Petrology and geochemistry of calc-alkaline volcanic and …
These characteristics are generated by the fractionation of amphibole and the suppression of plagioclase crystallization from hydrous calc-alkaline magmas.
WhatsApp: +86 18221755073These characteristics are generated by the fractionation of amphibole and the suppression of plagioclase crystallization from hydrous calc-alkaline magmas.
WhatsApp: +86 18221755073Mantle melting at mid-ocean ridges produces dry magmas that differentiate at low-pressure conditions, resulting in early plagioclase saturation, late oxide precipitation, and Fe …
WhatsApp: +86 18221755073In thin arcs, porphyry Cu–Au deposits are associated with both low-K and high-K calc-alkaline magmas as well as with alkaline magmas (Chiaradia, 2020).
WhatsApp: +86 18221755073We propose that such nepheline-normative dykes are a hallmark of hydrous cumulate melting in subvolcanic plumbing systems. Therefore, ne-normative dykes in arc batholiths may indicate periods with high magma fluxes. The online version contains supplementary material available at 10.1007/s00410-023-02047-3.
WhatsApp: +86 18221755073The most compatible rare earth elements in the amphibole structure are dysprosium (Dy) and holmium (Ho). The fractionation between LREE/MREE ( Amph/L D La / Amph/L D Sm = 0.12–0.08) and ( Amph/L D La / Amph/L D Yb = 0.09–0.06) decreases slightly with temperature for calcic amphiboles (Table 5 ).
WhatsApp: +86 18221755073We propose that such nepheline-normative dykes are a hallmark of hydrous cumulate melting in subvolcanic plumbing systems. Therefore, ne-normative dykes in arc batholiths may indicate periods with high magma fluxes.
WhatsApp: +86 18221755073Mantle melting at mid-ocean ridges produces dry magmas that differentiate at low-pressure conditions, resulting in early plagioclase saturation, late oxide precipitation, and Fe-enrichment in mid-ocean ridge basalts (MORBs).
WhatsApp: +86 18221755073We propose that such nepheline-normative dykes are a hallmark of hydrous cumulate melting in subvolcanic plumbing systems. Therefore, ne-normative dykes in arc …
WhatsApp: +86 18221755073The most compatible rare earth elements in the amphibole structure are dysprosium (Dy) and holmium (Ho). The fractionation between LREE/MREE ( Amph/L D La / Amph/L D …
WhatsApp: +86 18221755073We show that trace element ratios such as Nb/Ta and Dy/Yb systematically decrease with increasing SiO 2, for both the 17–16 Ma calc-alkaline and the 12–13 Ma K-rich …
WhatsApp: +86 18221755073We show that magnetite starts to fractionate only at MgO ≤ 4 wt% for nearly all arc magmas and thus has no bearing on the early Fe depletion in calc-alkaline arc magmas. The Fe enrichment at MgO > 4 wt% for tholeiitic arc magmas is …
WhatsApp: +86 18221755073We show that magnetite starts to fractionate only at MgO ≤ 4 wt% for nearly all arc magmas and thus has no bearing on the early Fe depletion in calc-alkaline arc magmas. The Fe enrichment at MgO > 4 wt% for tholeiitic arc magmas is largely caused by clinopyroxene …
WhatsApp: +86 18221755073Porphyry Cu–Au deposits are typically associated with oxidized intermediate or felsic calc-alkaline magmas (Pettke et al. 2010; Sillitoe 2010; Wilkinson 2013). Porphyry deposits host about two-thirds of the world's Cu resources, critical …
WhatsApp: +86 18221755073We propose that such nepheline-normative dykes are a hallmark of hydrous cumulate melting in subvolcanic plumbing systems. Therefore, ne-normative dykes in arc …
WhatsApp: +86 18221755073We show that trace element ratios such as Nb/Ta and Dy/Yb systematically decrease with increasing SiO 2, for both the 17–16 Ma calc-alkaline and the 12–13 Ma K-rich transitional magmatism. In contrast, Th/Nb and La/Nb monitor the changes in the source composition of these magmas.
WhatsApp: +86 18221755073Here we report results from experiments in which natural mélange materials were partially melted at upper mantle conditions to produce alkaline magmas.
WhatsApp: +86 18221755073Porphyry Cu–Au deposits are typically associated with oxidized intermediate or felsic calc-alkaline magmas (Pettke et al. 2010; Sillitoe 2010; Wilkinson 2013). Porphyry deposits host about two-thirds of the world's Cu resources, critical for the green energy transition (Singer 2017).
WhatsApp: +86 18221755073