1-6 OF 6 RESULTS FOR

Sarkhoi-Dzavhan volcanic belt

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.
... parts of the Tuva–Mongolian and Dzavhan massifs. The ~1500 km long SarkhoiDzavhan volcanic belt is a fragment of the Neoproterozoic active continental margin separated from the continent. In the Middle Neoproterozoic, the geodynamic system also included the Oka accretionary prism joining the Sarkhoi...
FIGURES | View All (8)
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 2006
Russ. Geol. Geophys. (2006) 47 (1): 53–70.
... in [ 3 ] and [ 8 ], with additions. 1 — fold-thrust belts on subsided craton margins (BP stands for Baikal-Patom basin); 2 — fragments of Precambrian microcontinents, abbreviated as: Al — Altai, TM — Tuva-Mongolia, Dz — Dzavhan, CM — Central Mongolia, Arg — Argun, SG — South Gobi, JB — Jiamusy-Bu...
FIGURES | View All (6)
Journal Article
Published: 01 October 2006
Russ. Geol. Geophys. (2006) 47 (10): 1045–1055.
... is valid. Different authors outline the Barguzin microcontinent in different ways. According to Zonenshain et al. [ 2 ], it is composed of the Olokit structure, Baikal-Muya belt, and the southern Barguzin zone ( Fig. 1 ). Belichenko et al. [ 3 ] extend the microcontinent southward, to Kyakhta, where...
FIGURES | View All (5)
Journal Article
Published: 01 June 2021
Russ. Geol. Geophys. (2021) 62 (6): 619–632.
... ), which can be considered the microcontinent foundation. The next belt consists of riftogenic complexes of volcano-plutonic and sedimentary formations of the Kuvai (775 Ma) ( Watanabe et al., 1999 ), Sarkhoi and Dzabkhan series (803–773 Ma) ( Levashova et al., 2010 ) and alkaline granites breaking through...
FIGURES | View All (7)
Journal Article
Published: 01 October 2013
Russ. Geol. Geophys. (2013) 54 (10): 1135–1149.
... analysis of gravity, magnetic, and seismic anomalies . Russian Geology and Geophysics (Geologiya i Geofizika) 54 ( 8 ), 859 – 873 (1108–1125). Kuzmichev , A.B. , Larionov , A.N. , 2011 . The Sarkhoi Group in East Sayan: Neoproterozoic (~770–800 Ma) volcanic belt of the Andean type...
FIGURES | View All (5)