Middle Paleozoic and Early Mesozoic anorogenic magmatism of the South Yenisei Ridge: first geochemical and geochronological data

被引:11
|
作者
Vernikovskaya, A. E. [1 ]
Vernikovsky, V. A. [1 ]
Matushkin, N. Yu. [1 ]
Romanova, I. V. [1 ]
Berejnaya, N. G. [2 ]
Larionov, A. N. [2 ]
Travin, A. V. [3 ]
机构
[1] Russian Acad Sci, AA Trofimuk Inst Petr Geol & Geophys, Siberian Branch, Novosibirsk 630090, Russia
[2] AP Karpinsky Russian Geol Res Inst, St Petersburg 199106, Russia
[3] Russian Acad Sci, VS Sobolev Inst Geol & Mineral, Siberian Branch, Novosibirsk 630090, Russia
基金
俄罗斯基础研究基金会;
关键词
South Yenisei Ridge; Yenisei suture zone; alkaline syenites and trachytes; A-type leucogranites; U-Pb and Ar-Ar geochronology; continental rifting; WESTERN MARGIN; SIBERIAN CRATON; GEODYNAMIC EVOLUTION; TRACE-ELEMENT; PB; NOMENCLATURE; AGE; ACCRETIONARY; AMPHIBOLES; EVENTS;
D O I
10.1016/j.rgg.2010.04.010
中图分类号
P [天文学、地球科学];
学科分类号
07 ;
摘要
In this paper we present complex geological, petrographic and geochronological data of the study of intermediate and acid composition intrusive and volcanogenic rocks from the Porozhnaya massif of the South Yenisei Ridge. For the first time in the Yenisei Ridge Devonian and Triassic U-Pb age values (SHRIMP method) have been obtained for leucogranites-387 +/- 5 Ma and alkaline trachytes-240 +/- 3 Ma, which allows us to attribute them to two different complexes, despite the fact that these rocks were formed within the same Severnaya riftogenic structure. Geochronological Ar-Ar data (392-387 Ma) for micas from paragneisses and leucogranitic dikes of the Yenisei suture zone on whose extension the Severnaya riftogenic structure is located are also given in this study. These data on Devonian tectonic-magmatic events in the South Yenisei Ridge agree well with coeval events of continental rifting-the formation of intrusive and volcanogenic rocks of the Agul graben in the Prisayan region and the Minusa basin in the Altai-Sayan folded area. The forming of alkaline trachytes and alkaline syenites of the Severnaya riftogenic structure, for which an age of 240 +/- 3 Ma has been established, is related to the trap magmatism of the Siberian platform. (C) 2010, V. S. Sobolev IGM, Siberian Branch of the RAS. Published by Elsevier B. V. All rights reserved.
引用
收藏
页码:548 / 562
页数:15
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