1) Age model tie points of sediment cores GeoB11035-1, GeoB13071-1, an...
14C age at base of GeoB11035-1 (asterisk) is not considered because beyond radiocarbon limits. a Correlation with d18O record of GISPII. b Leibniz Laboratory, Kiel, Germany. c... -
(Figure 10b, 11) Benthic electromagnetic profile of GeoB130106 on the northwe...
Porosity is derived from Archie's law with constants m = 1.6, a = 1 and 14.4% offset (susceptibility with 37.7 offset; based on Figure 9). -
(Figure 10a, 11, 12) Benthic electromagnetic profile of GeoB130124 on the nor...
Porosity is derived from Archie's law with constants m = 1.6, a = 1 and 14.4% offset (susceptibility with 37.7 offset; based on Figure 9). -
X-ray diffraction analysis of sediment samples from the NW Iberian shelf system
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Binocular component analysis performed on the grain-size fraction 250–500 µm ...
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(Table 2) Radiocarbon dates and age calibration
°1From Lantzsch et al. (2009a,b).*Age calibrationisbasedonthefunctionof Bard etal.(1998).Radiocarbon laboratory: KIA=Leibniz Laboratory in Kiel (Germany) and Poz=Poznan'... -
(Table 2) Radiocarbon dates and age calibration
The high-energy, low-accumulation NW Iberian shelf features three confined Holocene mud depocentres. Here, we show that the evolution of such depocentres follows successive... -
(Table 2) Radiocarbon measurements and age calibration
Continental shelves represent areas of highest economical and ecological importance. Nevertheless, these sedimentary systems remain poorly understood due to a complex interplay... -
Controls of sediment dynamics on the Galician slope reconstructed from three ...
Controls of sediment dynamics at the Galician continental slope (NW Iberia) during the past 30 ka were reconstructed from three new gravity cores (GeoB11035-1, 130206-1,... -
Magnetic susceptibility and electric conductivity of marine surficial sedimen...
Distribution, accumulation and diagenesis of surficial sediments in coastal and continental shelf systems follow complex chains of localized processes and form deposits of great... -
X-ray diffraction analysis, binocular component analysis and radiocarbon dati...
Based on a well-established stratigraphic framework and 47 AMS-14C dated sediment cores, the distribution of facies types on the NW Iberian margin is analysed in response to the...
