Skip Nav Destination
Close Modal
![Geological outlines of the Chakhyrtoi area (Sangilen Upland). 1 – shales of the Cholda Formation; 2 – limestones of the Canyon Formation; 3 – effusives; 4 – dolomites; 5 – limestones; 6 – limestones alternating with shales; 7 – shales, sometimes effusives; 8 – hyperbasite bodies; 9 – foraminifer findings; 10 – dips and strikes; 11 – faults: a – established, b – supposed; 12 – indices of formations: cl – Cholda; kn – Canyon; ch – Chakhyrtoi.]()
![First thumbnail for: Mantle–Crustal Nature of Early Paleozoic Alkaline ...]()
![Second thumbnail for: Mantle–Crustal Nature of Early Paleozoic Alkaline ...]()
![Third thumbnail for: Mantle–Crustal Nature of Early Paleozoic Alkaline ...]()
![First thumbnail for: The age of camptonite dikes of the Agardag alkali-...]()
![Second thumbnail for: The age of camptonite dikes of the Agardag alkali-...]()
![Third thumbnail for: The age of camptonite dikes of the Agardag alkali-...]()
![First thumbnail for: FINDINGS OF FORAMINIFERS IN “ANCIENT” DEPOSITS OF ...]()
![Second thumbnail for: FINDINGS OF FORAMINIFERS IN “ANCIENT” DEPOSITS OF ...]()
![Third thumbnail for: FINDINGS OF FORAMINIFERS IN “ANCIENT” DEPOSITS OF ...]()
![The range of δ18О values for minerals and rocks of alkaline plutons of the Sangilen upland. The “mantle” range values (δ18ОSMOW = 5.5 ± 0.5‰) are given after Taylor and Sheppard (1986). Designations follow Fig. 4.]()
![Geologic position and internal structure of intrusive alkaline massifs of the Sangilen upland. a, Fragment of a schematic map of the geologic structure of Western and Central Sangilen, after Gibsher et al. (2000). Inset shows the geographic location of the region; b–e, schematic geological maps of the Dakhu-Nur (b), Bayan-Kol (c), Chik (d), and Kharly (e) plutons (Kononova, 1957, 1962, 1976; Yashina, 1982; Andreeva et al., 1984; Vrublevskii et al., 2014b). 1, Cenozoic superposed basins; 2, Neoproterozoic complexes of metamorphic rocks (schists, gneisses, marbles, and quartzites) in the basement of the Tuva–Mongolian microcontinent; 3, continent-marginal complexes of Late Riphean–Vendian and Cambrian metamorphosed carbonate-terrigenous and volcanic rocks of Central Sangilen; 4, Vendian–Early Cambrian tectonic fragments (I, Agardag zone, II, Kaa-Khem zone) of back-arc basins, composed of pillow lavas, siliceous and turbidite deposits with serpentinite melange, and cutting gabbro-plagiogranites; 5, Vendian–Cambrian island-arc complexes (calc-alkalic volcanics, carbonate deposits, and gabbro-tonalite–plagiogranite intrusions) of the East Tannu-Ola structural-formation zone and intruding Late Cambrian–Ordovician collisional granitoid batholiths; 6, faults (a) and borders of nappe structures (b), 7, location of alkali massifs (1, Kharly, 2, Bayan-Kol, 3, Dakhu-Nur, 4, Chik), 8–13, igneous rocks: 8, jacupirangite–melteigites, 9, ijolites, ijolite-urtites, and urtites, 10, nepheline syenites (foyaites), 11, juvites (feldspathic urtites), 12, zones of carbonatization and endogenous carbonate rocks; 13, sites of pegmatoid alkaline rocks.]()
![Location of key sections of Neoproterozoic deposits in the structure of the Altai-Sayan Folded Area (after [66]; simplified). 1 — Siberian Platform; 2 — microcontinents and their blocks: D — Derba, K-A — Kan-Arzybei, Sh — Shutkhulai, G — Gargan, Kh — Khamar-Daban, S — Sangilen, K — Kaa-Khem, A-M — Altai-Mongolia; 3 — Riphean-Vendian structures; 4 — Vendian-Cambrian structures; 5 — overlapped depressions; 6 — undifferentiated terrane structures of the West Sayans; 7 — boundaries of the main structural elements; 8 — locations and numbers of reference sections of Neoproterozoic deposits (see Fig. 2): 1, 2 — northwestern East Sayans (Mana through): 1 — Goryunov ravine, 2 — Mana, Zhistyk, and Ungut Rivers; 3–5 — southeastern East Sayans: 3 — Sarkhoi, Ukha-Gol, and Bokson Rivers, 4 — Sarkhoi and Muya-Gol Rivers, 5 — Gorlyk and Shumak Rivers; 6 — Gornaya Shoria, Mrassu River; 7–10 — Kuznetsk Alatau: 7 — Kiya River downstream from the mouth of the Kundat Brook, 8 — Azyrtal Ridge, Kuten’-Buluk ravine, Mt. Charyshtag, 9 — Belyi Iyus River basin, Kharatas Brook, Synnig ravine, Mt. Amar, 10 — Son River basin (Podtemny ravine); 11 — Gorny Altai, Katun’ and Edigan Rivers; 12 — Southeastern Tuva (Sangilen Upland), Erzin, Naryn, and Balyktyg-Khem Rivers; 13 — Gargan Block, Irkutny Gargan and Zhakhoi Rivers; 14 — Kuznetsk Alatau, Tom’ River; 15 — southeastern East Sayans, Dibi and Khazalkha Rivers.]()
![Carbon and oxygen isotope composition of rocks of alkaline complexes and the host metacarbonate deposits. a, δ13С–δ18О diagram: PIC, domain of primary magmatogene carbonatites (Conway and Taylor, 1969); NSC, marine sedimentary carbonates (Pokrovskii, 2000). Arrows show the influence of crustal contamination and low-temperature hydrotherms (Demény et al., 1998). МСС, assumed field of mantle–crustal carbonatites (Vrublevskii, 2017). Gray fields mark predominant calcite/dolomite compositions in carbonatites of Kuznetsk Alatau, Central Tuva (CT), and Turkestan–Alai segment of the Tien Shan (TSh) (Nikiforov et al., 2006; Vrublevskii, 2015; Vrublevskii et al., 2018c). Mongolian car-bonatites are represented by dikes, veins, breccias, and tuffs of the Mushgai Hudag and Ulgei Hiyd complexes (Kuleshov, 1986). b, δ18О– 87Sr/86Sr(T) diagram. c, Fractionation of oxygen isotopes between calcite and apatite in carbonatites and carbonatite-like rocks. For calculation of equilibrium temperatures see Notes to Table 3. Apt, apatite, Cс, calcite. Data on carbonatites of Brazil, Angola, Siberia, and the South Tien Shan are after Santos and Clayton (1995), Alberti et al. (1999), Vrublevskii and Gertner (2005), and Vrublevskii et al. (2018c). Sangilen upland: 1, calcite of alkaline rocks, 2, carbonatite-like rocks, 3, hydrothermal veins of calcite, 4, limestones and marbles. Temperatures of apatite–calcite isotope equilibrium: 5, carbonatite-like rocks of Sangilen, 6, carbonatites of Angola, 7, carbonatites of Siberia and the South Tien Shan, 8, carbonatites of Brazil (Jacupiranga).]()
![Nd–Sr–Pb isotope composition of alkaline and carbonatite-like rocks of the Sangilen upland. a, εNd(T)–εSr(T) diagram. For comparison, the predominant compositions (gray fields) of igneous rocks of alkaline and carbonatite complexes of the CAOB (Mesozoic: 1, southern Mongolia, 2, western Transbaikalia; Paleozoic: 3, Vitim province of western Transbaikalia and northern Mongolia, 4, Kuznetsk Alatau) and the Precambrian Siberian, European, and North American Cratons (5) are shown (Nikiforov et al., 2002; Vrublevskii et al., 2003b; Vladykin, 2005; Vrublevskii and Gertner, 2005 (and references there); Sazonov et al., 2007; Doroshkevich et al., 2012; Vrublevskii, 2015). Localization of the PREMA, HIMU, EM 1, and EM 2 reservoirs is given in accordance with their present-day isotope parameters (Zindler and Hart, 1986; Stracke et al., 2005). Rocks: 1, alkaline, 2, carbonatite-like. b, c, Primary 207Pb/204Pb–206Pb/204Pb (b) and 208Pb/206Pb–207Pb/206Pb (c) ratios in microcline (black asterisk) from calcite veins of the Kharly pluton. The average composition of the mantle components PREMA, HIMU, DMM, EM-1, and EM-2, plumbotectonics model, and Pb isotope evolution (UC, upper crust, Oro, orogeny, M, mantle) (Stacey and Kramers, 1975; Zartman and Doe, 1981; Zindler and Hart, 1986; Hart et al., 1992; Stracke et al., 2005; Armienti and Gasperini, 2007) are shown; EACL, East African carbonatite line (Bell and Tilton, 2001); KA&GA, alkaline rocks and carbonatites of Kuznetsk Alatau and Gorny Altai in the western CAOB (Vrublevskii et al., 2017, 2018b).]()
![First thumbnail for: NEOPROTEROZOIC STRATIGRAPHY OF THE ALTAI-SAYAN FOL...]()
![Second thumbnail for: NEOPROTEROZOIC STRATIGRAPHY OF THE ALTAI-SAYAN FOL...]()
![First thumbnail for: RUBIDIUM-STRONTIUM DATING OF ALKALI GRANITES IN NO...]()
![Second thumbnail for: RUBIDIUM-STRONTIUM DATING OF ALKALI GRANITES IN NO...]()
![Third thumbnail for: RUBIDIUM-STRONTIUM DATING OF ALKALI GRANITES IN NO...]()
![First thumbnail for: Estimation of heat flow in Tuva from data on heliu...]()
![Second thumbnail for: Estimation of heat flow in Tuva from data on heliu...]()
![Third thumbnail for: Estimation of heat flow in Tuva from data on heliu...]()
![First thumbnail for: Ferro-pedrizite, NaLi 2 (Fe 2 + 2 Al 2 Li)Si 8 O 2...]()
![Second thumbnail for: Ferro-pedrizite, NaLi 2 (Fe 2 + 2 Al 2 Li)Si 8 O 2...]()
![Third thumbnail for: Ferro-pedrizite, NaLi 2 (Fe 2 + 2 Al 2 Li)Si 8 O 2...]()
![First thumbnail for: Geochemistry, isotope triad (Nd–Sr–O), and 40 Ar– ...]()
![Second thumbnail for: Geochemistry, isotope triad (Nd–Sr–O), and 40 Ar– ...]()
![Third thumbnail for: Geochemistry, isotope triad (Nd–Sr–O), and 40 Ar– ...]()
![First thumbnail for: GRANITOID MAGMATISM OF WESTERN <span class="search...]()
![Second thumbnail for: GRANITOID MAGMATISM OF WESTERN <span class="search...]()
![Third thumbnail for: GRANITOID MAGMATISM OF WESTERN <span class="search...]()
![First thumbnail for: The tectonomagmatic evolution of structure-litholo...]()
![Second thumbnail for: The tectonomagmatic evolution of structure-litholo...]()
![Third thumbnail for: The tectonomagmatic evolution of structure-litholo...]()
![First thumbnail for: Sillimanite group minerals: a new promising raw ma...]()
![Second thumbnail for: Sillimanite group minerals: a new promising raw ma...]()
![Third thumbnail for: Sillimanite group minerals: a new promising raw ma...]()
![First thumbnail for: Late Cambrian-Ordovician tectonics and geodynamics...]()
![Second thumbnail for: Late Cambrian-Ordovician tectonics and geodynamics...]()
![Third thumbnail for: Late Cambrian-Ordovician tectonics and geodynamics...]()
![First thumbnail for: Metallogeny of Endogenous Gold in Tuva]()
![Second thumbnail for: Metallogeny of Endogenous Gold in Tuva]()
![Third thumbnail for: Metallogeny of Endogenous Gold in Tuva]()
![First thumbnail for: THE OKA PLATEAU IN THE NEOTECTONIC FRAMEWORK OF SO...]()
![Second thumbnail for: THE OKA PLATEAU IN THE NEOTECTONIC FRAMEWORK OF SO...]()
![Third thumbnail for: THE OKA PLATEAU IN THE NEOTECTONIC FRAMEWORK OF SO...]()
1-20 OF 40 RESULTS FOR
Sangilen Upland
Results shown limited to content with bounding coordinates.
Follow your search
Access your saved searches in your account
Would you like to receive an alert when new items match your search?
1
Image
Geological outlines of the Chakhyrtoi area (Sangilen Upland). 1 – shales ... Available to Purchase
in FINDINGS OF FORAMINIFERS IN “ANCIENT” DEPOSITS OF EAST SAYAN, TUVA, AND GORNY ALTAI ( Late Precambrian?-Paleozoic )
> Russian Geology and Geophysics
Published: 01 March 1997
Fig. 2. Geological outlines of the Chakhyrtoi area (Sangilen Upland). 1 – shales of the Cholda Formation; 2 – limestones of the Canyon Formation; 3 – effusives; 4 – dolomites; 5 – limestones; 6 – limestones alternating with shales; 7 – shales, sometimes effusives; 8 – hyperbasite
Journal Article
Mantle–Crustal Nature of Early Paleozoic Alkaline Intrusions in Central Sangilen, Tuva (from Nd, Sr, Pb, C, and O Isotope Data) Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 May 2019
Russ. Geol. Geophys. (2019) 60 (5): 451–462.
...V.V. Vrublevskii; A.V. Nikiforov; A.M. Sugorakova; T.V. Kozulina Abstract —The Paleozoic foidolite–foyaite plutons of the Sangilen upland (Bayan-Kol, Dakhu-Nur, Chik, and Kharly ones) might have formed in the Late Cambrian–Early Ordovician (~490–500 Ma, Sm–Nd and U–Pb); they are the result...
FIGURES
Journal Article
The age of camptonite dikes of the Agardag alkali-basalt complex ( western Sangilen ): results of Ar/Ar and U/Pb dating Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 August 2012
Russ. Geol. Geophys. (2012) 53 (8): 763–775.
...A.A. Gibsher; V.G. Malkovets; A.V. Travin; E.A. Belousova; V.V. Sharygin; Z. Konc Abstract A camptonite dike swarm (Agardag alkali-basalt complex) in the western part of the Sangilen Upland abounds in mantle xenoliths. Mineralogical, petrographic, and petrochemical studies show that the dikes...
FIGURES
Journal Article
FINDINGS OF FORAMINIFERS IN “ANCIENT” DEPOSITS OF EAST SAYAN, TUVA, AND GORNY ALTAI ( Late Precambrian?-Paleozoic ) Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 March 1997
Russ. Geol. Geophys. (1997) 38 (3): 661–668.
...Fig. 2. Geological outlines of the Chakhyrtoi area (Sangilen Upland). 1 – shales of the Cholda Formation; 2 – limestones of the Canyon Formation; 3 – effusives; 4 – dolomites; 5 – limestones; 6 – limestones alternating with shales; 7 – shales, sometimes effusives; 8 – hyperbasite...
FIGURES
Image
The range of δ 18 О values for minerals and rocks of alkaline plutons of th... Available to Purchase
in Mantle–Crustal Nature of Early Paleozoic Alkaline Intrusions in Central Sangilen, Tuva (from Nd, Sr, Pb, C, and O Isotope Data)
> Russian Geology and Geophysics
Published: 01 May 2019
Fig. 5. The range of δ 18 О values for minerals and rocks of alkaline plutons of the Sangilen upland. The “mantle” range values (δ 18 О SMOW = 5.5 ± 0.5‰) are given after Taylor and Sheppard ( 1986 ). Designations follow Fig. 4 .
Image
Geologic position and internal structure of intrusive alkaline massifs of t... Available to Purchase
in Mantle–Crustal Nature of Early Paleozoic Alkaline Intrusions in Central Sangilen, Tuva (from Nd, Sr, Pb, C, and O Isotope Data)
> Russian Geology and Geophysics
Published: 01 May 2019
Fig. 1. Geologic position and internal structure of intrusive alkaline massifs of the Sangilen upland. a , Fragment of a schematic map of the geologic structure of Western and Central Sangilen, after Gibsher et al. ( 2000 ). Inset shows the geographic location of the region; b–e , schematic
Image
![Location of key sections of Neoproterozoic deposits in the structure of the Altai-Sayan Folded Area (after [66]; simplified). 1 — Siberian Platform; 2 — microcontinents and their blocks: D — Derba, K-A — Kan-Arzybei, Sh — Shutkhulai, G — Gargan, Kh — Khamar-Daban, S — Sangilen, K — Kaa-Khem, A-M — Altai-Mongolia; 3 — Riphean-Vendian structures; 4 — Vendian-Cambrian structures; 5 — overlapped depressions; 6 — undifferentiated terrane structures of the West Sayans; 7 — boundaries of the main structural elements; 8 — locations and numbers of reference sections of Neoproterozoic deposits (see Fig. 2): 1, 2 — northwestern East Sayans (Mana through): 1 — Goryunov ravine, 2 — Mana, Zhistyk, and Ungut Rivers; 3–5 — southeastern East Sayans: 3 — Sarkhoi, Ukha-Gol, and Bokson Rivers, 4 — Sarkhoi and Muya-Gol Rivers, 5 — Gorlyk and Shumak Rivers; 6 — Gornaya Shoria, Mrassu River; 7–10 — Kuznetsk Alatau: 7 — Kiya River downstream from the mouth of the Kundat Brook, 8 — Azyrtal Ridge, Kuten’-Buluk ravine, Mt. Charyshtag, 9 — Belyi Iyus River basin, Kharatas Brook, Synnig ravine, Mt. Amar, 10 — Son River basin (Podtemny ravine); 11 — Gorny Altai, Katun’ and Edigan Rivers; 12 — Southeastern Tuva (Sangilen Upland), Erzin, Naryn, and Balyktyg-Khem Rivers; 13 — Gargan Block, Irkutny Gargan and Zhakhoi Rivers; 14 — Kuznetsk Alatau, Tom’ River; 15 — southeastern East Sayans, Dibi and Khazalkha Rivers.](https://gsw.silverchair-cdn.com/gsw/Content_public/Journal/rgg/45/3/rgg-450295/2/s_s01mar04_page_3_1.jpeg?Expires=2147483647&Signature=cKrzXkbrUh3jkBAF6C2g9pvaD7UABVBuGWSInzKQp-e5QBUe3cFEqf7oWNtimgUxgG8xf7TUWTAapE56c9RXKlIrD1Hk4SCWQHXuAifPX1UfKqCIgHGsXaVfcSKPrGz74tcCC1-WvEhgvKw8lwDqfWbiZpLCkDZukW0xdP4np9qDxlxFvZ2AZ303N2Ys9E7oU3OetiUzmj3TWKOnoA3X9qLqDbvSgdNG3rhHhR9RUn2WV4jUDgz3TPXoAkGbPU~nEoiQi0sQdOnpnAX659OiPvKdKW-Qq6Ilh4XxgcS3yJwjLOvFafugoXjN3Eguj4GhaWYA0pB8~JpcFDnWkeJVCA__&Key-Pair-Id=APKAIE5G5CRDK6RD3PGA)
Location of key sections of Neoproterozoic deposits in the structure of the... Available to Purchase
Published: 01 March 2004
— Southeastern Tuva (Sangilen Upland), Erzin, Naryn, and Balyktyg-Khem Rivers; 13 — Gargan Block, Irkutny Gargan and Zhakhoi Rivers; 14 — Kuznetsk Alatau, Tom’ River; 15 — southeastern East Sayans, Dibi and Khazalkha Rivers.
Image
Carbon and oxygen isotope composition of rocks of alkaline complexes and th... Available to Purchase
in Mantle–Crustal Nature of Early Paleozoic Alkaline Intrusions in Central Sangilen, Tuva (from Nd, Sr, Pb, C, and O Isotope Data)
> Russian Geology and Geophysics
Published: 01 May 2019
al. ( 1999 ), Vrublevskii and Gertner ( 2005 ), and Vrublevskii et al. ( 2018c ). Sangilen upland: 1 , calcite of alkaline rocks, 2 , carbonatite-like rocks, 3 , hydrothermal veins of calcite, 4 , limestones and marbles. Temperatures of apatite–calcite isotope equilibrium: 5 , carbonatite-like
Image
Nd–Sr–Pb isotope composition of alkaline and carbonatite-like rocks of the ... Available to Purchase
in Mantle–Crustal Nature of Early Paleozoic Alkaline Intrusions in Central Sangilen, Tuva (from Nd, Sr, Pb, C, and O Isotope Data)
> Russian Geology and Geophysics
Published: 01 May 2019
Fig. 4. Nd–Sr–Pb isotope composition of alkaline and carbonatite-like rocks of the Sangilen upland. a , εNd( T )–εSr( T ) diagram. For comparison, the predominant compositions (gray fields) of igneous rocks of alkaline and carbonatite complexes of the CAOB (Mesozoic: 1 , southern Mongolia, 2
Journal Article
NEOPROTEROZOIC STRATIGRAPHY OF THE ALTAI-SAYAN FOLDED AREA Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 March 2004
Russ. Geol. Geophys. (2004) 45 (3): 295–309.
... — Southeastern Tuva (Sangilen Upland), Erzin, Naryn, and Balyktyg-Khem Rivers; 13 — Gargan Block, Irkutny Gargan and Zhakhoi Rivers; 14 — Kuznetsk Alatau, Tom’ River; 15 — southeastern East Sayans, Dibi and Khazalkha Rivers. ...
FIGURES
Journal Article
RUBIDIUM-STRONTIUM DATING OF ALKALI GRANITES IN NORTHEASTERN TUVA Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 July 1998
Russ. Geol. Geophys. (1998) 39 (7): 925–931.
... and in several cycles. They are of Late Ordovician age in the Early Paleozoic Kazyr-Kizir zone of northeastern Tuva, of Late Ordovician and, probably, Early Devonian age in the Sayan Proterozoic rocks, of Late Ordovician and, probably, Devonian and Middle Carboniferous age on the Sangilen Upland. – Early...
FIGURES
Journal Article
Estimation of heat flow in Tuva from data on helium isotopes in thermal mineral springs Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 February 2010
Russ. Geol. Geophys. (2010) 51 (2): 209–219.
... flow (q T ). Earlier ( Duchkov and Sokolova, 1974 ; Fotiadi, 1987 ; Sokolova and Duchkov, 2008 ), heat flow qT was measured by the standard geothermal method at ten sites ( Table 3 , Fig. 2 ). Two of them (Ak-Sug and Aryskan) are in eastern Tuva; one (Tanzek), on the Sangilen upland; and seven...
FIGURES
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
Journal: European Journal of Mineralogy
Publisher: GeoScienceWorld Journals
Published: 01 June 2015
European Journal of Mineralogy (2015) 27 (3): 417–426.
... of the study of spodumene pegmatites of the Sangilen Upland, in the southeast of Tyva. Ferro-fluoro-pedrizite, the F-dominant analogue of ferro-pedrizite, was described earlier as a new mineral from the same area (under the name “fluoro-sodic-ferropedrizite” suggested by the rules in force at that time...
FIGURES
Journal Article
Geochemistry, isotope triad (Nd–Sr–O), and 40 Ar– 39 Ar age of Paleozoic alkaline mafic intrusions of the Kuznetsk Alatau (by the example of the Belaya Gora pluton) Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 March 2016
Russ. Geol. Geophys. (2016) 57 (3): 464–472.
... .
Nikiforov , A.V. , Sugorakova , A.M. , Vrublevskii , V.V. , Lykhin , D.A. , 2014 . Nepheline–syenite complexes of the Sangilen upland: the time of formation of the Chik massif, in: Proceedings of the Scientific Meeting “Geodynamic Evolution of the Lithosphere of the Central Asian Mobile...
FIGURES
Journal Article
GRANITOID MAGMATISM OF WESTERN SANGILEN ( the problem of genesis of S- and A-type granites ) Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 June 2001
Russ. Geol. Geophys. (2001) 42 (6): 887–900.
.... H. Blake , R. W. D. Elwell , J. L. Gibson , et al. , Quartz. J. Geol. Soc. London , vol. 121 , p. 31 , 1965 . [18] N. V. Rogov , Geology of the Precambrian complex of the Tuva upland of Sangilen (migmatite-anatectic formation of high denudation level), PhD thesis...
FIGURES
Journal Article
The tectonomagmatic evolution of structure-lithologic complexes in the Tannu-Ola zone, Tuva, in the Late Vendian–Early Cambrian ( from geochemical , Nd isotope, and geochronological data ) Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 May 2011
Russ. Geol. Geophys. (2011) 52 (5): 503–516.
.... , 1980 . The stratigraphic volume of Lower Cambrian deposits on the northwestern margin of the Sangilen upland in Tuva , in: The Cambrian Strata in the Altai–Sayan Folded Area [in Russian] . Nauka , Moscow , pp. 95 – 115 .
Yarmolyuk , V.V. , Kovalenko...
FIGURES
Journal Article
Sillimanite group minerals: a new promising raw material for the Russian aluminum industry Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 December 2010
Russ. Geol. Geophys. (2010) 51 (12): 1247–1256.
... deposit are the alumina-richest (Al 2 O 3 = 26.5%). This deposit is localized within the Sangilen upland (Tuva Republic). The balance ore (types A + B + C) reserves are estimated at 350 mln tons. Other promising raw materials for alumina and aluminum production are synnyrites, anorthosites, kaolines...
FIGURES
Journal Article
Late Cambrian-Ordovician tectonics and geodynamics of Central Asia Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 January 2007
Russ. Geol. Geophys. (2007) 48 (1): 71–82.
... by the Sangilen Upland, SE Tuva), in: Geodynamic evolution of the lithosphere of the Central Asian mobile belt (from ocean to continent). Vol. 1 [in Russian], Inst. Geograph. Publ. , Irkutsk , pp. 141 – 145 .
Volkova , N.I , Stupakov , S.I. , Tret’yakov...
FIGURES
Journal Article
Metallogeny of Endogenous Gold in Tuva Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 November 2022
Russ. Geol. Geophys. (2022) 63 (11): 1300–1312.
... , I.T. , Pegel’ , T.V. , Fefelov , A.F. , 1980 . The stratigraphic volume of lower Cambrian deposits on the northwestern margin of the Sangilen upland in Tuva , in: The Cambrian of the Altai–Sayan Folded Area [in Russian]. Nauka, Moscow , pp. 95 – 115...
FIGURES
Journal Article
THE OKA PLATEAU IN THE NEOTECTONIC FRAMEWORK OF SOUTHERN EAST SIBERIA Available to Purchase
Journal: Russian Geology and Geophysics
Publisher: Novosibirsk State University
Published: 01 June 2001
Russ. Geol. Geophys. (2001) 42 (6): 930–938.
... trending system of basins (Terekhopol, Bilingol, and Busingol) marking the descending topography of the foothill of the western flank of the rift zone. This feature is atypical of the common structure of the Baikal Rift. West of the Darkhat basin there is a small upland, which is the western flank...
FIGURES
1
