The partition of iron and magnesium between cordierite and garnet depends on {Mathematical expression} as well as temperature. The apparently conflicting experimental data on the values of KD may be reconciled by considering the {Mathematical expression} pertaining during the different experiments. © 1973 Springer-Verlag
At one atmosphere total pressure, at temperatures of 1180-1300 °C and oxygen fugacities of 10-9-10-3...
We present major and trace element data on coexisting garnet and clinopyroxene from experiments carr...
International audienceWe have investigated the partitioning of Fe3+ between orthopyroxene (Opx) and ...
The partitioning of Fe and Mg between coexisting garnet and olivine has been studied at 30 kb pressu...
The partitioning of Fe and Mg between garnet and olivine has been determined as a function of Fe/Mg ...
Fe)garnet/(Mg/Fe)biotite has been calculated for eight garnet-biotite pairs from rocks ranging from ...
The equilibrium conditions of the reaction, 3 cordierite ⇋ 2 garnet + 4 sillimanite + 5 quartz (+ n ...
Garnet-melt trace element partitioning experiments were performed in the system FeO-CaO-MgO-Al2O3-Si...
The assemblage randite garnet plus epidote is observed in contact metasomatic de-posits in Japan, su...
An experimental study on melting of pelitic rocks shows that garnet is an important residual phase c...
The partitioning of Fe and Mg between olivine and Ca-rich clinopyroxene was treated applying simple ...
Understanding the geochemical behaviour of trace and minor elements in mineral assemblages is of pri...
Ferric iron to total iron ratios in coexisting orthopyroxene and garnet from eighteen mantle xenolit...
Exchange reactions of Fe^ and Mg^ between orthopyroxene and cordierite (abbreviated to Opx and Crd, ...
The phase lelations in the system of Mg-rich garnet composition (P_1p_Alm_) were investigated using ...
At one atmosphere total pressure, at temperatures of 1180-1300 °C and oxygen fugacities of 10-9-10-3...
We present major and trace element data on coexisting garnet and clinopyroxene from experiments carr...
International audienceWe have investigated the partitioning of Fe3+ between orthopyroxene (Opx) and ...
The partitioning of Fe and Mg between coexisting garnet and olivine has been studied at 30 kb pressu...
The partitioning of Fe and Mg between garnet and olivine has been determined as a function of Fe/Mg ...
Fe)garnet/(Mg/Fe)biotite has been calculated for eight garnet-biotite pairs from rocks ranging from ...
The equilibrium conditions of the reaction, 3 cordierite ⇋ 2 garnet + 4 sillimanite + 5 quartz (+ n ...
Garnet-melt trace element partitioning experiments were performed in the system FeO-CaO-MgO-Al2O3-Si...
The assemblage randite garnet plus epidote is observed in contact metasomatic de-posits in Japan, su...
An experimental study on melting of pelitic rocks shows that garnet is an important residual phase c...
The partitioning of Fe and Mg between olivine and Ca-rich clinopyroxene was treated applying simple ...
Understanding the geochemical behaviour of trace and minor elements in mineral assemblages is of pri...
Ferric iron to total iron ratios in coexisting orthopyroxene and garnet from eighteen mantle xenolit...
Exchange reactions of Fe^ and Mg^ between orthopyroxene and cordierite (abbreviated to Opx and Crd, ...
The phase lelations in the system of Mg-rich garnet composition (P_1p_Alm_) were investigated using ...
At one atmosphere total pressure, at temperatures of 1180-1300 °C and oxygen fugacities of 10-9-10-3...
We present major and trace element data on coexisting garnet and clinopyroxene from experiments carr...
International audienceWe have investigated the partitioning of Fe3+ between orthopyroxene (Opx) and ...
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