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(Appendix A1) Geochemistry of sediment core GIK17603-1
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(Appendix A1) Geochemistry of sediment profile GIK17597-1_17607-1
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(Appendix A1) Geochemistry of sediment core GIK17594-1
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(Appendix A1) Geochemistry of sediment core GIK17591-1
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(Appendix A1) Geochemistry of sediment core GIK17590-1
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(Appendix A1) Geochemistry of sediment core GIK17587-1
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(Appendix A1) Geochemistry of sediment core GIK17582-1
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(Appendix A1) Geochemistry of sediment core GIK17580-1
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(Appendix A1) Geochemistry of sediment core GIK17576-1
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(Supplement EA1) Elements, Neodymium and Hafnium analysis on lavas from Nevad...
Major elements were determined by X-ray fluorescence spectroscopy (XRF) using a Siemens SRS-3000 instrument in the Laboratorio Universitario de Geoquímica Isotópica (LUGIS),... -
(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 13-2) Chemical composition of basalts from the Romanche Fracture Zone
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(Table 29) Chemical composition of minerals from basalts of the Vema and Roma...
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(Table 13-1) Chemical composition of basalts from the Vema Fracture Zone
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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
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(Table 3) Representative chemical analyses of clinoamphibole and garnet in ba...
Structural formula calculated on the basis of 23 oxygens. -
Major elements of sediment cores of the active channel and lobes of the Benga...
Major element concentration measured on the gravity core GeoB25818-2 core and on the MUC cores sampling in the active Southern Lobe of the Bengal Fan. These cores were recovered... -
Major element composition of glass shards from 1458/59 CE cryptotephra in VK2...
We present the major element compositions (SiO₂, TiO₂, Al₂O₃, FeO, MgO, CaO, Na₂O, and K₂O) of unpolished micron-sized volcanic glass shards within cryptotephra layers...
