Metamorphism, fluid flow, anatexis and the petrogenesis of peraluminous magmas: constraints from boron and lithium elemental and isotopic geochemistry

变质作用、流体流动、深熔作用和过铝质岩浆的岩石成因：硼和锂元素和同位素地球化学的限制

• 批准号: ARC : DP0342473
• 金额: $ 76.63万
• 依托单位: La Trobe University
• 依托单位国家: 澳大利亚
• 项目类别: Discovery Projects
• 财政年份: 2003
• 资助国家: 澳大利亚
• 起止时间: 2003-01-01 至 2008-12-31
• 项目状态: 已结题
• 来源: https://researchdata.edu.au/metamorphism-fluid-flow-isotopic-geochemistry/68091
• 关键词: Metamorphism; fluid; flow; anatexis; petrogenesis

Metamorphism, fluid flow, anatexis and the petrogenesis of peraluminous magmas: constraints from boron and lithium elemental and isotopic geochemistry. Boron (B) and lithium (Li) elemental and isotopic variations are sensitive monitors of metamorphism, fluid flow and melting; the generation of granites; and hydrothermal alteration. However, in detail B- and Li- geochemistry are poorly understood. This project uses field-based, analytical and experimental techniques to constrain B and Li elemental and stable isotope variations in order to better understand high-temperature metamorphism, fluid flow, melting and the generation of granites and pegmatites. The results of this project will greatly increase our understanding of B and Li systematics in high-temperature crustal environments, and have implications for a range of metamorphic and igneous processes.

变质作用、流体流动、深成作用与过铝质岩浆的成因：来自硼、锂元素和同位素地球化学的制约。硼(B)和锂(Li)元素和同位素变化是变质作用、流体流动和熔融、花岗岩生成和热液蚀变的灵敏监测。然而，在细节上，人们对B-和Li-地球化学知之甚少。该项目使用现场、分析和实验技术来约束B和Li元素和稳定同位素的变化，以便更好地了解高温变质作用、流体流动、熔融以及花岗岩和伟晶岩的生成。该项目的研究结果将极大地加深我们对高温地壳环境中B和Li系统学的理解，并对一系列变质作用和火成岩作用具有重要意义。