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Lead and neodymium isotope time-series for manganese crust D137-01
Ages were calculated using growth rates derived by 10Be/9Be ratios and constant Co-flux model. For compatibility all ratios were normalized to the NIST SRM981 values of Galer... -
Radiosonde measurements in Nigardsbreen and Mjølverdalen during fall 2023 (gp...
This dataset has no description
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Radiosonde measurements in Nigardsbreen and Mjølverdalen during fall 2023 (gp...
This dataset has no description
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(Table 2) Be isotope and Co concentrations for the four crusts
This dataset has no description
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(Table 1) AMS radiocarbon dates of sediment core GeoB3910-2
AMS radiocarbon dates, reservoir age of the surface waters off the coast of Northeast Brazil for two different AMOC strengths (R), two sigma ranges of the calibration using... -
Inherent damage tolerance of fine grained nuclear graphite at elevated temper...
Current UK reactors use a graphite composite material in the core and this material comprises coarse grains and about 20 vol.% porosity. This material functions well so far but... -
Magnetic properties of photomagnetic molecular square complexes
This experiment aims at studying the magnetic behaviour of the molecular square complex {[Fe{B(pz)_4}(CN)_3]_2[Co(bik)_2]_2}(ClO_4)_2 . 3H_2O [B(pz)_4 = tetrapyrazolylborate,... -
Characterisation of Zeolite Precursor Gels Over Wide Q Range
Our objective is to determine new structural information about the structure of amorphous silicate gels formed early in the synthesis of crystalline, microporous zeolites. This... -
Neodymium and lead isotopes from manganese crust G9632-47 (ROM32)
The ages are calculated for the respective mean depths. Depending on the different growth rates of the crusts, samples correspond to different age intervals. -
Neodymium and lead isotopes from manganese crust S1601-13 (ROM16)
The ages are calculated for the respective mean depths. Depending on the different growth rates of the crusts, samples correspond to different age intervals. -
Neodymium and lead isotopes from manganese crust G9646-63 (ROM46)
The ages are calculated for the respective mean depths. Depending on the different growth rates of the crusts, samples correspond to different age intervals. -
(Table 4) Average composition of glass shards and glassy mesostasis in sedime...
This dataset has no description
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(Table III) Size measurements of the species Paralia sulcata from sediment co...
measurement of 50 valves per sample -
(Table III) Size measurements of the species Paralia sulcata from sediment co...
measurement of 50 valves per sample -
Tabelle 3. Temperaturen an der Oberfläche und in 500 mb
This dataset has no description
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Analysis of tidal notches in the Mediterranean Sea
Exp. = exposed.Shelt. = sheltered. -
Transect characteristics obtained on nearshore lagoonal reefs on the Belize M...
This dataset has no description
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(Table S1a) Oregon margin sediment grain sizes
This dataset has no description
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Age determination of core MF4-12 from Mfabeni peatland
a: Modern age, expressed as percent modern carbon (pMC), equals –307±23 14C yrs BP.b: Modern age, expressed as percent modern carbon (pMC), equals –143±24 14C yrs BP. -
Neodymium and lead isotopes from manganese crust DR01-001a (Vema)
The ages are calculated for the respective mean depths. Depending on the different growth rates of the crusts, samples correspond to different age intervals.
