Výsledky vyhledávání - "G. B. Flerov"

The Generation of Trachytes and Comendites in the Subalkaline Differentiated Series, Sredinnyi Range, Kamchatka

Autor: N. V. Bryansky, G. B. Flerov, A. B. Perepelov, Yu. D. Shcherbakov, M. Yu. Puzankov

Publikováno v: Journal of Volcanology and Seismology. 14:83-95

The main subject of this article is research on the genetic relationships in the K–Na subalkaline series that occurs in the Belogolovsky volcanic center located in the back part of Sredinny Range. The differentiated rock series includes trachybasal

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::54b0fdca60841c7d6a169992ba121339
https://doi.org/10.1134/s0742046320020062

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Space–time relationships between volcanic associations of different alkalinities: The Belogolovskii Massif, Sredinnyi Range, Kamchatka. Part II. Geochemistry of volcanic rocks and magma sources

Autor: A. V. Koloskov, Yu. D. Shcherbakov, A. B. Perepelov, S. V. Palesskii, G. B. Flerov, M. Yu. Puzankov, S. I. Dril

Publikováno v: Journal of Volcanology and Seismology. 10:219-241

Data are presented relating to volcanic series in the Belogolovskii Massif, Sredinnyi Range, Kamchatka. We discuss new geochronologic data, the distributions of rare elements and platinum elements in the rocks, and list the isotope characteristics of

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::b814bd8af46bc7b9e968c933b42b3a84
https://doi.org/10.1134/s0742046316040023

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The petrogenesis of rocks of the Ostryi and Ploskii volcanoes and the relationship between volcanic occurrences of basaltic and trachybasaltic magmas in the Tolbachik Dol area, Kamchatka

Autor: G. P. Ponomarev, V. V. Anan’ev, G. B. Flerov

Publikováno v: Journal of Volcanology and Seismology. 9:162-181

We developed a petrologic and geodynamic model for the magma generation of volcanic formations in the Tolbachik Dol area. Differences have been found in the evolution of volcanic ejecta and the mineral composition of rocks on Ostryi and Ploskii Tolba

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https://doi.org/10.1134/s0742046315030021

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The evolutionary stages and petrology of the kekuknai volcanic massif reflecting the magmatism in the backarc zone of the kuril-kamchatka island arc system. Part II. petrologic and mineralogical features, petrogenesis model

Autor: G. B. Flerov, I. V. Melekestsev, M. Yu. Puzankov, T. M. Filosofova, A. B. Perepelov, A. V. Koloskov

Publikováno v: Journal of Volcanology and Seismology. 7:145-169

The Kekuknai massif was formed in the course of tectono-magmatic activity that involved the origin of a shield volcano and a caldera depression with associated emplacement of extrusions that terminated in intense post-caldera areal volcanism. The min

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::831146e7296e5301cf3bafbf7ebca442
https://doi.org/10.1134/s0742046313020048

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Late Cretaceous-Paleocene magmatic complexes of central Kamchatka: Geological settings and compositional features

Autor: V. A. Koloskov, G. B. Flerov, D. V. Kovalenko

Publikováno v: Russian Journal of Pacific Geology. 3:319-337

A comparative analysis of the Late Cretaceous-Paleocene volcanism was conducted for four areas of Kamchatka: the Pravyi Tolbachik-Levaya Shchapina-Adrianovka interlfuve (the northern part of the Tumrok Range), the area south of the Ipuin River and Mt

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https://doi.org/10.1134/s1819714009040022

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The Cretaceous-Paleogene magmatism of the Sredinnyi range of Kamchatka: Magma sources

Autor: V. A. Seliverstov, G. B. Flerov

Publikováno v: Journal of Volcanology and Seismology. 2:71-82

Based on published and new data, a new petrological model of the preorogenic Late Cretaceous-Paleogene intrusive rock association is suggested. The principle of plume geodynamics is the essential one: homodromous intrusion of dunite-clinopyroxenite-g

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::b7c8d5077efaadc4e7636e9e69981289
https://doi.org/10.1134/s0742046308020012

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The space-time relationships between volcanic associations of different alkalinities: The Belogolovskii massif in Kamchatka’s Sredinnyi Range. Part 1. The geology, mineralogy, and petrology of volcanic rocks

Autor: A. B. Perepelov, A. V. Koloskov, T. M. Filosofova, Yu. D. Shcherbakov, M. Yu. Puzankov, G. B. Flerov

We proposed a geological and petrologic model for the generation of the Belogolovskii Late Pliocene to Early Pleistocene volcanic massif. We identified two petrochemical series of rocks with varying alkalinities, viz., normal and moderate. The evolut

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Evolution Stages and Petrology of the Kekuknai Volcanic Massif as Reflecting the Magmatismin Backarc Zone of Kuril-Kamchatka Island Arc System. Part 1. Geological Position and Geochemistry of Volcanic Rocks

Autor: A. V. Koloskov, G. B. Flerov, T. M. Filosofova, M. Yu. Puzankov, A. B. Perepelov, I. V. Melekestsev

The evolution of the Quaternary Kekuknai volcanic massif (the western flank of the Sredinnyi Range in Kamchatka) has been subdivided into five stages: (I) the pre-caldera trachybasalt- basaltic andes- ite, (2) the extrusive trachyandesite-trachydacit

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