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李曙光院士论文选集(卷2金属稳定同位素示踪深部碳循环研究)(精)
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湖南大学
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  • ISBN:
    9787030775634
  • 作      者:
    编者:李曙光//刘盛遨//杨蔚|责编:焦健
  • 出 版 社 :
    科学出版社
  • 出版日期:
    2024-11-01
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内容介绍
本卷有选择地汇集了李曙光研究团队2012~2022年在金属稳定同位素示踪深部碳循环方面的主要学术论文。本卷汇集的论文涉及金属同位素分析测试方法的建立,标定地质储库的同位素组成和地质过程的同位素分馏,以及应用Mg-Zn-Fe等金属同位素示踪深部碳-氧循环的实例研究等,探讨了俯冲和岩浆过程中金属同位素行为,不同俯冲带和不同俯冲深度的深部碳循环过程以及再循环碳酸盐种属及通量等许多重要科学问题。这些论文大部分发表在高水平期刊上,引用率高。其中论文(Lietal.,2017,NSR)被NSR评为2019最佳论文。 本文集所收集论文源自多种学术期刊,各源刊格式标准可能不统一,本着尊重历史、忠于原文的精神,所用物理量单位、符号、图例、参考文献等尽量保留了原文风貌。 本书可供地质学领域科技工作者和相关领域教师、研究生与本科生参考。
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目录
前言
第一部分 非传统稳定同位素分析方法
High-precision copper and iron isotope analysis of igneous rock standards by MC-ICP-MS
High-precision iron isotope analysis of geological reference materials by high-resolution MC-ICP-MS
Mass-independent and mass-dependent Ca isotopic compositions of thirteen geological reference materials measured by thermal ionization mass spectrometry
High-precision measurement of stable Cr isotopic in geological reference materials by double-spike TIMS method
第二部分 地质储库的金属稳定同位素组成
Magnesium isotopic compositions of altered oceanic basalts and gabbros from IODP Site 1256 at the East Pacific Rise
The behavior of magnesium isotopes in low-grade metamorphosed mudrocks
Magnesium isotopic heterogeneity across the cratonic lithosphere in eastern China and its origins
第三部分 地质过程中的金属稳定同位素分馏行为
Copper and iron isotope fractionation during weathering and pedogenesis: Insights from saprolite pro?les
Magnesium isotopic systematics of mafic rocks during continental subduction
Tracing carbonate-silicate interaction during subduction using magnesium and oxygen isotopes
Copper isotope fractionation during adsorption onto kaolinite: Experimental approach and applications
Copper and zinc isotope fractionation during deposition and weathering of highly metalliferous black shales in central China
Magnesium isotope fractionation during dolostone weathering
Mineral composition control on inter-mineral iron isotopic fractionation in granitoids
Diffusion-driven magnesium and iron isotope fractionation at a gabbro-granite boundary
Diffusion-driven extreme Mg and Fe isotope fractionation in Panzhihua ilmenite: Implications for the origin of mafic intrusion
Origins of two types of Archean potassic granite constrained by Mg isotopes and statistical geochemistry:
Implications for continental crustal evolution
Large Mg-Fe isotope fractionation in volcanic rocks from northeast China: The role of chemical weathering and magma compositional effect
Zinc isotopic behavior of mafic rocks during continental deep subduction
Zinc isotope fractionation between Cr-spinel and olivine and its implications for chromite crystallization during magma differentiation
Magnesium isotope geochemistry of the carbonate-silicate system in subduction zones
Chromium isotope fractionation during magmatic processes: Evidence from mid-ocean ridge basalts
第四部分 金属稳定同位素示踪深部碳循环
Magnesium isotopic systematics of continental basalts from the North China craton:Implications for tracing subducted carbonate in the mantle
Magnesium isotopic variations in cratonic eclogites:Origins and implications
深部碳循环的Mg同位素示踪
Origin of low δ26Mg Cenozoic basalts from South China Block and their geodynamic implications
Magnesium isotope evidence for a recycled origin of cratonic eclogites
Mg, Sr, and O isotope geochemistry of syenites from northwest Xinjiang, China:Tracing carbonate recycling during Tethyan oceanic subduction
Zinc isotope evidence for a large-scale carbonated mantle beneath eastern China
Origin of low δ26Mg basalts with EM-I component: Evidence for interaction between enriched lithosphere and carbonated asthenosphere
Deep carbon cycles constrained by a large-scale mantle Mg isotope anomaly in eastern China
Could sedimentary carbonates be recycled into the lower mantle? Constraints from Mg isotopic composition of Emeishan basalts
Tracing subduction zone fluid-rock interactions using trace element and Mg-Sr-Nd isotopes
中国东部大地幔楔形成时代和华北克拉通岩石圈减薄新机制—深部再循环碳的地球动力学效应
Subducted Mg-rich carbonates into the deep mantle wedge
Low δ26Mg volcanic rocks of Tengchong in Southwestern China: A deep carbon cycle induced by supercritical liquids
Compositional transition in natural alkaline lavas through silica-undersaturated melt—lithosphere interaction
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