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The magnetostratigraphy and cyclostratigraphy age data, and MS and NGR data u...
The IODP Expedition 368 began drilling in the South China Sea in 2017. The initial chronology of Site 368-U1505, including magnetostratigraphy and biostratigraphy, was completed... -
Trace-element concentrations of hydrothermally altered basaltic rocks in IODP...
a Relative standard deviation between 10–16%.b Data determined by XRF with better quality are used.Values in mg/kg given in ppm. -
Natural gamma ray (120-180 mcd) for IODP Hole 368-U1505C and 368-U1505D
This dataset has no description
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Detrended natural gamma ray (120-180 mcd) for IODP Hole 368-U1505C and 368-U1...
This dataset has no description
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Detrended natural gamma ray (60-120 mcd) for IODP Hole 368-U1505C and 368-U1505D
This dataset has no description
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Natural gamma ray (60-120 mcd) for IODP Hole 368-U1505C and 368-U1505D
This dataset has no description
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Natural gamma ray (raw data) for IODP Hole 368-U1505C and 368-U1505D
This dataset has no description
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Magnetic susceptibility (120-180 mcd) for IODP Hole 368-U1505C and 368-U1505D
This dataset has no description
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Detrended magnetic susceptibility (120-180 mcd) for IODP Hole 368-U1505C and ...
This dataset has no description
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Detrended magnetic susceptibility (60-120 mcd) for IODP Hole 368-U1505C and 3...
This dataset has no description
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Magnetic susceptibility (60-120 mcd) for IODP Hole 368-U1505C and 368-U1505D
This dataset has no description
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Magnetic susceptibility (raw data) for IODP Hole 368-U1505C and 368-U1505D
This dataset has no description
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Palaeomagnetic age from IODP Hole 368-U1505C and 368-U1505D
This dataset has no description
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Astronomical timescale for IODP Hole 368-U1505C and 368-U1505D
This dataset has no description
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Description of investigated samples in IODP Hole 368-U1502B (Table S1)
This dataset has no description
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Strontium and Nd isotope compositions of hydrothermally altered basaltic rock...
a Six sample-types are distinguished (see Section 4); note that the fully altered samples and the breccia sample are taken as endmembers of the hydrothermal alteration and... -
Rare-earth-element (REE) concentrations of hydrothermally altered basaltic ro...
a Eu anomaly is calculated using Eu/Eu* = EuN / (SmN 2 + GdN 2) 1/2; the subscript N denotes normalized to chondrite (Anders and Grevesse, 1989).b Normalized to chondrite... -
Major-element concentrations of hydrothermally altered basaltic rocks in IODP...
a Fe2O3* refers to total iron oxides.b LOI (i.e. loss on ignition at 600°C) contents are shown.c Total percentages range between 93.0–101.0%, on average 98.3%.% values are given... -
Major element composition of IODP Site U1501 in the South China Sea from 5.2 ...
IODP Site U1501 (18°53.09′N, 115°45.95′E, water depth: 2846 m) is situated on the west side of Pearl River Canyon. The length for hole C at IODP Site U1501 is up to 461.8 m,...
