1-20 OF 60 RESULTS FOR

Sarkhoi Group

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?
Close Modal
Sort by
Journal Article
Published: 01 July 2011
Russ. Geol. Geophys. (2011) 52 (7): 685–700.
...A.B. Kuzmichev; A.N. Larionov Abstract The Sarkhoi Group localized in the stratotype area is composed of various volcanics and volcanoclastics more than 4 km in total thickness. The volcanics of the lower part are greenschist facies altered rocks ranging from basalt to dacite, and those...
FIGURES | View All (8)
Image
Geologic structure of the <span class="search-highlight">Sarkhoi</span> <span class="search-highlight">Group</span> stratotype locality.  1 , Quaternar...
Published: 01 July 2011
Fig. 2. Geologic structure of the Sarkhoi Group stratotype locality. 1 , Quaternary deposits; 2 , Neogene–Quaternary basalts; 3 , carbonate rocks of the Bokson Group; 4 , variegated terrigenous rocks in the basement of the Bokson Group, the wavy line in their basement marks an unconformity
Image
SiO 2 –(Na 2 O + K 2 O) diagram for <span class="search-highlight">Sarkhoi</span> <span class="search-highlight">Group</span> effusive rocks. A-B — and...
Published: 01 August 2007
Fig. 2. SiO 2 –(Na 2 O + K 2 O) diagram for Sarkhoi Group effusive rocks. A-B — andesite-basalts, B+T — basalt + tephrite, P+T — phonolite + tephrite, P+N — phonolite + nephelinite; rhombuses mark the compositions of the studied rocks.
Journal Article
Published: 01 August 2007
Russ. Geol. Geophys. (2007) 48 (8): 643–655.
...Fig. 2. SiO 2 –(Na 2 O + K 2 O) diagram for Sarkhoi Group effusive rocks. A-B — andesite-basalts, B+T — basalt + tephrite, P+T — phonolite + tephrite, P+N — phonolite + nephelinite; rhombuses mark the compositions of the studied rocks. ...
FIGURES | View All (7)
Journal Article
Published: 01 December 2011
Russ. Geol. Geophys. (2011) 52 (12): 1662–1671.
...E.F. Letnikova; S.V. Veshcheva; A.I. Proshenkin; A.B. Kuznetsov Abstract We have established that the terrigenous deposits of the Haisuin Formation and metamorphic deposits of the Shutkhulai block are similar in geochemical characteristics to the rocks of the Oka Group. The volcanics of the Sarkhoi...
FIGURES | View All (9)
Image
Harker’s variation diagrams for granites of the Khorin-Gol complex ( 1 ) an...
Published: 01 August 2007
Fig. 4. Harker’s variation diagrams for granites of the Khorin-Gol complex ( 1 ) and effusive rocks of the Sarkhoi Group ( 2 ).
Image
Rb-Sr isochrons for plagiogranites of the Khorin-Gol complex ( a ) and bere...
Published: 01 August 2007
Fig. 3. Rb-Sr isochrons for plagiogranites of the Khorin-Gol complex ( a ) and beresites ( b ) and effusive rocks ( c ) of the Sarkhoi Group.
Image
Trace-element distribution pattern for granites of the Khorin-Gol complex (...
Published: 01 August 2007
Fig. 5. Trace-element distribution pattern for granites of the Khorin-Gol complex (horizontal hatching) and effusive rocks of the Sarkhoi Group (vertical hatching).
Image
EMORB-normalized ( Sun and McDonough, 1989 ) REE patterns of the <span class="search-highlight">Sarkhoi</span> Gr...
Published: 01 July 2011
Fig. 8. EMORB-normalized ( Sun and McDonough, 1989 ) REE patterns of the Sarkhoi Group volcanics. A , Typical rocks of the greenstone and ignimbrite units; B , atypical rocks, granophyre, and Sumsunur tonalites.
Image
Chondrite-normalized ( Sun and McDonough, 1989 ) REE patterns of the Sarkho...
Published: 01 July 2011
Fig. 7. Chondrite-normalized ( Sun and McDonough, 1989 ) REE patterns of the Sarkhoi Group volcanics. A , Greenstone and granophyric unit, B , ignimbrite unit. For comparison, the data on the tonalites from the Gargan massif of the Sumsunur complex, possible plutonic comagmates, are given.
Image
Schematic geological map of the Tissa River basin (scale 1 : 50,000).  1  —...
Published: 01 August 2007
Fig. 1. Schematic geological map of the Tissa River basin (scale 1 : 50,000). 1 — Quaternary deposits; 2 — Neogene-Quaternary basalts; 3 — effusions of the Sarkhoi Group (Є 1 ); 4 — granitoids of the Urik complex (PR 3 ); 5–7 — Khorin-Gol complex (V–Є 1 ) : 5 — plagiogranites
Image
REE patterns of the terrigenous deposits of the Oka <span class="search-highlight">Group</span> and Haisuin Forma...
Published: 01 December 2011
), wackes of the Haisuin Formation ( 6 ); 7 , field of plagiogneisses and plagiogranites of the Early Precambrian Gargan lock; 8 , field of Neoproterozoic volcanics of the Sarkhoi Group, after Kuz’michev (2004) .
Image
Schematic geologic structure of the Tuva–Mongolian massif, compiled after  ...
Published: 01 December 2011
, Neoproterozoic terrigenous deposits of the Oka Group (1) and Haisuin Formation (3) and metamorphic rocks of the Shutkhulai block (2); 4 , Neoproterozoic volcanogenic Sarkhoi Group; 5 , 6 , rocks of the Dunjugur ophiolite complex; 7 , tonalities of the Sumsunur complex; 8 , crystalline rocks of the Late
Image
Simplified geology of Dunzhugur site, modified after  Kuzmichev (2004) . Fo...
Published: 01 January 2016
margin complexes (800–700 Ma): 5 , Holbin porphyry; 6 , Sarkhoy Group varicolored rocks; 7 – 13 , Dunzhugur oceanic arc (1000–800): 7 , sediments related to ophiolites; 8 , basaltic andesites ( a ) and boninites ( b ); 9 , sheeted dike complex; 10 , gabbro; 11 , layered gabbro-pyroxenite series
Image
a , Simplified geological map of the Tuva–Mongolian massif (TMM) and the Tu...
Published: 01 August 2022
, Kitoi complex; 2 , Khangarul Formation; 3 , Il’chir Complex; 4 , Il’chir Formation; 5 , unnamed formation; 6 , Sarkhoi Group; 7 , Bokson Group; 8 , Gorlyk Formation; 9 , Zun-Murin Complex; 10, Barun-Gol Formation; 11 , Urik Complex; 12 , Sagan-Sair Formation; 13 , Narin-Gol Formation; 14
Image
Major lithotectonic units in southeastern East Sayan (after [ 15 ], with su...
Published: 01 January 2006
-autochthone). Lower allochthone: 4 — shales, olistostromes, and metavolcanics, 5 — ophiolites with melange (white triangles), 6 — flysch and basic volcanics, 7 — island-arc volcanics of the Sarkhoi Group. Middle allochthones: 8 — limestones and dolomites of the Bokson Group (V–Є 2 ). Upper
Journal Article
Published: 01 December 2011
Russ. Geol. Geophys. (2011) 52 (12): 1634–1642.
...F.I. Zhimulev; M.M. Buslov; S. Glorie; J. De Grave; M.A. Fidler; A. Izmer Abstract Granites from the Tunka pluton of the Sarkhoi complex, located in the eastern Tunka bald mountains (East Sayan), have been dated at the Middle Ordovician (462.6 ± 7.8 Ma) by LA ICP MS. The granites of the Sarkhoi...
FIGURES | View All (5)
Journal Article
Published: 01 June 2003
Russ. Geol. Geophys. (2003) 44 (6): 531–541.
... complex); 7 — Vendian-Cambrian sedimentary cover; 8 – 13 — Riphean basement rocks: 8 — sediments and volcano-sedimentary deposits (Oka Group), 9 — volcano-sedimentary deposits (Khugein Group), 10 — calc-alkaline volcanics (Sarkhoi and Darkhat Groups), 11 — ophiolites ( a ) and turbidites ( b...
FIGURES | View All (4)
Journal Article
Published: 01 January 2013
Russ. Geol. Geophys. (2013) 54 (1): 34–43.
... , pp. 130 – 150 . Kuzmichev , A.B. , 2004 . Tectonic History of the Tuva–Mongolian Massif: Early Baikalian, Late Baikalian, and Early Caledonian Stages [in Russian] . PROBEL , Moscow . Kuzmichev , A.B. , Larionov , A.N. , 2011 . The Sarkhoi Group in East Sayan...
FIGURES | View All (10)
Image
The Precambrian Tuva–Mongolian and Dzavhan massifs. Granitoids and young de...
Published: 01 July 2011
: 5 , complex of active continental margin (Sarkhoi, Darkhat, and Dzavhan Groups), 6 , Oka accretionary prism, 7 , Shishkhid island arc; 8 , East Tuva orogenic trough. The rectangle marks the position of the site shown in Fig. 2 .