Zobrazeno 1 - 10
of 16
pro vyhledávání: '"P. D. Kotler"'
Publikováno v:
Геодинамика и тектонофизика, Vol 13, Iss 1 (2022)
The paper presents new petrographic and geochemical data from volcanic and sedimentary rocks and first U-Pb ages of detrital zircons from sandstones of the Itmurundy zone of central Kazakhstan. The volcanic rocks are aphyric and porphyric basalts, an
Externí odkaz:
https://doaj.org/article/b3afb6cd157a40ba8260fcc00b9db143
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:
Sergey V. Khromykh, Pavel D. Kotler, Anna V. Kulikova, Dina V. Semenova, Kamil R. Minnebaev, Bulat I. Gareev, Georgii A. Batalin, Tatiana N. Antsiferova, Ekaterina A. Il’icheva, Alexey S. Volosov
Publikováno v:
Minerals, Vol 12, Iss 9, p 1101 (2022)
We provide the results of studying the internal structure and composition of the rocks of the Semeitau and Delbegetei massifs located in Eastern Kazakhstan. It was previously believed that these massifs have different ages and were formed in differen
Externí odkaz:
https://doaj.org/article/6fa5284dda054a30942639cc267102fd
Autor:
A. A. Perfilova, I. Yu. Safonova, K. E. Degtyarev, I. A. Savinsky, P. D. Kotler, B. P. Khassen
Publikováno v:
Doklady Earth Sciences. 505:416-421
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:
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
Autor:
Yertlek Suiekpayev, Reimar Seltmann, Galiya Bekenova, Mikhail Kravchenko, S. V. Khromykh, A.Zh. Azelkhanov, Alla Dolgopolova, Yerzhan Sapargaliyev, Franco Pirajno, P. D. Kotler
Publikováno v:
Ore Geology Reviews. 131:104015
The Karaotkel deposit of fossil Ti-Zr placers is situated in the north-western edge of the Zaysan intermontane depression in Eastern Kazakhstan. The geological structure of the mineral sands is characterized by complex morphology and a two-layered as
Late Paleozoic granitoid magmatism of Eastern Kazakhstan and Western Transbaikalia: plume model test
Autor:
P. D. Kotler, D. S. Yudin, N. N. Kruk, G. S. Karavaeva, O. V. Navozov, A. V. Travin, V. B. Khubanov, Alexander Vladimirov, A.A. Tsygankov, M.D. Buyantuev, T. N. Antsiferova, G.N. Burmakina, S. V. Khromykh
Publikováno v:
Russian Geology and Geophysics. 57:773-789
We present results of a comparative study of Late Paleozoic granitoids of Eastern Kazakhstan and Western Transbaikalia composing the large Kalba–Narym and Angara–Vitim batholiths. We have established that despite the different geologic history of