Zobrazeno 1 - 10
of 10
pro vyhledávání: '"O. N. Volynets"'
Publikováno v:
Nature. 409:500-504
Most island-arc magmatism appears to result from the lowering of the melting point of peridotite within the wedge of mantle above subducting slabs owing to the introduction of fluids from the dehydration of subducting oceanic crust. Volcanic rocks in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7ee011e0c9cc858bd842c998ffd8e1da
https://doi.org/10.1038/35054039
https://doi.org/10.1038/35054039
Publikováno v:
Geological Society of America Bulletin. 107:505-519
The role of the subducting lithospheric slab in the genesis of mantle-derived (primitive) magmas is investigated through a study of volcanic rocks formed in the tectonically strike-slip–dominated western Aleutian arc. Two types of chemically and pe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::24ea5aadedd74f954d051ef53ed006e6
https://doi.org/10.1130/0016-7606(1995)107<0505:maitwa>2.3.co
https://doi.org/10.1130/0016-7606(1995)107<0505:maitwa>2.3.co
Publikováno v:
Journal of Petrology. 35:163-204
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8c0a6a56e72e11faffa26b66f7f93dcf
https://doi.org/10.1093/petrology/35.1.163
https://doi.org/10.1093/petrology/35.1.163
Publikováno v:
Tectonophysics. 199:271-287
This study discusses the structural and spatial characteristics of all known Kurile island-arc Quaternary volcanoes, which include 105 that are subaerial and 96 submarine. Volcanic activity in the island arc is distributed in two zones parallel to th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::de4690fc5253a943e56d6fc81639bfd8
https://doi.org/10.1016/0040-1951(91)90175-r
https://doi.org/10.1016/0040-1951(91)90175-r
Autor:
O. N. Volynets, G. P. Avdeyko, N. G. Gladkov, V. V. Anan'yev, A. Yu. Antonov, A. A. Tsvetkov, I. A. Markov
Publikováno v:
International Geology Review. 32:321-337
(1990). ULTRAMAFIC INCLUSIONS IN THE QUATERNARY LAVAS OF THE KURILEISLAND ARC. International Geology Review: Vol. 32, No. 4, pp. 321-337.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c4ba8624a9ac7d2b82eeba7019416d18
https://doi.org/10.1080/00206819009465780
https://doi.org/10.1080/00206819009465780
Autor:
I. A. Markov, O. N. Volynets, G. P. Avdeyko, T. M. Filosofova, A. Yu. Antonov, A. A. Tsvetkov
Publikováno v:
International Geology Review. 32:128-142
(1990). MINERAL ZONING OF THE QUATERNARY LAVAS OF THE KURILE ISLAND ARC. International Geology Review: Vol. 32, No. 2, pp. 128-142.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a61935414fe9ad59e737ce8d52ce3a43
https://doi.org/10.1080/00206819009465763
https://doi.org/10.1080/00206819009465763
Autor:
O. N. Volynets, A. A. Tsvetkov
Publikováno v:
Isotopenpraxis Isotopes in Environmental and Health Studies. 26:603-607
Concentrations of 10 Be were measured in 23 lava samples representing historically and 14C dated eruptions of major Kurile and Kamchatka volcanoes. We report 2.2–7.9 · 106 at/g of 10Be for Kuriles and in most cases less than 1.2 · 106 at/g for Ka
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d2adb5695d8a3ea62d66d6c10b48c210
https://doi.org/10.1080/10256019008622445
https://doi.org/10.1080/10256019008622445
The combination of geological, tephrochronological and geochemical studies is used to reconstruct the Holocene eruptive history of Ksudach volcanic massif, South Kamchatka and to trace the evolution of its magma. Ksudach is located in the frontal vol
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c2db0cc7b87f848140693cca076ec0af
http://repo.kscnet.ru/1032/1/jvgr_ks_99.pdf
http://repo.kscnet.ru/1032/1/jvgr_ks_99.pdf
Autor:
B. G. Pokrovsky, O. N. Volynets
Publikováno v:
Chinese Science Bulletin. 43:102-102
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::16a7f2754c0acce0c42a4493725cbd62
https://doi.org/10.1007/bf02891546
https://doi.org/10.1007/bf02891546
Publikováno v:
International Geology Review. 31:1107-1122
(1989). PETROLOGICAL AND TEPHROCHRONOLOGICAL STUDIES OF KRASHENINNIKOV VOLCANO, KAMCHATKA. International Geology Review: Vol. 31, No. 11, pp. 1107-1122.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0a661ccdfb59d98aec459cfc60e7d899
https://doi.org/10.1080/00206818909465964
https://doi.org/10.1080/00206818909465964