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Supplemental Table 3: Data used for clinopyroxene-melt thermobarometry
Data used fro clinopyroxene-melt thermobarometry. Clinopyroxene rim compositions from electron microprobe analysis on selected submarine lavas from Serreta Ridge (SR-A) and the... -
(Table 1) Chemical composition of Black Sea sediments
This dataset has no description
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Major oxide concentrations of individual glass tephra shards from the Greenla...
Major oxide concentrations of individual glass tephra shards from tephra deposits in the Greenland TUNU2013 [78.04°N/33.88°W] and Summit2023 [72.6°N/38.3°W] ice cores. Deposits... -
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... -
Major and trace elements, Sr-Nd-Pb isotope data of lavas from D. João de Cast...
The D. João de Castro seamount is located on the ultraslow diverging Terceira Rift, Azores. D. João de Castro is a young central volcano (<0.5 Ma) with recent volcanic and... -
Mineral quantification of sediment cores GeoB2703-5, GeoB6812-1, GeoB13861-1,...
Results are weight % if not stated differently values smaller than 1 wt.% can only be seen as traces of the mineral. -
(Table 2) Selected analyses for garnet pyroxenite and amphibolite samples fro...
Garnet pyroxenite samples = W216, W218, W240, W242A and garnet amphibolite samples = W232, W251, W334. -
(Table T2) Mean geochemistry and mineralogy of garnet sand grains from ODP Sa...
Sediment depth is given in mbsf. Number of ions is calculated on the basis of 12 oxygen atoms. Abundance of minerals is given in molecular percent, major element oxides in wt %. -
(Table S7) Representative analyses of garnet from meta-chert samples VT08129 ...
Structural formulae have been calculated on the basis of 12 oxygens. #0 = below detection limit. -
Table 2. Element composition of the Yangla granodiorite
This dataset has no description
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(Table 2) Average major-element composition of glass shards from Toba Tephra ...
Positions are estimated from map. Analyses done on a Cameca SX-50 wavelength dispersive electron microprobe operating at 15 kV accelerating voltage, 20-mm beam diameter, 6nA... -
(Table 3) Representative chemical analyses of clinoamphibole and garnet in ba...
Structural formula calculated on the basis of 23 oxygens. -
Table D.14: Microprobe analyses of garnets from sample 2119
Number of ions on the basis of 24 O; oxides given in weight percentage -
Table C.18: Microprobe analysis of garnets from samples no. 2168 and 2181
Number of ions on the basis of 24 O; oxides given in weight percentage -
Table C.17: Microprobe analysis of garnets from sample no. 1563
Number of ions on the basis of 24 O; oxides given in weight percentage -
Table C.15+16: Microprobe analysis of garnets from sample no. 1562
Number of ions on the basis of 24 O; oxides given in weight percentage -
Wavelength Dispersive Electron Microprobe Analysis of single glass shards (WD...
This dataset has no description
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Tephra geochemistry from Lake Ohrid (Macedonia/Albania) sediment core ICDP5045-1
Geochemical finger print data (in wt. %) of individual glass shards from 3 three previously described cryptotephra layer in the Late Glacial to Holocene sediments of the DEEP... -
X-ray diffraction results from IODP Hole 386-M0095B
Results of X-ray diffraction (XRD) analyses from the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). The offshore... -
X-ray diffraction results from IODP Hole 386-M0095A
Results of X-ray diffraction (XRD) analyses from the above given hole of International Ocean Discovery Program (IODP) Expedition 386 (Japan Trench Paleoseismology). The offshore...
