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 mo...... 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 prese...... 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 p...... 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...... hiện toàn bộ