Zobrazeno 1 - 10
of 38
pro vyhledávání: '"S. V Khromykh"'
Publikováno v:
Геодинамика и тектонофизика, Vol 10, Iss 1, Pp 79-99 (2019)
The history of the Central Asian Orogenic Belt (CAOB) was marked by several major events of magmatism which produced large volumes of volcanic and intrusive (mafic-ultramafic and granitic) rocks within a relatively short time span (30–40 Ma) over a
Externí odkaz:
https://doaj.org/article/bdf90528f5344b9197080e772a3b8411
Publikováno v:
Геодинамика и тектонофизика, Vol 8, Iss 3, Pp 489-493 (2017)
Altai collision system of Hercynides was formed in Late Paleozoic as a result of oblique collision of Siberian continent and Kazakhstan composed terrane [Vladimirov et al., 2003; 2008; Xiao et al., 2010]. At the late stages of its evolution (time int
Externí odkaz:
https://doaj.org/article/50edb6a743d0408d9f538a53d8b99541
Publikováno v:
Геодинамика и тектонофизика, Vol 8, Iss 2, Pp 311-330 (2017)
The paper reports on studies of the Preobrazhensky gabbro‐granitoid intrusion, East Kazakhstan, com‐ posed of the rocks that belong to four phases of intrusion, from quartz monzonites and gabbroids to granite‐ leucogranites. Specific relationsh
Externí odkaz:
https://doaj.org/article/21396d7e349345f6bd75d785276621e4
Autor:
A. G. Vladimirov, A. S. Mekhonoshin, S. V. Khromykh, E. I. Mikheev, A. V. Travin, N. I. Volkova, T. B. Kolotilina, Yu. A. Davydenko, E. V. Borodina, V. V. Khlestov
Publikováno v:
Геодинамика и тектонофизика, Vol 8, Iss 2, Pp 223-268 (2017)
In the Chernorud granulite zone in the Olkhon region of West Pribaikalie, we studied gabbro‐pyroxenites composing tectonic plates (Chernorud, Tonta) and synmetamorphic intrusive bodies (Ulan‐Khargana), as well as nu‐ merous disintegrated boudin
Externí odkaz:
https://doaj.org/article/350811f3c23441a584e68e1cfe32f1b8
Autor:
S. V. Khromykh, Alexandra V. Gurova, P. D. Kotler, A. A. Perfilova, E. I. Mikheev, D. V. Semenova
Publikováno v:
Geotectonics. 54:510-528
Studies of volcanic rocks in orogenic troughs of Eastern Kazakhstan were carried out. The troughs were formed at late-orogenic stages of evolution of Hercynian Altai collision system. Volcanic rocks are represented by basalts, andesites, dacites and
Publikováno v:
Naukovyi Visnyk Natsionalnoho Hirnychoho Universytetu. :16-21
Purpose. Study on the chemical composition of lake waters, salt brines, brine and bottom sediments to identify the mineralization of rare metals and other types of minerals. Methodology. Mass spectrometric studies (mass spectrometer with inductively
Publikováno v:
Geosfernye issledovaniya. :6-26
Autor:
P.D. Kotler, E. A. Kruk, Y. V. Kuibida, N.N. Kruk, M.L. Kuibida, Boris Dyachkov, S. V. Khromykh, A. G. Vladimirov, S. N. Rudnev, Tatiana A. Oitseva
Publikováno v:
Journal of Asian Earth Sciences. 175:178-198
The paper presents new original data and a review of previous studies on the Late Carboniferous – Early Permian granitoids of the Kunush and Kalguty intrusive complexes from the Kalba fold belt (East Kazakhstan). These rocks formed at the initial p
Autor:
S. Maruyama, Olga Obut, I. A. Savinsky, P.D. Kotler, S. K. Krivonogov, Alina Perfilova, Alexandra V. Gurova, S. V. Khromykh, I.Yu. Safonova, N. A. Petrenko, R. I. Chyornyi
Publikováno v:
Russian Journal of Pacific Geology. 13:283-296
The Itmurundy zone of the northern Balkhash area is a Pacific-type orogenic belt. It possesses a complex geological structure and hosts rocks of mantle, accretionary and post-orogenic associations. The volcanic and sedimentary rocks of the accretiona
Publikováno v:
Petrology. 26:368-388
The paper reports results of petrological-geochemical, isotope, and geochronological studies of the Preobrazhenka gabbro–granitoid massif located in the Altai collisional system of Hercynides, Eastern Kazakhstan. The massif shows evidence for the i