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X-ray diffraction (XRD) data of basaltic rocks cored at IODP Site 369-U1513
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X-ray fluorescence Ca/Fe-ratios of IODP Site 369-U1514
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Bulk stable isotopes of IODP Site 369-U1514
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X-Ray Fluorescence (XRF) spectrometry data from a volcanic sequence from IODP...
Core samples were collected from a volcanic sequence at Holes D and E, Site U1513 on the eastern Naturaliste Plateau, offshore southwest Australia. The site was drilled by the... -
Lower to middle Eocene astronomically-tuned Ca/Fe-ratios and bulk stable isot...
The geologic time scale for the Cenozoic Era has been notably improved over the last decades by virtue of integrated stratigraphy, combining high-resolution astrochronologies,... -
Compositional results from the Late Miocene and Pliocene of Sites U1514 and U...
Late Miocene and Pliocene marine sediments were cored at Sites U1514 and U1516 in the Mentelle Basin offshore Western Australia, as part of the International Ocean Discovery... -
X-ray diffraction (XRD), X-ray fluorescence (XRF) and 40Ar/39Ar data obtained...
A series of basaltic flows and associated dolerite dykes were cored at depths of >680m below the seafloor, at the base of IODP Site U1513. These cores were obtained from the... -
Element analysis (XRF) of basaltic rocks of IODP Site 369-U1513
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Sample information of basaltic rocks of IODP Site 369-U1513
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40Ar/39Ar isotopic analyse of basaltic rocks of IODP Site 369-U1513
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Laser driffaction grain-size fractions for IODP Hole 369-U1516A (Table S3)
Hole U1516A laser diffraction grain-size fractions. Dx (10) - 10% percentile size; Dx (50) - 50% percentile size; Dx (90) - 90% percentile size. -
Compositional results from discrete x-ray fluorescence measurements for IODP ...
Compositional results (%) from discrete x-ray fluorescence measurements (WD-XRF) for Site U1514. Excess silica is calculated from the linear relationship between terrigenous... -
Compositional results from discrete x-ray fluorescence measurements for IODP ...
Compositional results (%) from discrete x-ray fluorescence measurements (WD-XRF) for Site U1516. Excess silica is calculated from the linear relationship between terrigenous...