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| Main Authors: | Bleil, Ulrich, Dillon, Melanie |
|---|---|
| Format: | Dataset Open Access |
| Language: | en |
| Published: |
PANGAEA
2010
|
| Subjects: | |
| Online Access: | https://doi.org/10.1594/PANGAEA.734079 |
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(Fig. 11) Pseudo-Thellier relative paleointensity (PT-RPI) estimates of sediment core GeoB8601-3
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(Fig. 9) NRM20mT/ARM20mT and NRM20mT/SIRM20mT relative paleointensity estimates after 20 mT AF demagnetization of sediment core GeoB6007-2
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(Fig. 8a) ChRM inclinations and declinations of sediment core GeoB6007-2
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Down-core element intensities for iron of sediment core GeoB6007-2
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(Fig. 9) NRM20mT/ARM20mT and NRM20mT/SIRM20mT relative paleointensity estimates after 20 mT AF demagnetization of sediment core GeoB8601-3
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(Figs. 2 and 3) Magnetic susceptibility profile of sediment core GeoB6007-2
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Paleomagnetic analysed of two sediment cores off Cape Ghir
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(Figs. 4, 5 and 6) Saturation remanent magnetization (SIRM), anhysteretic remanent magnetization (ARM), natural remanent magnetization (NRM), ARM/NRM ratio and ARM/SIRM ratio of sediment core GeoB6007-2
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Age model of sediment core GeoB6007-2
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Potassium measured with X-ray fluorescence core scanner on sediment core GeoB6007-2
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(Figure 2) Proxy records of sediment core GeoB6007-2
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Terrigenous sedimentation of sediment core GeoB6007-2
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Down-core element intensities for Ca, Fe, K, Ti and Al of sediment core GeoB6008-1
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(Fig. 8a) ChRM inclinations and declinations of sediment core GeoB8601-3
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(Tabel 1) AMS 14C radiocarbon dates for multicore GeoB6007-1 and gravity core GeoB6007-2
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Zero-field-cooling and warming of room temperature SIRM of sediment core GeoB6229-6
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Low-temperature susceptibilities of sediment core GeoB6229-6
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(Figure 2) Carbon isotopes of sediment core GeoB6007-2
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High resulution end-member model of sediment core GeoB8903-1 (1 cm spacing)
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(Figs. 4, 5 and 6) Saturation remanent magnetization (SIRM), anhysteretic remanent magnetization (ARM), natural remanent magnetization (NRM), ARM/NRM ratio and ARM/SIRM ratio of sediment core GeoB8601-3
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Bulk rock magnetic measurements and thermomagnetic analyses of sediment core GeoB4901-8 from the southeastern flank of the Niger deep-sea fan
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Normalized low-temperature in-phase susceptibility of magnetic extracts measured at 1000 Hz of sediment core GeoB4901-8 from sample depth of 1.65 m to 16.25 m
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