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Effects of the hydrous domain in the mantle wedge on magma formation and mixi...
Major and trace element concentrations of young volcanic rocks from the Northeast Lau Basin in the SW Pacific Ocean, as well as Sr-Nd-Hf-Pb isotope compositions. Analyses were... -
Trace element compositions in clinopyroxene and plagioclase, and crystallizat...
As largest and best-exposed paleo-fast-spread oceanic crust on land, the Samail ophiolite in the Sultanate of Oman represents an ideal natural laboratory for investigating... -
U-Pb analyses and trace element data for detrital zircon, apatite and titanit...
This data set was replaced by a newer version on July 15th, 2020. Changes in then new dataset: Unit of "Age" and precision in data for element values. -
Collated apatite trace element data (ppm) from the literature
This database contains trace element compositional data for apatite from 23 published (cited) datasets on bedrock apatite trace element compositions. IM = Mafic I-type... -
Particulate REE and Hf concentrations in surface sediment from RV Meteor crui...
All samples were obtained during RV Meteor cruise M147 (April–May 2018), conducted as the official process study GAPR11 within the framework of the international GEOTRACES program. -
Dissolved REE concentrations in near-bottom water samples from RV Meteor crui...
All samples were obtained during RV Meteor cruise M147 (April–May 2018), conducted as the official process study GAPR11 within the framework of the international GEOTRACES program. -
Dissolved, soluble, and truly dissolved rare earth element and yttrium and ma...
The Neodymium (Nd) isotopic signature (εNd) has been widely used as a proxy to reconstruct past ocean circulation. Recently it has been increasingly questioned which archives... -
Dissolved rare earth element and yttrium and manganese concentrations in pore...
The Neodymium (Nd) isotopic signature (εNd) has been widely used as a proxy to reconstruct past ocean circulation. Recently it has been increasingly questioned which archives... -
Rare earth element and yttrium concentrations in leach fractions of sediment ...
The Neodymium (Nd) isotopic signature (εNd) has been widely used as a proxy to reconstruct past ocean circulation. Recently it has been increasingly questioned which archives... -
Dissolved rare earth element and yttrium and manganese concentrations in pore...
The Neodymium (Nd) isotopic signature (εNd) has been widely used as a proxy to reconstruct past ocean circulation. Recently it has been increasingly questioned which archives... -
Dissolved rare earth element and yttrium concentrations in bottom seawater fr...
The Neodymium (Nd) isotopic signature (εNd) has been widely used as a proxy to reconstruct past ocean circulation. Recently it has been increasingly questioned which archives... -
Trace element contents for the <2 μm, 2-20 μm and bulk fractions from LGM Eur...
Trace element contents in microg/g measured on the <2 microns, 2-20 microns size fractions and bulk samples from LGM European loess sequences. Samples were crushed in an... -
Inorganic geochemistry of sedimentary rocks in the catchment of river Thuring...
A literature retrieval was performed for whole rock geochemical analyses of sedimentary, magmatic and metamorphic rocks in the catchment of River Thuringian Saale for the past... -
(Table 4a) Chemical composition of metamorphic rocks from the upper unit of t...
This dataset has no description
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(Table 12) Whole-rock analyses of interlaboratory samples of ODP Leg 121
Oxide data determined on fused glass beads and given on an anhydrous basis; trace elements measured on unignited powder samples. -
(Table 9) Chemical composition of whole rocks from DSDP sites
Fe2O3, FeO, CIPW norms, and FeO/MgO ratios have been calculated from total iron using a Fe2O3/FeO ratio of 0.15. -
(Table 8) Chemical composition of whole rocks from ODP Hole 121-758A
Fe2O3, FeO, CIPW norms, and FeO/MgO ratios have been calculated from total iron using a Fe2O3/FeO ratio of 0.15. -
(Table 7) Chemical composition of whole rocks from ODP Site 121-757B
Fe2O3, FeO, CIPW norms, and FeO/MgO ratios have been calculated from total iron using a Fe2O3/FeO ratio of 0.15. -
(Table 6) Chemical composition of whole rocks from ODP Site 121-756
Fe2O3, FeO, CIPW norms, and FeO/MgO ratios have been calculated from total iron using a Fe2O3/FeO ratio of 0.15. -
Major and trace element analyses of ODP Leg 120 volcanic rocks (Table 1)
Widespread Lower Cretaceous magmatism occurred along the Indian-Australian/Antarctic margins, and in the juvenile Indian Ocean, during the rifting of eastern Gondwana. The...
