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Indian OceanPlace
IndiaPlace
Instead of the isotopes Jo, Th, and Pa the radioactive daughter products Rn, Tn, and An were measured. It was possible to date four cores and to calculate the sedimentation rates. A rough estimation of the sedimentation in the northern part of the Indian Ocean can be given. In the middle part, the sedimentation rate is s = 0.32 cm/103 years, and near Africa and near India this rate increases to values of about 2 cm/103 years
A down-core 231Pa/230Th record has been measured from the southwestern Indian Ocean to reconstruct t...
Here we present reconstructions of water residence times (depicted as ΔΔ14C and δ13C) for the last 3...
Of the six deep-sea cores obtained from the central equatorial Indian Ocean along Long. 78°E. from L...
Instead of the isotopes Jo, Th, and Pa the radioactive daughter products Rn, Tn, and An were measure...
International audienceThe rate of oceanic sedimentation was determined by gamma-ray spectroscopy. Th...
Radiocarbon datings are used to calculate mean sedimentation rates of metalliferous sediments in the...
A continuous 10-m-long section consisting of roughly two thirds Ethmodiscus rex (a diatom) and one t...
The determination of the sedimentation rates of carbonate-free, virtually organic-free marine sedime...
This study of subseabed sediments indicates that natural radionuclides can be employed to define pas...
We present a dating method for deep-sea sediments that is independent from the presence of microfoss...
We present a dating method for deep-sea sediments that uses the natural radionuclide 230Th (half-lif...
The vertical profiles of 230Thexcess and 230Thexcess/232Th in a sediment core have been used to dete...
Three cores taken in the tidal flat of the Bay of Mont Saint-Michel were dated with two different me...
This thesis considers the use of two U-series nuclides – 231 Pa and 230 Th – as proxies for studying...
This thesis considers the use of two U-series nuclides – 231 Pa and 230 Th – as proxies for studying...
A down-core 231Pa/230Th record has been measured from the southwestern Indian Ocean to reconstruct t...
Here we present reconstructions of water residence times (depicted as ΔΔ14C and δ13C) for the last 3...
Of the six deep-sea cores obtained from the central equatorial Indian Ocean along Long. 78°E. from L...
Instead of the isotopes Jo, Th, and Pa the radioactive daughter products Rn, Tn, and An were measure...
International audienceThe rate of oceanic sedimentation was determined by gamma-ray spectroscopy. Th...
Radiocarbon datings are used to calculate mean sedimentation rates of metalliferous sediments in the...
A continuous 10-m-long section consisting of roughly two thirds Ethmodiscus rex (a diatom) and one t...
The determination of the sedimentation rates of carbonate-free, virtually organic-free marine sedime...
This study of subseabed sediments indicates that natural radionuclides can be employed to define pas...
We present a dating method for deep-sea sediments that is independent from the presence of microfoss...
We present a dating method for deep-sea sediments that uses the natural radionuclide 230Th (half-lif...
The vertical profiles of 230Thexcess and 230Thexcess/232Th in a sediment core have been used to dete...
Three cores taken in the tidal flat of the Bay of Mont Saint-Michel were dated with two different me...
This thesis considers the use of two U-series nuclides – 231 Pa and 230 Th – as proxies for studying...
This thesis considers the use of two U-series nuclides – 231 Pa and 230 Th – as proxies for studying...
A down-core 231Pa/230Th record has been measured from the southwestern Indian Ocean to reconstruct t...
Here we present reconstructions of water residence times (depicted as ΔΔ14C and δ13C) for the last 3...
Of the six deep-sea cores obtained from the central equatorial Indian Ocean along Long. 78°E. from L...
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