Mixing of magmatic-hydrothermal and metamorphic fluids and the origin of peribatholitic Sn vein-type deposits in Rwanda
The fluid sources of granite-related Sn-quartz vein deposits are commonly obscured by fluid
mixing or fluid-rock interactions. As a result, fluid inclusions, minerals and isotopes in these …
mixing or fluid-rock interactions. As a result, fluid inclusions, minerals and isotopes in these …
Origin of high electrical conductivity in the lower continental crust: A review
X Yang - Surveys in Geophysics, 2011 - Springer
Electromagnetic measurements have demonstrated that the lower continental crust has
remarkable electrical anomalies of high conductivity and electrical anisotropy on a global …
remarkable electrical anomalies of high conductivity and electrical anisotropy on a global …
Recognition of a 600-km-long Late Triassic rare metal (Li-Rb-Be-Nb-Ta) pegmatite belt in the western Kunlun orogenic belt, Western China
QH Yan, H Wang, G Chi, Q Wang, H Hu… - Economic …, 2022 - pubs.geoscienceworld.org
The rising demand of strategic metals, especially lithium, necessitates discovery of new
resources to meet the global supply chain. Recently, several pegmatite-hosted rare metal (Li …
resources to meet the global supply chain. Recently, several pegmatite-hosted rare metal (Li …
Alkali metal and rare earth element evolution of rock-forming minerals from the Gatumba area pegmatites (Rwanda): Quantitative assessment of crystal-melt …
This study presents a general model for the evaluation of Rayleigh fractional crystallisation
as the principal differentiation mechanism in the formation of regionally zoned common and …
as the principal differentiation mechanism in the formation of regionally zoned common and …
Fluid fractionation of tungsten during granite–pegmatite differentiation and the metal source of peribatholitic W quartz veins: Evidence from the Karagwe-Ankole Belt …
The identification of a magmatic source for granite-associated rare metal (W, Nb, Ta and Sn)
mineralisation in metasediment-hosted quartz veins is often obscured by intense fluid–rock …
mineralisation in metasediment-hosted quartz veins is often obscured by intense fluid–rock …
Electrical conductivity of orthopyroxene and plagioclase in the lower crust
The electrical conductivities of lower crustal orthopyroxene and plagioclase, as well as their
dependence on water content, were measured at 6–12 kbar and 300–1,000° C on both …
dependence on water content, were measured at 6–12 kbar and 300–1,000° C on both …
[HTML][HTML] Genetic relationship between greisenization and Sn-W mineralizations in vein and greisen deposits: Insights from the Panasqueira deposit (Portugal)
G Launay, S Sizaret, P Lach… - Bulletin de la …, 2021 - pubs.geoscienceworld.org
The W-Sn Panasqueira ore deposit is a magmatic-hydrothermal system, which includes a
high grade quartz-vein type mineralization and underneath disseminated greisen-type …
high grade quartz-vein type mineralization and underneath disseminated greisen-type …
Detailed paragenesis and Li-mica compositions as recorders of the magmatic-hydrothermal evolution of the Maoping W-Sn deposit (Jiangxi, China)
Li-micas have been used as indicators of the evolution of granites. However, hydrothermal
Li-micas are less documented. World-class W-Sn deposits associated with Early …
Li-micas are less documented. World-class W-Sn deposits associated with Early …
A new style of rare metal granite with Nb-rich mica: The Early Cretaceous Huangshan rare-metal granite suite, northeast Jiangxi Province, southeast China
Z Zhu, R Wang, C Marignac, M Cuney… - American …, 2018 - degruyter.com
In rare-metal granites, niobium and tantalum are generally hosted by Nb–Ta oxides.
However, in SE China, the Nb-specialized Huangshan granites are a unique occurrence in …
However, in SE China, the Nb-specialized Huangshan granites are a unique occurrence in …
Mineralogy of the Koktokay No. 3 pegmatite, Altai, NW China: implications for evolution and melt–fluid processes of rare-metal pegmatites
Q Zhou, K Qin, D Tang, C Wang… - European Journal …, 2015 - pubs.geoscienceworld.org
The Koktokay No. 3 pegmatite is the largest Li-Be-Nb-Ta-Cs pegmatitic rare-metal deposit of
the Chinese Altai orogenic belt, and is famous for its concentric ring zonation pattern (nine …
the Chinese Altai orogenic belt, and is famous for its concentric ring zonation pattern (nine …