Garnet-pyroxene and lawsonite-bearing rocks of the Maksyutov Complex (Southern Urals)

2013 ◽  
Vol 54 (11) ◽  
pp. 1369-1384 ◽  
Author(s):  
P.M. Valizer ◽  
A.I. Rusin ◽  
A.A. Krasnobaev ◽  
I.I. Likhanov
2015 ◽  
Vol 461 (1) ◽  
pp. 291-296 ◽  
Author(s):  
P. M. Valizer ◽  
A. A. Krasnobaev ◽  
A. I. Rusin

2007 ◽  
Vol 417 (2) ◽  
pp. 1421-1423 ◽  
Author(s):  
T. G. Shumilova ◽  
N. P. Yushkin ◽  
E. V. Pushkarev

1995 ◽  
Vol 37 (7) ◽  
pp. 584-600 ◽  
Author(s):  
V. I. Lennykh ◽  
P. M. Valizer ◽  
Rachel Beane ◽  
Mary Leech ◽  
W. G. Ernst

2015 ◽  
Vol 461 (2) ◽  
pp. 414-418 ◽  
Author(s):  
A. A. Krasnobaev ◽  
P. M. Valizer ◽  
V. N. Anfilogov ◽  
S. V. Busharina

2002 ◽  
Vol 66 (7) ◽  
pp. 1221-1235 ◽  
Author(s):  
Johannes Glodny ◽  
Bernard Bingen ◽  
Håkon Austrheim ◽  
José F Molina ◽  
Anatolij Rusin

Author(s):  
A. O. Khotylev ◽  
N. B. Devisheva ◽  
Al. V. Tevelev ◽  
V. M. Moseichuk

Within the Western slope of the Southern Urals, there are plenty of basite dyke complexes of Riphean to Vendian among Precambrian terrigenous-carbonate formations. In metamorphic formations of the Taratash complex (Archean to Early Proterozoic, the northern closure of the Bashkirian meganticlinorium) there was observed the andesitic dyke with isotopic age of 71±1 Ma (U-Pb SHRIMP II on zircons) and near Bakal two bodies of gabbroids with zircons of similar ages were found. These are the first evidence of possible Mezozoic magmatism in this region.


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