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(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 13-2) Chemical composition of basalts from the Romanche Fracture Zone
This dataset has no description
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(Table 29) Chemical composition of minerals from basalts of the Vema and Roma...
This dataset has no description
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(Table 13-1) Chemical composition of basalts from the Vema Fracture Zone
This dataset has no description
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(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 3) Representative chemical analyses of clinoamphibole and garnet in ba...
Structural formula calculated on the basis of 23 oxygens. -
Secondary standards for major oxide concentrations of individual glass tephra...
Secondary standards of Lipari, BCR-2Ga, ML3B-G, StHS6/80-G, and Old Crow for major element oxide tephra glass analyses obtained from individual glass shards from samples... -
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... -
Table 5 to 12 - Concentration of major elements in samples from the Esmeralda...
Die vorliegende Arbeit besitzt mit der geologischen Kartierung des Marianen Trogs zwischen 15° und 18°N und der mineralogischen Untersuchung der hydrothermalen Gesteine im... -
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 -
Secondary standards for major element oxide analyses for the geochemical comp...
Secondary Standards of Cannetto Lami Lava, Lipari and BCR-2Ga for major element oxide tephra glass analyses obtained across the period 750-940 CE. Data was obtained using... -
Raw major element oxide data obtained by EPMA for volcanic events analysed fr...
Raw major element oxide data for volcanic events analysed from two proximal sites from Iceland across the period 750-940 CE. Tephra (ash) samples were taken from soil outcrops... -
Raw major element oxide data obtained by EPMA for volcanic events analysed fr...
Raw major element oxide data for volcanic events analysed from B19 [78.00°N/36.40°W], TUNU2013 [78.04°N/33.88°W], and RECAP [71.3°N/26.7°W] ice cores (Greenland) across the... -
Secondary standard for determining geochemical composition of tephra layers f...
We investigated marine sediment core GS16-204-22CC for increased tephra occurrences and geochemically analysed the major element composition of tephra shards to identify their... -
Geochemical composition of tephra layers from deep sediment core GS16-204-22C...
This dataset contains major element oxide data of tephra layers from marine sediment core GS16-204-22CC-A , located in the eastern Labrador Sea, south of Greenland. The core is... -
Lithology, major element composition, and volatile content of analyzed samples
Shown are the averages of glass or groundmass analyses of a single sample; major elements are normalized to 100 wt.% volatile-free. Sum_orig is the original sum prior to...
