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Mineralogical and chemical evolution of tantalum-(niobium-tin) mineralisation in pegmatites and granites. Part 2: Worldwide examples (excluding Africa) and an overview of global metallogenetic patterns. / Melcher, F.; Graupner, T.; Gäbler, H.-E.; Sitnikova, M.; Oberthür, T.; Gerdes, A.; Badanina, E.; Chudy, T.

In: Ore Geology Reviews, Vol. 89, 10.2017, p. 946-987.

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Melcher, F. ; Graupner, T. ; Gäbler, H.-E. ; Sitnikova, M. ; Oberthür, T. ; Gerdes, A. ; Badanina, E. ; Chudy, T. / Mineralogical and chemical evolution of tantalum-(niobium-tin) mineralisation in pegmatites and granites. Part 2: Worldwide examples (excluding Africa) and an overview of global metallogenetic patterns. In: Ore Geology Reviews. 2017 ; Vol. 89. pp. 946-987.

BibTeX

@article{01288b361d6b4ea1b3e677e64484311b,
title = "Mineralogical and chemical evolution of tantalum-(niobium-tin) mineralisation in pegmatites and granites. Part 2: Worldwide examples (excluding Africa) and an overview of global metallogenetic patterns",
abstract = "{\textcopyright} 2016 Elsevier B.V.Columbite-group minerals (CGM) account for the majority of the production of tantalum, an important metal for high-technology applications. Along with other Ta-Nb oxides such as tapiolite, wodginite, ixiolite and pyrochlore supergroup minerals, CGM are recovered from rare-metal granites and granitic rare-element pegmatites. In this paper mineralogical and geochemical data with a focus on CGM, tapiolite, wodginite and ixiolite are presented for rare-element granites and pegmatites from worldwide occurrences except Africa that has been covered in a previous contribution (Melcher et al., 2015). Major and trace element data of the Ta-Nb oxides are presented and compared for a total of 25 granite/pegmatite provinces, and one carbonatite for comparison. Based on CGM compositions, the data allow to distinguish between various subgroups of Li-Cs-Ta (LCT)-family pegmatites, Nb-Y-F (NYF)-family pegmatites, mixed LCT-NYF pegmatites, and rare-element granites.Each period of Ta-ore formation in Earth h",
author = "F. Melcher and T. Graupner and H.-E. G{\"a}bler and M. Sitnikova and T. Oberth{\"u}r and A. Gerdes and E. Badanina and T. Chudy",
year = "2017",
month = oct,
doi = "10.1016/j.oregeorev.2016.03.014",
language = "English",
volume = "89",
pages = "946--987",
journal = "Ore Geology Reviews",
issn = "0169-1368",
publisher = "Elsevier",

}

RIS

TY - JOUR

T1 - Mineralogical and chemical evolution of tantalum-(niobium-tin) mineralisation in pegmatites and granites. Part 2: Worldwide examples (excluding Africa) and an overview of global metallogenetic patterns

AU - Melcher, F.

AU - Graupner, T.

AU - Gäbler, H.-E.

AU - Sitnikova, M.

AU - Oberthür, T.

AU - Gerdes, A.

AU - Badanina, E.

AU - Chudy, T.

PY - 2017/10

Y1 - 2017/10

N2 - © 2016 Elsevier B.V.Columbite-group minerals (CGM) account for the majority of the production of tantalum, an important metal for high-technology applications. Along with other Ta-Nb oxides such as tapiolite, wodginite, ixiolite and pyrochlore supergroup minerals, CGM are recovered from rare-metal granites and granitic rare-element pegmatites. In this paper mineralogical and geochemical data with a focus on CGM, tapiolite, wodginite and ixiolite are presented for rare-element granites and pegmatites from worldwide occurrences except Africa that has been covered in a previous contribution (Melcher et al., 2015). Major and trace element data of the Ta-Nb oxides are presented and compared for a total of 25 granite/pegmatite provinces, and one carbonatite for comparison. Based on CGM compositions, the data allow to distinguish between various subgroups of Li-Cs-Ta (LCT)-family pegmatites, Nb-Y-F (NYF)-family pegmatites, mixed LCT-NYF pegmatites, and rare-element granites.Each period of Ta-ore formation in Earth h

AB - © 2016 Elsevier B.V.Columbite-group minerals (CGM) account for the majority of the production of tantalum, an important metal for high-technology applications. Along with other Ta-Nb oxides such as tapiolite, wodginite, ixiolite and pyrochlore supergroup minerals, CGM are recovered from rare-metal granites and granitic rare-element pegmatites. In this paper mineralogical and geochemical data with a focus on CGM, tapiolite, wodginite and ixiolite are presented for rare-element granites and pegmatites from worldwide occurrences except Africa that has been covered in a previous contribution (Melcher et al., 2015). Major and trace element data of the Ta-Nb oxides are presented and compared for a total of 25 granite/pegmatite provinces, and one carbonatite for comparison. Based on CGM compositions, the data allow to distinguish between various subgroups of Li-Cs-Ta (LCT)-family pegmatites, Nb-Y-F (NYF)-family pegmatites, mixed LCT-NYF pegmatites, and rare-element granites.Each period of Ta-ore formation in Earth h

U2 - 10.1016/j.oregeorev.2016.03.014

DO - 10.1016/j.oregeorev.2016.03.014

M3 - Article

VL - 89

SP - 946

EP - 987

JO - Ore Geology Reviews

JF - Ore Geology Reviews

SN - 0169-1368

ER -

ID: 3999498