24 datasets found

Stable O isotopic ratios were analysed in core MD13-3473, collected from the Tore seamount on the Iberian margin, for δ18O. Bulk subsamples of approximately 30 grams each were...

We investigated seismogenic mass failure deposits in the Dead Sea center over the last 220 kyr based on the ICDP Dead Sea Core 5017-1. We subdivide the seismogenic mass failure...

The grain-size distribution of the sediment was determined in 2019, following a mean of 5 cm sampling step all along the longest sequence (IZN_19_21). As the sequence contains...

For the Bengal Fan samples, the measurements of major and trace elements were performed at SARM (Nancy, France), following (Carignan et al., 2001)...

Six duplicates of various granulometric fractions (col. 6-7) for the Bengal Fan samples and one for the Lower Meghna were measured for 10Be. The results are presented in a...

Samples from the Bengal Fan and Lower Meghna River were measured. Each line gives the 10Be measurement result for one aliquot of the sample in a specific granulometric sandy...

Core D11956T/P (T stands for trigger core; P for piston core) was collected from the Tagus Abyssal Plain in 1989, photographed, and the magnetic susceptibility logged in 1992...

Sedimentation rate of core MD13-3473 assumed to be constant after linear interpolation between the key-pointers of the hemipelagic record established to construct the age models...

Sedimentation rate of core D219/3P assumed to be constant after linear interpolation between the key-pointers of the hemipelagic record established to construct the age models...

Sedimentation rate of core D11956TC/P assumed to be constant after linear interpolation between the key-pointers of the hemipelagic record established to construct the age...

Semiquantitative element concentrations of 8 sections of core D11956TC/P (TC stands for trigger core; P for piston core) from the Tagus Abyssal Plain were measured at a...

Record of frequency of turbidites during Heinrich events for the last 68 ka, calculated for intervals of 500 years, for core MD03-2698 from the Portuguese margin....

The Ca and Ti of core MD03-2698 from the Portuguese margin were measured within a series of thirteen chemical elements, using a X-Ray Fluorescence (XRF) AVAATECH core-scanner at...

The Ca and Ti of core D11956T/P from the Tagus Abyssal Plain were measured at a resolution of 2 mm, performed at BOSCORF, Southampton National Center, U.K., using a COX...

The Ca and Ti of core D219/3P from the Portuguese margin was measured at a resolution of 1 cm performed at BOSCORF, Southampton National Center, U.K., using a COX Analytical...

Sections of core MD13-3473, collected from the Tore seamount on the Iberian margin, were analysed by using non-destructive, continuous X-ray fluorescence (XRF), with an...

The seismic profiles were acquired in Lake Iznik in 2005, using a 3.5 kHz system (Geopulse, Geoacoustic) with a single channel streamer (20-elements AE5000, GeoAcoustics) and an...

Ganga, Brahmaputra and Lower Meghna sample data are presented. Al/Si and Fe/Si ratios are from Lupker et al. (2013) (URI:https://doi.org/10.1016/j.epsl.2013.01.038) and Sr...

Bulk silicate Sr-Nd data, extracted from bank and bedload, are from Galy and France-Lanord (2001) (URI:https://doi.org/10.1130/0091-7613(2001)029<0023:HERITH>2.0.CO;2),...

Five analytical blanks were prepared synchronously with the samples of Tables S1-S2 (https://doi.org/10.1594/PANGAEA.912098 and https://doi.org/10.1594/PANGAEA.912100). The...