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(Figure F3) Orthogonal vector plots of AF demagnetization steps of IODP Hole ...
This dataset has no description
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(Figure F3) Orthogonal vector plots of AF demagnetization steps of IODP Hole ...
This dataset has no description
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Low-temperature field-cooling-SIRM experiments of sediment core GeoB6229-6
This dataset has no description
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Low-temperature zero-field-cooling-SIRM experiments of sediment core GeoB6229-6
This dataset has no description
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Low-temperature susceptibilities of sediment core GeoB6229-6
This dataset has no description
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Zero-field-cooling and warming of room temperature SIRM of sediment core GeoB...
This dataset has no description
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(Table T3) Anisotropy of magnetic susceptibility of ODP Holes 191-1179B and 1...
This dataset has no description
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(Tables T3, T4) Major and trace element composition of fine-grained sediments...
Sediment depth is given in mbsf. The atomic formula for the hydrothermal chlorite has been calculated on the basis of the ideal O20(OH)16 anion content. -
(Table 2) Flow conditions and bed form dimensions used for the numerical expe...
Geocode: depth, water = mean water depth -
AMS measurements from discrete samples of IODP Exp 371 sites
This dataset has no description
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Fig. 7 data correlation susc at LPSS Süttö, tuned susc Chinese Loess Plateau ...
Correlation between the climatically driven magnetic susceptibility signal found in the LPSS at Sütto and the stacked and independently tuned susceptibility record from the CLP... -
(Supplement 1) Ground-based measurements on aerosol number concentrations at ...
This dataset has no description
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Thermal behaviour of the specific susceptibility (Fig. 11a)
Heating 3-130// Cooling 131-271TSUSC=uncorrected total susceptibilitySCSUSC=total suceptibility corrected for empty furnaceNSUSC= susceptibility normalized by maximum... -
Thermal behaviour of the specific susceptibility (Fig. 11b)
Heating 3-135// Cooling 136-278TSUSC=uncorrected total susceptibilitySCSUSC=total suceptibility corrected for empty furnaceNSUSC= susceptibility normalized by maximum... -
Thermal behaviour of the specific susceptibility (Fig. 11c)
Heating 3-126// Cooling 127-267TSUSC=uncorrected total susceptibilitySCSUSC=total suceptibility corrected for empty furnaceNSUSC= susceptibility normalized by maximum... -
Thermal behaviour of the specific susceptibility (Fig. 11d1)
Heating 3-133// Cooling 134-275TSUSC=uncorrected total susceptibilitySCSUSC=total suceptibility corrected for empty furnaceNSUSC= susceptibility normalized by maximum... -
Thermal behaviour of the specific susceptibility (Fig. 11d2)
Heating 3-132// Cooling 133-274TSUSC=uncorrected total susceptibilitySCSUSC=total suceptibility corrected for empty furnaceNSUSC= susceptibility normalized by maximum... -
Erosion intensity recorded in Lake Anterne (North-western Alps) over the Holo...
Information on the dataset production: The sediment record of Lake Anterne is mostly made of flood deposits characterized by the succession of three facies: a coarse-grained and... -
Erosion intensity recorded in Lake Gers (North-western Alps) over the last 46...
Information on the production of the dataset: The sediment record of Lake Gers consists partly of flood deposits characterised by the succession of three facies: coarse-grained... -
Erosion intensity recorded in Lake Savine (North-western Alps) over the last ...
Information on the production of the dataset: The sediment record of Lake Savine consists partly of flood deposits characterised by the succession of three facies:...
