The Geochemical Effect of Lanthanides: Its Types and Application for Magmatic Rocks—A New Method to Semi-Quantitatively Determine Strength of Magmatic Fluid Complexation and Fractional Crystallization

Jianye Yang; Lei Zhao; Weiguo Zhang

doi:10.1007/s12583-014-0420-z

Volume 25 Issue 2

Apr 2014

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Journal of Earth Science > 2014 > 25(2): 252-262.

Jianye Yang, Lei Zhao, Weiguo Zhang. The Geochemical Effect of Lanthanides: Its Types and Application for Magmatic Rocks—A New Method to Semi-Quantitatively Determine Strength of Magmatic Fluid Complexation and Fractional Crystallization. Journal of Earth Science, 2014, 25(2): 252-262. doi: 10.1007/s12583-014-0420-z

Citation:

Jianye Yang, Lei Zhao, Weiguo Zhang. The Geochemical Effect of Lanthanides: Its Types and Application for Magmatic Rocks—A New Method to Semi-Quantitatively Determine Strength of Magmatic Fluid Complexation and Fractional Crystallization. Journal of Earth Science, 2014, 25(2): 252-262. doi: 10.1007/s12583-014-0420-z

Citation:

Jianye Yang, Lei Zhao, Weiguo Zhang. The Geochemical Effect of Lanthanides: Its Types and Application for Magmatic Rocks—A New Method to Semi-Quantitatively Determine Strength of Magmatic Fluid Complexation and Fractional Crystallization. Journal of Earth Science, 2014, 25(2): 252-262. doi: 10.1007/s12583-014-0420-z

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The Geochemical Effect of Lanthanides: Its Types and Application for Magmatic Rocks—A New Method to Semi-Quantitatively Determine Strength of Magmatic Fluid Complexation and Fractional Crystallization

doi: 10.1007/s12583-014-0420-z

1.
College of Material Science and Engineering, Xi'an University of Science and Technology, Xi'an, 710054, China
2.
State Key Laboratory of Coal Resources and Safe Mining, Beijing, 100083, China
3.
College of Geology and Environment, Xi'an University of Science and Technology, Xi'an, 710054, China

More Information

Corresponding author: Jianye Yang, yjyxust@163.com
Received Date: 21 Jul 2013
Accepted Date: 27 Oct 2013
Publish Date: 01 Apr 2014

Abstract

Abstract

In this paper, the relationship between rare earth elements (REEs) geochemical behavior and their ionic radii was studied. According to the basic law called the effect on geochemistry of lanthanides, five types and some of subtypes of REEs occurrence, both in magmatic rocks and their minerals, were found, which may correspond to the evolutionary way of magmatic rocks. Analysis of REEs data for an amazonite-topaz granite pluton in East Xinjiang, one of the administrative regions of West China, and Cenozoic alkaline volcanic-intrusive rocks in the Xialiaohe depression of Bohai Bay Basin, China show that types Ⅱ1, Ⅲ and Ⅳ of effect on geochemistry of lanthanides not only reflect fluid complexation and fractional crystallization existed in magmatic evolution directly, but also can determine semi-quantitatively the strength of fluid complexation and fractional crystallization. Therefore, the effect on geochemistry of lanthanides, a new way to study semi-quantitatively evolution of magmatic rocks, is probably practicable. Moreover, the mafic lavas of different sources from the margin of Gonghe Basin, Qinghai Province, China, can be effectively distinguished in the diagram which can be drawn with some parameters of linear equation of LREEs and its ion radius.

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