The 2405 Ma and 2310 Ma Mafic Dyke Swarms in the Karelian Craton: Age, Chemical and Sr-Nd Isotope Composition, and Tectonic Setting

被引:0
|
作者
Stepanova A.V. [1 ]
Salnikova E.B. [2 ]
Samsonov A.V. [3 ]
Larionova Yu.O. [3 ]
Egorova S.V. [1 ]
Stepanov V.S. [1 ]
机构
[1] IG Kar RC RAS
[2] IPGG RAS
[3] IGEM RAS
关键词
Nd; Sr; and Tectonic Setting; Age;
D O I
暂无
中图分类号
P597.3 []; P542 [构造运动];
学科分类号
070902 ; 070904 ;
摘要
Until recently the time period 2400-2200 Ma in the Erath history was characterized by low amount of age data for igneous events,and was even considered as‘magmatic age gap’(Condie et al,2009;Eriksson and Condie,2014).
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页码:123 / 123
页数:1
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