Crystal chemistry and significance of cation ordering in Mg-Al rich spinels from high-grade hornfels (Predazzo-Monzoni, NE Italy)Mineralogical Magazine - Tập 63 Số 2 - Trang 257-262 - 1999
Francesco Princivalle, A. Della Giusta, Ângelo De Min, E. M. Piccirillo
AbstractTwo Mg-Al spinels (FAS1 and FAS2) in high-grade hornfels from the Toal
de Mason skarn (Predazzo Monzoni, NE Italy) were investigated by means of single
crystal X-ray diffraction and electron microprobe analysis in order to evaluate
the last intra-crystalline closure temperature.The evidence provided by crystal
chemical data from the investigated spinels, compared with that for two other
sp... hiện toàn bộ
Pyrite-pyrrhotine redox reactions in natureMineralogical Magazine - Tập 50 Số 356 - Trang 223-229 - 1986
A. J. Hall
AbstractThe origin in rocks of the common iron sulphides, pyrrhotine, Fe1-xS and
pyrite, FeS2 and their behaviour during geochemical processes is best considered
using the simplified redox reaction: 2FeS ⇌ FeS2 + Fe2+ + 2e−.Thus pyrrhotine is
more reduced than pyrite and is the stable iron sulphide formed from magmas
except where relatively high oxygen fugacities result from falling pressure or
hy... hiện toàn bộ
Carbonatitic melts in cuboid diamonds from Udachnaya kimberlite pipe (Yakutia): evidence from vibrational spectroscopyMineralogical Magazine - Tập 68 Số 1 - Trang 61-73 - 2004
D. A. Zedgenizov, Hiroyuki Kagi, V. S. Shatsky, N. V. Sobolev
AbstractMicro-inclusions (1 –10 μm) in 55 diamonds of cubic habit from the
Udachnaya kimberlite pipe have been studied using vibrational spectroscopy. This
has revealed a multiphase assemblage in cuboid diamonds from the Udachnaya
kimberlite pipe. This assemblage includes carbonates, olivine, apatite,
graphite, water and silicate glasses. The micro-inclusions preserve the high
internal pressure an... hiện toàn bộ
TheREE-and HFSE-bearing phases in the Itatiaia alkaline complex (Brazil) and geochemical evolution of feldspar-rich felsic meltsMineralogical Magazine - Tập 81 Số 2 - Trang 217-250 - 2017
Leone Melluso, Vincenza Guarino, Michele Lustrino, Vincenzo Morra, Roberto dè Gennaro
AbstractThe Late Cretaceous Itatiaia complex is made up of nepheline syenite
grading to peralkaline varieties, quartz syenite and granite, emplaced in the
metamorphic rocks of the Serra do Mar, SE Brazil. The nepheline syenites are
characterized by assemblages with alkali feldspar, nepheline, Fe-Ti oxides,
clinopyroxene, amphibole, apatite and titanite, while the peralkaline nepheline
syenites hav... hiện toàn bộ
Mineral replacement reactions: from macroscopic observations to microscopic mechanismsMineralogical Magazine - Tập 66 Số 5 - Trang 689-708 - 2002
Andrew Putnis
AbstractMineral replacement reactions take place primarily by
dissolution-reprecipitation processes. Processes such as cation exchange,
chemical weathering, deuteric alteration, leaching, pseudomorphism,
metasomatism, diagenesis and metamorphism are all linked by common features in
which one mineral or mineral assemblage is replaced by a more stable assemblage.
The aim of this paper is to review s... hiện toàn bộ
The catalysis of mineral reactions by water and restrictions on the presence of aqueous fluid during metamorphismMineralogical Magazine - Tập 50 Số 357 - Trang 399-415 - 1986
D. C. Rubie
AbstractThe problems of characterizing inter-granular regions and of estimating
rates of intergranular diffusion in metamorphic rocks are discussed.
Inter-granular regions can be anhydrous, hydrated but under-saturated with H2O,
or saturated with H2O, but only in the latter case can a free aqueous fluid
phase be present. Estimates of intergranular diffusion coefficients (DIGR) at
550°C derived fro... hiện toàn bộ