Geochemistry and geochronology of permo-triassic basites in the northwestern altai-sayan folded area; Geologiya i Geofizika; Vol. 46, N 3

Bibliografiske detaljer
Parent link:Geologiya i Geofizika.— , 2005
Vol. 46, N 3.— 2005.— P. 289-302
Hovedforfatter: Fedoseev G. S.
Andre forfattere: Sotnikov V. I., Rikhvanov L. P. Leonid Petrovich
Summary:Petrogeochemical and isotope-geochronological data are of paramount importance for refining the geologic correlation between weakly exposed magmatites of the Kolyvan'-Tomsk folded zone and Kuznetsk basin. We report data on dike and dike-sill basite complexes of shallow-depth genesis. According to the 40Ar/39Ar age estimates, basites in the Kuznetsk and Gorlovka basins are older than dikes free of xenogenous matter in the Tomsk magmatic area(248.95 ± 1.81- 246.2 ± 1.4, 259.1 ± 3.4, and 241.6 ± 2.7-238.0 ± 5.2 Ma, respectively) and are close in petrogeochemistry to basites of the Tashara complex in the Novosibirsk magmatic area. These data suggest the synchronous occurrence of magmatic events related to the Permo-Triassic plume activity within the West Siberian Plate, Siberian Platform, and their southern folded framing
В фонде НТБ ТПУ отсутствует
Sprog:russisk
Udgivet: 2005
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Format: Book Chapter
KOHA link:https://koha.lib.tpu.ru/cgi-bin/koha/opac-detail.pl?biblionumber=595803

MARC

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200 1 |a Geochemistry and geochronology of permo-triassic basites in the northwestern altai-sayan folded area  |f G. S. Fedoseev , V. I. Sotnikov , L. P. Rikhvanov 
330 |a Petrogeochemical and isotope-geochronological data are of paramount importance for refining the geologic correlation between weakly exposed magmatites of the Kolyvan'-Tomsk folded zone and Kuznetsk basin. We report data on dike and dike-sill basite complexes of shallow-depth genesis. According to the 40Ar/39Ar age estimates, basites in the Kuznetsk and Gorlovka basins are older than dikes free of xenogenous matter in the Tomsk magmatic area(248.95 ± 1.81- 246.2 ± 1.4, 259.1 ± 3.4, and 241.6 ± 2.7-238.0 ± 5.2 Ma, respectively) and are close in petrogeochemistry to basites of the Tashara complex in the Novosibirsk magmatic area. These data suggest the synchronous occurrence of magmatic events related to the Permo-Triassic plume activity within the West Siberian Plate, Siberian Platform, and their southern folded framing 
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461 |t Geologiya i Geofizika  |d 2005 
463 |t Vol. 46, N 3  |v P. 289-302  |d 2005 
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701 1 |a Rikhvanov  |b L. P.  |c Professor of Tomsk Polytechnic University  |c Doctor of geological- mineralogical sciences  |c Honored geologist of Russia  |c Honored employee of higher vocational education of the Russian Federation  |f 1945-  |g Leonid Petrovich  |3 (RuTPU)RU\TPU\pers\25922 
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