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CT DICOM for Core CE18011_VC2
Computed Tomography DICOM images of core CE18011_VC2 acquired from the western Porcupine Bank (Latitude 51.9765, Longitude -15.037) on board the RV Celtic Explorer using the... -
The Late Pleistocene-Holocene sedimentary evolution of the Sines Contourite D...
The Sines Contourite Drift (SCD), located in the Alentejo margin, southwest Iberian continental margin, has been through many depositional phases in result of climatic... -
Age determination and sea-surface reconstruction of sediment cores from the N...
Polycystine radiolarians are used to reconstruct summer sea surface temperatures (SSSTs) for the Late Pleistocene-Holocene (600-13,400 14C years BP) in the Norwegian Sea. At... -
(Table 3) SSST from polycystine radiolarians, and ages of sediment core MD95-...
AGE is calender age -
High-resolution paleomagnetic records during 11.5-14.5 ka from the northern S...
The dataset contains the inclination and relative paleointensity (RPI) data during 11.5-14.5 ka of core NC2，which is located at the northen South China Sea (114.27E, 21.67N).... -
Physical properties of sediment core CO14-GC-07
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Magnetizations IRM, ARM of sediment core CO14-GC-07
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Geochemical properties of sediment core CO14-GC-07
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Magnetic susceptibility of sediment core CO14-GC-07
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Grain size measurements of sediment core CO14-GC-07
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Age determination of sediment core CO14-GC-07
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Carbonate content of sediment core CO14-GC-07
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