-
(Table 1f) Chemistry and structural formulae from chlorites of ODP Site 135-841
Numbers of cations on the basis of O10(OH)8 -
(Table 1e) Chemistry and structural formulae from corrensites of ODP Site 135...
Numbers of cations on the basis of O10(OH)5 -
(Table 1d) Chemistry and structural formulae from kaolinites of ODP Site 135-841
Numbers of cations on the basis of O10(OH)8 -
(Table 1c) Chemistry and structural formulae from trioctahedral smectites of ...
Numbers of cations on the basis of O10(OH)2 -
(Table 1b) Chemistry and structural formulae from dioctahedral illites of ODP...
Numbers of cations on the basis of O10(OH)2 -
(Table 1a) Chemistry and structural formulae from dioctahedral smectites and ...
Numbers of cations on the basis of O10(OH)2 -
(Table 1) Geochemistry of sector-zoned crystal at DSDP Hole 45-395A
Variations in crystal morphologies in pillow basalts and probable sheet flows sampled from the region of the East Pacific Rise drilled during Leg 54 are related both to... -
(Table 1) Geochemistry of feldspars at DSDP Holes 62-464 and 62-465A
Labradorite is the principal feldspar in tholeiitic basalt from Deep Sea Drilling Project Site 464, on northern Hess Rise. Andesine and oligoclase constitute most primary... -
(Table 1) Determined and theoretical chemical composition of thaumasite of OD...
Hole 841B was drilled in the forearc region of the Lau Basin at a water depth of 4810 m. The hole penetrated a roughly 500-m-thick series of Miocene volcanic sediments with a... -
(Table 4) Representative chemical compositions of prehnite from the Ohmachi S...
This dataset has no description
-
(Table S5) Representative analyses of the epidote group minerals of sample VT...
Structural formulae have been calculated on the basis of 12.5 oxygens and 8 cations. All Fe assumed as Fe3+; Fe2+ calculated by charge balance to 25 negative charges. #0 = below... -
(Table S3) Representative analyses of titanite of Valtournenche samples
Structural formulae have been calculated on the basis of 5 oxygens, #0 = below detection limit. -
(Table S1) Representative analyses of phengite of sample VT08122
Structural formulae have been calculated on the basis of 12 oxygens for phengite. -
(Table S2) Representative analyses of Mn-cummingtonite, Mg-riebeckite, crossi...
Structural formulae have been calculated on the basis of 26 charges, excluding OH, F and Cl and with a fix Fe3+/Fetot of 0.200 for Mn-cummingtonite. Structural formulae of... -
(Table S6) Amphibole compositions of Pito Deep samples
Mineral formulas were recalculated on the basis of 23 anhydrous oxygens, using the 15 NK procedure of Robinson (1982). -
(Table S7) Epidote compositions of Pito Deep samples
This dataset has no description
-
(Table S5) Chlorite and chlorite-smectite compositions of Pito Deep samples
This dataset has no description
-
(Table S3) Plagioclase compositions of Pito Deep samples
This dataset has no description
-
(Table S4) Clinopyroxene compositions of Pito Deep samples
This dataset has no description
-
(Tab. S2) individual pyroxenes analyses from Ni-Cu-PGE-bearing mafic and ultr...
This dataset has no description
