Semantic Scholar extracted view of "Implications of UPb ages of columbite-tantalites from granitic pegmatites for the Palaeoproterozoic accretion of 1.90–1.85 Ga magmatic arcs to the Baltic Shield" by R. Romer et al. ... Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the …
Tin granites and associated Ta-Nb pegmatites in the Kibaran belt of central Africa have been dated earlier only by highly scattered Rb-Sr data that were interpreted to reflect events at 1000 to 900 and 650 to 550 Ma. New U-Pb dating of columbite from the Kivuvu and Ruhembe pegmatites in Burundi precisely determines the age of the mineralization and …
what can we use columbite for. The U-Pb dating of columbite and monazite of the Mayo Salah leucogranite indicates a late-Neoproterozoic magmatic-hydrothermal mineralization event from 603.2 ± 5.3 to 581.6 ± 7.2 Ma, as consistent with both late D2 to D3 events that were recorded in the CAFB in Cameroon, and the associated continental collision …
It provides economic minerals of cassiterite, columbite-tantalite, spodumene, wolframite, monazite as well as some rare earth minerals [4-6]. ... Dewaele, S., Henjes-Kunst, F., Melcher, F., et al. (2011). Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the Gatumba area, Rwanda …
Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the Gatumba area, Rwanda (Central Africa ravi chandra The Mesoproterozoic Kibara belt in Central Africa has recently been redefined and subdivided into the Karagwe–Ankole belt (KAB) and the Kibara belt (KIB), separated by Palaeoproterozoic ...
Dewaele S, Henjes-Kunst F, Melcher F, Sitnikova M, Burgess R, Gerdes A, Fernandez MA, De Clercq F, Muchez P, Lehmann B (2011) Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the Gatumba area, Rwanda (Central Africa). J Afr Earth Sci 61:10–26. Article Google Scholar
Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the Gatumba area, Rwanda (Central Africa) J. African Earth Sci. ... These metasedimentary rocks have been overprinted by Pan-African deformation and greenschist facies metamorphism in the late Neoproterozoic (e.g., Van Daele et al., …
Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the Gatumba area, Rwanda (Central Africa) August …
The pegmatites of the Gatumba area (western Rwanda) have historically been mined for their columbite-tantalite and cassiterite mineralisation, but contain also beryl, apatite, spodumene, amblygonite, and rare phosphates. Columbite-tantalite formed during the crystallisation of the pegmatites, followed by intense alkali metasomatism, i.e ...
Late Neoproterozoic over of the ... African Kibara orogen forms a metallogenic province that hosts a variety of granite-related mineralizations rich in cassiterite, columbite (also called ...
Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the Gatumba area, Rwanda (Central Africa ravi chandra The Mesoproterozoic Kibara belt in Central Africa has recently been redefined and subdivided into the Karagwe–Ankole belt (KAB) and the Kibara belt (KIB), separated by Palaeoproterozoic ...
Dewaele S, Henjes-Kunst F, Melcher F, Sitnikova M, Burgess R, Gerdes A et al. Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing …
The pegmatites are mineralised with columbite-tantalite and cassiterite. Recent investigation by Dewaele et al. (2007a Dewaele et al. (, 2008 indicates that the columbite-tantalite mineralisation ...
Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the Gatumba area, Rwanda (Central Africa) Journal Contribution - Journal …
Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the Gatumba area, Rwanda (Central Africa) S. Dewaele F. Henjes‐Kunst +7 authors B. Lehmann Geology
A number of Sn deposits associated with Neoproterozoic granites are located in the western Jiangnan Orogen of northern Guangxi. The distribution of Sn mineralization is controlled by faults occurring within and around the Neoproterozoic granites. The hydrothermal alteration and mineralization of these Sn deposits exhibit …
Cassiterite and columbite-tantalite mineralization can be found in the more evolved pegmatites, pegmatites of the LCT-type (Lithium Caesium Tantalum)-type according the paragenetic-geochemical classification scheme of Cerny (1991). ... & Lehmann, B., 2011. Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing ...
The chemical and textural features of columbite-tantalite and cassiterite in the Leinster albite-spodumene pegmatites are seen in similar rare element pegmatites and rare metal granites elsewhere ...
Semantic Scholar extracted view of "Geological setting and timing of the cassiterite vein type mineralization of the Kalima area (Maniema, Democratic Republic of Congo)" by S. Dewaele et al. ... which are associated with equigranular to pegmatitic late Mesoproterozoic (1094–755 Ma) granites ... Late Neoproterozoic over of the ...
The 40 Ar- 39 Ar spectra of muscovite samples associated with different steps in the paragenesis of the pegmatites show a spread of apparent ages between ∼940 Ma …
VDOMDHTMLtml>. Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the Gatumba area, Rwanda (Central Africa) The …
Here, we provide cassiterite and columbite-group mineral (CGM) U-Pb ages along with oxide, mica and phosphate mineral compositions for Li-pegmatites from the Fregeneda-Almendra field in order to ...
The No. 31 vein is identified as pegmatite by CMS features. New U–Pb dating CGMs (columbite-tantalite group minerals) in five zones have a consistent age (380 ± 10 Ma). Whilst U–Pb dating of apatite and cassiterite from different structural zones show remarkable two group isotopic ages (370–390 Ma and 145–160 Ma).
Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the Gatumba area, Rwanda (Central Africa) | Semantic …
The Central African Mesoproterozoic Karagwe-Ankole belt in the Great Lakes area (DRCongo, Rwanda, Burundi, Uganda and Tanzania) forms a metallogenic province that hosts a variety of granite-related mineralization, which contains cassiterite, columbite-tantalite, wolframite/ferberite, spodumene and beryl.The Kalima area in the Maniema …
The Mesoproterozoic Kibara orogen in Central Africa hosts different granite-related rare element deposits that contain cassiterite, columbite-tantalite ( coltan ), wolframite, beryl, spodumene, etc. as typical minerals. The primary deposits of these minerals are formed by pegmatites and quartz veins that have historically been related to the youngest, most …
Geology of the cassiterite mineralisation in the Rutongo area, Rwanda (Central Africa): Current state of knowledge. Geol. Belgica. 13, 91-112 Dewaele, S., et al., 2011. Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the Gatumba area, Rwanda (Central Africa). J. Afr. Earth.
Microlite and U-enriched microlite were found in eluvium close to highly weathered granitic pegmatites actively mined as a source of tantalum ore and situated within the ~1000–900 Ma old Kibara belt unit, Numbi mining area, South Kivu province of the Democratic Republic of the Congo. Two examined pegmatites differ in their mineral assemblages and in the …
Coltan 139 and these three columbite-tantalite samples with variable compositions yielded internally consistent LA-ICP-MS U-Pb ages when using each other for calibration and the weighted mean 206 Pb/ 238 U ages are comparable to respective ID-TIMS ages. Composition-dependent U-Pb fractionation seems to be insignificant under …
The major part of the cassiterite mineralisation is, however, concentrated in zones associated with intense phyllic alteration.U–Pb ages of columbite-tantalite samples vary between ∼975Ma and ...
Coltan 139 and these three columbite-tantalite samples with variable compositions yielded internally consistent LA-ICP-MS U-Pb ages when using each other for calibration and the weighted mean 206 Pb/ 238 U ages are comparable to respective ID-TIMS ages. Composition-dependent U-Pb fractionation seems to be insignificant under …
The similar columbite-(Fe) and cassiterite ages demonstrate that these minerals can be precisely dated and could provide useful alternatives to accurately constrain the timing and evolution of rare metal mineralization. ... Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the …
Dewaele, S., Henjes-Kunst, F., Melcher, F., Sitnikova, M., Burgess, R., Gerdes, A., … Lehmann, B. (2011). Late Neoproterozoic over of the cassiterite and ...
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The 40 Ar– 39 Ar spectra of muscovite samples associated with different steps in the paragenesis of the pegmatites show a spread of apparent ages between ∼940 Ma …
Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the Gatumba area, Rwanda (Central Africa) J. Afr. Earth …
In April 2016 Manchester eScholar was replaced by the University of Manchester's new Research Information Management System, Pure. In the autumn the University's …
Few investigations have focused on the potential uses of artisanal gold (Au) mine tailings, despite the fact that artisanal gold mining activity contributes to environmental issues such as greenhouse gas. …
Secondary Ionisation Mass Spectrometry (SIMS) U-Th-Pb dating of cassiterite with very low to sub-ppm U contents, zircon and monazite has provided direct measurements of the ages of Mesoproterozoic–Neoproterozoic pegmatite and quartz vein Sn mineralisation in the Karagwe–Ankole Belt (KAB), Rwanda, and through dates on …
Late Neoproterozoic over of the cassiterite and columbite-tantalite bearing pegmatites of the Gatumba area, Rwanda (Central Africa) Journal Contribution - Journal Article ...