Results 51 to 60 of about 262 (125)

On the structure and formation of earthquake sources in the faults located in the subsurface and deep levels of the crust. Part II. Deep level

Геодинамика и тектонофизика, 2018
In the part 2 of the study [Ruzhich, Kocharyan, 2017, we aimed at identifying the elements of paleoearthquake sources in the crust, which formed at the hypocentral depths in the exhumed Primorsky segment of the ancient collisional suture.
V. V. Ruzhich, G. G. Kocharyan, V. B. Savelieva, A. V. Travin   +3 more
doaj   +1 more source

THE CENOZOIC GRABEN IN THE MARGINAL SUTURE ZONE OF THE SIBERIAN CRATON: INTERIOR STRUCTURAL FEATURES AND TECTONIC STRESS RECONSTRUCTIONS

Геодинамика и тектонофизика
Marginal suture zones of ancient platforms are deep-seated fault zones separating the craton from the mobile belt. Of particular interest is the Pribaikalian marginal suture of the Siberian craton, activated during the Cenozoic rifting.
A. V. Cheremnykh, A. A. Bobrov, I. K. Dekabryov, A. S. Cheremnykh, G. A. Gridin, D. V. Pavlov, A. A. Yuriev   +6 more
doaj   +1 more source

EARLY STAGE OF THE CENTRAL ASIAN OROGENIC BELT BUILDING: EVIDENCES FROM THE SOUTHERN SIBERIAN CRATON

Геодинамика и тектонофизика, 2017
The origin of the Central-Asian Orogenic Belt (CAOB), especially of its northern segment nearby the southern margin of the Siberian craton (SC) is directly related to development and closure of the Paleo-Asian Ocean (PAO).
D. P. Gladkochub, T. V. Donskaya, Shihong Zhang, S. A. Pisarevsky, A. M. Stanevich, A. M. Mazukabzov, Z. L. Motova   +6 more
doaj   +1 more source

Tectonic Evolution and Structural Control of Dike-Hosted Orogenic Gold Deposits in the Yana–Kolyma Collision Orogen (Eastern Siberia): Insights from the Eastern Margin of the Siberian Craton

Geosciences
The Yana–Kolyma collision orogen, Eastern Siberia, is one of world-class gold economic belts, where large gold deposits are localized, mainly in the Upper Paleozoic and Lower Mesozoic clastic rocks.
Valery Yurievich Fridovsky, Maxim Vasilievich Kudrin   +1 more
doaj   +1 more source

Geochronology of sillimanite-cordierite gneiss Atamanovo series of the South Yenisei Ridge (Russia)

Литосфера, 2017
The paper provides justification of Paleo Archaean age (3221 ± 15 Ma) of the granulite plutonic metamorphism that formed the Kan metamorphic complex of the Archaean crust in the Angara-Kan block of the Siberian craton. The age was defined on the basis of
A. M. Sazonov, K. A. Zablotsky, U. . Linnemann, E. A. Zvyagina, N. A. Nekrasova, E. A. Naumov, S. A. Sil′yanov   +6 more
doaj   +2 more sources

EARLY NEOPROTEROZOIC GRANITOIDS IN THE RYAZANOVSKY MASSIF OF THE YENISEI RIDGE AS INDICATORS OF THE GRENVILLE OROGENY AT THE WESTERN MARGIN OF THE SIBERIAN CRATON

Геодинамика и тектонофизика
Studies of the geological history of the Yenisei Ridge are important not only for understanding the tectonic evolution of mobile belts at the boundaries of ancient cratons but also for problem solving whether the Siberian craton was a part of the Rodinia
A. D. Nozhkin, O. M. Turkina, I. I. Likhanov, Yu. L. Ronkin   +3 more
doaj   +1 more source

AMPHIBOLE-PHLOGOPITE XENOLITHS FROM KIMBERLITES AS EVIDENCE OF METASOMATIC PROCESSES IN THE LITHOSPHERIC MANTLE BENEATH KUOIKA FIELD

Геодинамика и тектонофизика
This paper devoted to the mantle xenoliths with evidence of modal metasomatic alteration from the Obnazhennaya kimberlite pipe (Kuoika kimberlite field).
T. V. Kalashnikova, S. I. Kostrovitsky, A. M. Dymshits   +2 more
doaj   +1 more source

88th Annual Meeting of the Meteoritical Society 2026: Abstracts

Meteoritics &Planetary Science, Volume 61, Issue S1, Page S48-S551, August 2026.
wiley   +1 more source

Oroclines in the Central Asian Orogenic Belt. [PDF]

Natl Sci Rev, 2023
Liu Y, Xiao W, Ma Y, Li S, Peskov AY, Chen Z, Zhou T, Guan Q.   +7 more
europepmc   +1 more source

Genesis of the Xiaotazigou gold deposit in the northern margin of the north China craton: constraints from sulfur isotopes, rare earth elements, and trace elements

Frontiers in Earth Science
The Xiaotazigou gold deposit is located in the eastern section of the Chifeng–Chaoyang gold metallogenic belt on the northern margin of the North China Craton. In this study, rare earth and trace element compositions of ores and host rocks, together with
He Yuan, He Yuan, Lichun Fu, Lichun Fu, Yinzeng Bai, Qiang Wei, Zejiao Wang, Yongtao Zhao, Jingyao Sun, Jingyao Sun   +9 more
doaj   +1 more source