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Journal Article

Ferro-pedrizite, NaLi 2 (Fe 2 + 2 Al 2 Li)Si 8 O 22 (OH) 2 , a new amphibole-supergroup mineral from the Sutlug pegmatite, Tyva Republic, Russia Available to Purchase

Sergey I. Konovalenko, Sergey A. Ananyev, Nikita V. Chukanov, Sergey M. Aksenov, Ramiza K. Rastsvetaeva, Anatoliy I. Bakhtin, Anatoliy G. Nikolaev, Ramil R. Gainov, Farit G. Vagizov, Anatoliy N. Sapozhnikov, Dmitriy I. Belakovskiy, Yana V. Bychkova, Göstar KlingelhÖfer, Mathias Blumers
Published: 01 June 2015
European Journal of Mineralogy (2015) 27 (3): 417–426.
DOI: https://doi.org/10.1127/ejm/2015/0027-2438
...: Ferro-pedrizite, a new amphibole-supergroup mineral was discovered in the Sutlug pegmatite occurrence situated in the Targi River Basin, Tyva Republic, Eastern Sibera, Russia. The associated minerals are quartz, albite, microcline, spodumene, cassiterite, beryl, columbite-(Mn), fergusonite-β-(Y...
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View PDF for article title, Ferro-pedrizite, NaLi 2 (Fe 2 + 2 Al 2 Li)Si 8 O 22 (OH) 2 , a new amphibole-supergroup mineral from the <span class="search-highlight">Sutlug</span> <span class="search-highlight">pegmatite</span>, Tyva Republic, Russia
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Image
Contents of trace elements (Y) (a) and ΣREE (b) and Na2O/K2O ratio (c) in spodumene pegmatites from different SSB fields depending on their contents of Li. Pegmatite fields: 1, Burchin and Sutlug; 2, Khusuingol; 3, Kharty.

Contents of trace elements (Y) ( a ) and ΣREE ( b ) and Na 2 O/K 2 O ratio ... Available to Purchase

Published: 01 December 2018
Fig. 11. Contents of trace elements (Y) ( a ) and ΣREE ( b ) and Na 2 O/K 2 O ratio ( c ) in spodumene pegmatites from different SSB fields depending on their contents of Li. Pegmatite fields: 1 , Burchin and Sutlug; 2 , Khusuingol; 3 , Kharty.
Image
Chondrite-normalized (Sun and McDonough, 1989) REE patterns of: a: 1, granites of major phase of the Kystarys complex; 2–4, spodumene pegmatites from different SSB fields: 2, Kharty, 3, Khusuingol, 4, Burchin and Sutlug; b, rocks from the Kharty pegmatite field: 1, alkali aegirine granites, 2, metasomatites developed after monzonites, 3, spodumene pegmatites with amazonite.

Chondrite-normalized ( Sun and McDonough, 1989 ) REE patterns of: a : 1 ,... Available to Purchase

Published: 01 December 2018
Fig. 7. Chondrite-normalized ( Sun and McDonough, 1989 ) REE patterns of: a : 1 , granites of major phase of the Kystarys complex; 2–4 , spodumene pegmatites from different SSB fields: 2 , Kharty, 3 , Khusuingol, 4 , Burchin and Sutlug; b , rocks from the Kharty pegmatite field: 1
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Average-crust-normalized (Rudnick and Gao, 2003) multielement patterns of granites of major phase of the Kystarys complex (from three massifs) and spodumene pegmatites from different SSB fields. 1–3, spodumene pegmatites from different fields: 1, Burchin and Sutlug, 2, Khusuingol, 3, Kharty; 4, granites of major phase from three massifs.

Average-crust-normalized ( Rudnick and Gao, 2003 ) multielement patterns of... Available to Purchase

Published: 01 December 2018
Fig. 9. Average-crust-normalized ( Rudnick and Gao, 2003 ) multielement patterns of granites of major phase of the Kystarys complex (from three massifs) and spodumene pegmatites from different SSB fields. 1–3 , spodumene pegmatites from different fields: 1 , Burchin and Sutlug, 2 , Khusuingol
Journal Article

Fluoro-sodic-ferropedrizite, NaLi 2 ( \batchmode \documentclass[fleqn,10pt,legalpaper]{article} \usepackage{amssymb} \usepackage{amsfonts} \usepackage{amsmath} \pagestyle{empty} \begin{document} \(\mathrm{Fe}_{2}^{2+}\) \end{document} Al 2 Li)Si 8 O 22 F 2 , a new mineral of the amphibole group from the Sutlug River, Tuva Republic, Russia: description and crystal structure Available to Purchase

R. Oberti, M. Boiocchi, N. A. Ball, F. C. Hawthorne
Published: 01 June 2009
Mineralogical Magazine (2009) 73 (3): 487–494.
DOI: https://doi.org/10.1180/minmag.2009.073.3.487
...+}\) \end{document} Al 2 Li) T Si 8 O 22 W F 2 , is a new mineral of the amphibole group from the Sutlug River, Tuva Republic, Russia. It occurs at the endogenic contact of a Li-pegmatite with country rocks near to a diabase dyke and formed by reaction of the pegmatitic melt with the country rock. Fluoro...
View PDF for article title, Fluoro-sodic-ferropedrizite, NaLi 2 ( \batchmode \documentclass[fleqn,10pt,legalpaper]{article} \usepackage{amssymb} \usepackage{amsfonts} \usepackage{amsmath} \pagestyle{empty} \begin{document} \(\mathrm{Fe}_{2}^{2+}\) \end{document} Al 2 Li)Si 8 O 22 F 2 , a new mineral of the amphibole group from the <span class="search-highlight">Sutlug</span> River, Tuva Republic, Russia: description and crystal structure
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Add to Citation Manager for Fluoro-sodic-ferropedrizite, NaLi 2 ( \batchmode \documentclass[fleqn,10pt,legalpaper]{article} \usepackage{amssymb} \usepackage{amsfonts} \usepackage{amsmath} \pagestyle{empty} \begin{document} \(\mathrm{Fe}_{2}^{2+}\) \end{document} Al 2 Li)Si 8 O 22 F 2 , a new mineral of the amphibole group from the <span class="search-highlight">Sutlug</span> River, Tuva Republic, Russia: description and crystal structure
Image
Schematic map of the localization of Early Paleozoic granite complexes and vein series of rare-element pegmatites on the Sangilen Highland (Tyva Republic), after Rudenko (2010), refined and supplemented. Inset shows the locality of the study objects. 1, 2, Naryn monometamorphic complex of the Tuva–Mongolian massif (V–Ꞓ1): 1, carbonate and terrigenous-carbonate strata; 2, metaterrigenous strata; 3–5, fields of Early Paleozoic intrusions of: 3, Tserigiingol complex (Ꞓ1–2), 4, Tannu-Ola complex (Ꞓ3–O1), 5, Argolik and Kystarys complexes (Ꞓ3–O1); 6–7, fields of Middle Paleozoic intrusions of: 6, Bren’ complex (D1); 7, Sangilen complex (D1); 8, fault zones; 9, fields of Li-pegmatites. Arabic numerals mark the largest occurrences of Li-pegmatites: South Sangilen pegmatite belt (SSB) (Ꞓ3–O1): 1, 2, Tastyg and Pichi-Tastyg deposits of the Khusuingol field, 3, occurrences in the Burchin field, 4, occurrences in the Sutlug field, 5, occurrences in the Kharty field; Central Sangilen pegmatite belt (CSB) (P3): 6, 7, Kara-Adyr and Shuk-Byul’ occurrences in the Sol’bel’der field. Roman numerals stand for the granite plutons of the Kystarys complex (Ꞓ3–O1): I, Dzos-Khusuingol, II, Uchuglyk, III, Temenchulu, V, Bystraya–Kargy; IV, Verkhnii Tserigiingol massif of the Tserigiingol complex (Ꞓ1–2). Outlined are SSB pegmatite fields with different trace-element signatures: Burchin and Sutlug fields (LCT) in the middle part of the SSB and Khusuingol and Kharty fields (LCT–NIF) in the east and west of the SSB, respectively. The latter two fields are shown in more detail in Figs. 2 and 3.

Schematic map of the localization of Early Paleozoic granite complexes and ... Available to Purchase

Published: 01 December 2018
of the Khusuingol field, 3, occurrences in the Burchin field, 4, occurrences in the Sutlug field, 5, occurrences in the Kharty field; Central Sangilen pegmatite belt (CSB) (P3): 6 , 7 , Kara-Adyr and Shuk-Byul’ occurrences in the Sol’bel’der field. Roman numerals stand for the granite plutons of the Kystarys
Journal Article

Interaction of crustal and mantle materials, sources of trace elements during the formation and evolution of Early Paleozoic Li-rich granite–pegmatite systems in southeastern Tuva Available to Purchase

L.G. Kuznetsova
Published: 01 December 2018
Russ. Geol. Geophys. (2018) 59 (12): 1660–1678.
DOI: https://doi.org/10.1016/j.rgg.2018.12.010
...Fig. 11. Contents of trace elements (Y) ( a ) and ΣREE ( b ) and Na 2 O/K 2 O ratio ( c ) in spodumene pegmatites from different SSB fields depending on their contents of Li. Pegmatite fields: 1 , Burchin and Sutlug; 2 , Khusuingol; 3 , Kharty. ...
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View PDF for article title, Interaction of crustal and mantle materials, sources of trace elements during the formation and evolution of Early Paleozoic Li-rich granite–<span class="search-highlight">pegmatite</span> systems in southeastern Tuva
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Distribution of Early Paleozoic granite complexes and vein series of rare-metal pegmatites in the Sangilen Highland (Tyva), after (Rudenko, 2010). 1, 2, Naryn monometamorphic complex of the Tuva–Mongolian microcontinent (V–Є1): 1, carbonate and terrigenous carbonate sediments; 2, metaterrigenous sediments; 3–6, fields of Early Paleozoic intrusions: 3, Tannuola complex (Є2); 4, Argolik, Sarkhoi, and Kys-Tarys complexes (Є3–O1); 5, Bren’ complex (D1); 6, Sangilen complex (D1); 7, fault zones; 8, areas of Li pegmatites. 1–7, largest occurrences of Li pegmatites: 1–5, South Sangilen pegmatite belt (Tastyg (1), Pichi-Tastyg (2), Burchin Group (3), Sutlug (4), Khartyn (5)); 6, 7, Central Sangilen belt (Kara-Adyr (6), Shuk-Byul’ (7)); I–III, granite plutons of the Kys-Tarys complex: I, Dzos–Khusuingol; II, Tumenchulu; III, Solbelder.

Distribution of Early Paleozoic granite complexes and vein series of rare-m... Available to Purchase

Published: 01 February 2014
of Li pegmatites: 1–5, South Sangilen pegmatite belt (Tastyg (1), Pichi-Tastyg (2), Burchin Group (3), Sutlug (4), Khartyn (5)); 6, 7, Central Sangilen belt (Kara-Adyr (6), Shuk-Byul’ (7)); I–III, granite plutons of the Kys-Tarys complex: I, Dzos–Khusuingol; II, Tumenchulu; III, Solbelder.
Journal Article

Large fields of spodumene pegmatites in the settings of rifting and postcollisional shear–pull-apart dislocations of continental lithosphere Available to Purchase

V.Ye. Zagorsky, A.G. Vladimirov, V.M. Makagon, L.G. Kuznetsova, S.Z. Smirnov, B.A. D’yachkov, I.Yu. Annikova, S.P. Shokalsky, A.N. Uvarov
Published: 01 February 2014
Russ. Geol. Geophys. (2014) 55 (2): 237–251.
DOI: https://doi.org/10.1016/j.rgg.2014.01.008
... of Li pegmatites: 1–5, South Sangilen pegmatite belt (Tastyg (1), Pichi-Tastyg (2), Burchin Group (3), Sutlug (4), Khartyn (5)); 6, 7, Central Sangilen belt (Kara-Adyr (6), Shuk-Byul’ (7)); I–III, granite plutons of the Kys-Tarys complex: I, Dzos–Khusuingol; II, Tumenchulu; III, Solbelder. ...
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View PDF for article title, Large fields of spodumene <span class="search-highlight">pegmatites</span> in the settings of rifting and postcollisional shear–pull-apart dislocations of continental lithosphere
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Journal Article

The Age, Composition, and Provenances of Terrigenous Rocks in the South of the Sangilen Block of the Central Asian Orogenic Belt Available to Purchase

L.G. Kuznetsova, S.I. Dril’, S.I. Shkol’nik
Published: 01 March 2024
Russ. Geol. Geophys. (2024) 65 (3): 326–344.
DOI: https://doi.org/10.2113/RGG20234622
... from the eastern segment of the SB (Tserigiyn-Gol River basin, sampling sites III and IV) are much more silicic than those from the western and central segments (area from the source of the Marat Brook to the source of the Sutlug Brook, sites I and II). Minimum contents (wt.%) of SiO 2 (60–64...
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Journal Article

New Mineral Names Available to Purchase

Paula C. Piilonen, Glenn Poirier
Published: 01 August 2010
American Mineralogist (2010) 95 (8-9): 1357–1361.
DOI: https://doi.org/10.2138/am.2010.565
... the endogenic contact of a lithium pegmatite with country rock and formed by reaction of the pegmatitic melt with the country rock. The sample comes from the collection of the Fersman Mineralogical Museum (64715) and the collection location was given as Sutlug River, Tuva Republic, Russia. The species and name...
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New Mineral Names, Free

Dmitriy I. Belakovskiy, Fernando Cámara, Olivier C. Gagne, Yulia Uvarova
Published: 01 July 2016
American Mineralogist (2016) 101 (7): 1709–1716.
DOI: https://doi.org/10.2138/am-2016-NMN101714
... ( Fe 2 2 + Al 2 Li ) Si 8 O 22 ( OH ) 2 , a new amphibole-supergroup mineral from the Sutlug pegmatite, Tyva Republic, Russia. European Journal of Mineralogy, 27, 417–426. Ferro-pedrizite (IMA2014-037), ideally NaLi 2 ( Fe 2 2...
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