INFLUENCE OF EUSTASY AND TECTONISM ON REEF ARCHITECTURE IN EARLY PERMIAN REEF COMPLEXES, SOUTHERN URALS, RUSSIA

2002 ◽  
pp. 205-218 ◽  
Author(s):  
EMMANUELLE VENNIN ◽  
THIERRY BOISSEAU ◽  
JEAN-NOËL PROUST ◽  
BORIS I. CHUVASHOV
Keyword(s):  
Southern Urals ◽  
Early Permian

scholarly journals Early Permian granitoids of the East Magnitogorsk zone (South- ern Urals): petrology, geochemistry, and geodynamic formation environment

2020 ◽  
Vol 1 (1) ◽  
pp. 47-62
Author(s):  
Timofey Nikolaevich SURIN ◽  
Keyword(s):  
Water Pressure ◽  
Southern Urals ◽  
Geodynamic Setting ◽  
Type I ◽  
Early Permian ◽  
The Southern Urals ◽  
Quartz Syenite ◽  
Crystallization Differentiation ◽  
Geochemical Study

The relevance of the problem. The Early Permian magmatism of the Southern Urals is poorly studied with the help of modern methods. The granitoid massifs of this age locally developed in the East Magnitogorsk zone contain important information about the geodynamic conditions of their formation. Clarification of this issue makes an important contribution to the understanding of the geodynamic development of the Urals. The nature of granitoids is still debatable. The connection with the massifs combined in the Balkan complex of gold-tungsten mineralization indicates the need for a comprehensive study. The purpose of the study is to determine the petrological and geochemical features of the rocks of the Balkan complex, to identify the mechanism of their petrogenesis and to establish the geodynamic conditions of their formation. Results. The petrological and geochemical study of the formations of the Balkan complex was carried out and their place in the typical taxonomy of granitoids was determined. Their belonging to the I-type is shown. Mineralogical and petrogeochemical methods were first studied for shonkinite xenoliths in granitoids. The mechanism of petrogenesis of rocks is proposed and the geodynamic setting of their formation is determined. It is shown that the monzonitemonzodiorite-quartz syenite-granosyenite-leucogranite series of rocks was formed as a result of crystallization differentiation of a single parental melting, and it was also concluded that the massifs of the complex are formed under conditions of early collision conditions with the important role of the subduction process. The mechanism of formation of the massifs of the complex is largely similar to mechanism for granitoids in other conflict areas, although it has its own specifics. Conclusions. 1). The Early Permian granitoids of the Balkan complex relates to type I. 2). All rocks of the complex, from monzonites to quartz syenites and leucogranites, including xenolith shonkinites, form a petrogenetic series formed as a result of crystallization differentiation of a single parent alkaline-gabbroic melting with increased water pressure. 3). The Balkan complex was formed in an early collisional setting under the action of deep subduction. 4). Transpression in the upper part of the crust induced formation of the massifs of the complex. 5). The Balkan complex is a kind of indicator of the growth of the newly formed crust as a result of collision and accretion processes.

Large-sized Early Permian “caninioid” corals from the Karavanke Mountains, Slovenia

2016 ◽  
Vol 90 (6) ◽  
pp. 1049-1067 ◽  
Author(s):  
Olga L. Kossovaya ◽  
Matevž Novak ◽  
Dieter Weyer
Keyword(s):  
Southern Urals ◽  
Wide Distribution ◽  
Time Span ◽  
Lower Permian ◽  
New Taxon ◽  
Early Permian ◽  
The Southern Urals ◽  
Predominant Species ◽  
Large Numbers ◽  
Distinguishing Features

AbstractA new monospecific “caninioid” genus,Preisingerellan. gen., from the lower Permian of the Karavanke Mountains (Southern Alps, Slovenia) is erected. The type species isPreisingerella stegovnikensisn. sp. The new taxon can be differentiated from otherCaninia-type genera by its specific ontogeny and features of its dissepimentarium. Corals with such morphology had a wide distribution during the Carboniferous and early Permian, occurring in mostly shallow-water carbonate rocks. The phylogenetic relationships within this group are mostly unclear due to similarities in the adult stages. The earlier stages reveal the main distinguishing features that are decisive for a generic assignment, but these have rarely been well preserved and properly considered. The new taxon is compared with related genera of the Cyathopsidae and species ofCaninellaGorskiy, 1938 characterized by lateral dissepiments. Large numbers of specimens of the new species, representing a monospecific assemblage, have been collected from the Born Formation at Mt. Stegovnik. Sedimentological and microfacies characteristics, as well as macro- and microfossil assemblages, underline this correlation. The fusulinoidean assemblage of the Born Formation, withSphaeroschwagerina carniolica(Kahler and Kahler, 1937), as the predominant species, corresponds to the time span between theSphaeroschwagerina moelleri-Schwagerina fecundaandPseudofusulina moellerizones, indicating a late Asselian to early Sakmarian age in the Southern Urals.

Carbon isotope chemostratigraphy and implications of palaeoclimatic changes during the Cisuralian (Early Permian) in the southern Urals, Russia

2012 ◽  
Vol 21 (2-3) ◽  
pp. 601-610 ◽  
Author(s):  
Jun Zeng ◽  
Chang-qun Cao ◽  
V.I. Davydov ◽  
Shu-zhong Shen
Keyword(s):  
Carbon Isotope ◽  
Southern Urals ◽  
Early Permian ◽  
The Southern Urals

The first data on possible Mezozoic magmatism within the Western slope of the Southern Urals

2018 ◽  
pp. 24-34
Author(s):  
A. O. Khotylev ◽  
N. B. Devisheva ◽  
Al. V. Tevelev ◽  
V. M. Moseichuk
Keyword(s):  
Southern Urals ◽  
Western Slope ◽  
Isotopic Age ◽  
The Southern Urals ◽  
Early Proterozoic ◽  
Carbonate Formations ◽  
Two Bodies

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.

On the bryophyte flora of “Iremel” Nature Park (Southern Urals)

Arctoa ◽  
2015 ◽  
Vol 24 (1) ◽  
pp. 194-203 ◽  
Author(s):  
Elvira Z. Baisheva ◽  
Elena A. Ignatova ◽  
Nijole Kalinauskaite ◽  
Alexey D. Potemkin
Keyword(s):  
Southern Urals ◽  
Nature Park
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