Meso-Neoarchean Key Magmatic Systems from Karelian Craton: Geochemical Characteristics and Geodynamic Implication

Svetov Sa, Vinod Ks, Chazengina Sy, Rybnikova Zp, Gogolev Ma
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Abstract

The rock assemblages of the Vedlozero-Segozero greenstone belt (Central Karelia) were used as reference pattern for the study of Archean crust-forming processes of the Karelian Craton. This paper presents geochemical and U-Pb (SHRIMP II) zircon dating data for the mafic and andesite rocks. The results obtained by using the approach, based on the analysis of the volcanic rocks, combined with intrusive and sedimentary rocks, maintain the model of the initial stage of the assembling of the Karelian Craton.
卡累利阿克拉通中-新太古代关键岩浆系统:地球化学特征及其地球动力学意义
以中部卡累利阿Vedlozero-Segozero绿岩带的岩石组合为参考模式,研究了卡累利阿克拉通太古宙的地壳形成过程。本文介绍了基性岩和安山岩的地球化学和U-Pb (SHRIMP II)锆石定年资料。该方法在火山岩分析的基础上,结合侵入岩和沉积岩,维持了卡累利阿克拉通初始组装阶段的模型。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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