考古时代的大陆地是由地积物形成的
Matthijs A Smit1,2, Kira A Musiyachenko3, Jeroen Goumans3
1Department of Earth, Ocean and Atmospheric Sciences, University of British Columbia, 2020-2207 Main Mall, Vancouver, V6T 1Z4, Canada. msmit@eoas.ubc.ca.
Nature communications
|January 24, 2024
概括
早期大陆地的生长涉及色岩石-三岩石-花岩石 (TTG) 岩. 新的研究揭示了TTG是由原大陆根中的融化累积物形成的,解释了没有外部触发因素的古老地进化.
科学领域:
- 地质化学 地质化学
- 石化学 石化学是一门学科.
- 考古地质学 考古地质学
背景情况:
- 色石-三石-花石 (TTG) 岩对于早期大陆地的生长和化至关重要.
- 石化形成,构造设置和TTG的来源仍然不太清楚.
研究的目的:
- 调查古老TTG的组成和石化过程.
- 使用高场强度元素系统学来理解TTG形成.
主要方法:
- 在TTGs中分析Nb度和Ti异常.
- 检查两类和类的分离效应.
- 限制初级TTG化的组成.
主要成果:
- TTG的组成受到两类和类分离的影响.
- 主要的TTG融是不相容的元素贫乏,具有高的La/Sm,Sm/Yb,Sr/Y和正的Eu异常.
- 化的参数表明不同程度的化和分量结晶,而不是化的深度.
结论:
- 考古时代的TTG起源于原大陆根中融化含有鲁和石榴石的石质积累岩石.
- 这种融过程将TTG岩与桑尼基托伊德和K丰富的花岩形成联系起来.
- 这些过程解释了Archaean大陆地的生长和分化,而没有外部强迫.
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