4.7 Article Proceedings Paper

Non-traditional fractionation of non-traditional isotopes: Evaporation, chemical diffusion and Soret diffusion

Journal

CHEMICAL GEOLOGY
Volume 258, Issue 1-2, Pages 92-103

Publisher

ELSEVIER
DOI: 10.1016/j.chemgeo.2008.06.011

Keywords

Isotope fractionation; Evaporation; Chemical diffusion; Thermal diffusion; Grain boundary diffusion

Ask authors/readers for more resources

Recent developments documenting high temperature isotope fractionations of a variety of elements (Li, Mg, Si, Ca, Fe, Ni) by a variety of processes (evaporation, chemical diffusion and thermal diffusion) are reviewed along with some recent applications of these fractionations to Earth and meteoritic problems. (C) 2008 Elsevier B.V. All rights reserved.

Authors

I am an author on this paper
Click your name to claim this paper and add it to your profile.

Reviews

Primary Rating

4.7
Not enough ratings

Secondary Ratings

Novelty
-
Significance
-
Scientific rigor
-
Rate this paper

Recommended

Article Multidisciplinary Sciences

Nickel isotopic evidence for late-stage accretion of Mercury-like differentiated planetary embryos

Shui-Jiong Wang, Wenzhong Wang, Jian-Ming Zhu, Zhongqing Wu, Jingao Liu, Guilin Han, Fang-Zhen Teng, Shichun Huang, Hongjie Wu, Yujian Wang, Guangliang Wu, Weihan Li

Summary: During Earth's late-stage accretion, impactors delivered most of the volatiles, with nickel serving as an important tracer. Research has found that the BSE has a lighter nickel isotopic composition compared to chondrites, suggesting that this sub-chondritic signature was established during the Moon-forming giant impact.

NATURE COMMUNICATIONS (2021)

Article Geochemistry & Geophysics

Potassium isotopic composition of various samples using a dual-path collision cell-capable multiple-collector inductively coupled plasma mass spectrometer, Nu instruments Sapphire

Frederic Moynier, Yan Hu, Kun Wang, Ye Zhao, Yvan Gerard, Zhengbin Deng, Julien Moureau, Weiqiang Li, Justin I. Simon, Fang-Zhen Teng

Summary: The Nu SapphireTM MC-ICP-MS is a high-precision instrument for measuring potassium isotopes, effectively addressing major isobaric interferences and providing high potassium sensitivity. The precision and accuracy of potassium isotopic data are influenced by several parameters, including total potassium concentration, matching of potassium intensities between sample and standard, and the presence of matrix elements.

CHEMICAL GEOLOGY (2021)

Article Geochemistry & Geophysics

Potassium isotopic evidence for sedimentary input to the mantle source of Lesser Antilles lavas

Yan Hu, Fang-Zhen Teng, Catherine Chauvel

Summary: This study used stable potassium isotopes to track the crustal signatures in lavas from Martinique Island in the Lesser Antilles arc. The results show that the variations in K isotopes in these lavas are related to chemical parameters and radiogenic isotope ratios, indicating modification of mantle sources by input of subducted sediments. Most lavas have <1% to 5% of subducted sediments added to their mantle sources, with some samples showing divergence likely caused by the addition of K-bearing fluids from slab dehydration.

GEOCHIMICA ET COSMOCHIMICA ACTA (2021)

Article Geochemistry & Geophysics

Permian ridge subduction in the easternmost Central Asian Orogenic Belt: Magmatic record using Sr-Nd-Pb-Hf-Mg isotopes

Feng Wang, Kai-Chen Xing, Wen-Liang Xu, Fang-Zhen Teng, Yi-Gang Xu, De-Bin Yang

Summary: The Khanka Massif in late Paleozoic is considered as an ideal site to trace fossil ridge-subduction, with different types of Permian igneous rocks showing evidence of subduction setting. The isotope compositions of the rocks support the hypothesis of abnormal high-heat conditions caused by ridge subduction and resultant slab window.

LITHOS (2021)

Article Geochemistry & Geophysics

Potassium Isotope Fractionation During Magmatic Differentiation and the Composition of the Mantle

Yan Hu, Fang-Zhen Teng, Rosalind T. Helz, Catherine Chauvel

Summary: Stable potassium isotopes are being used as tracers for terrestrial recycling and planetary processes. This study investigated K isotope fractionation during the differentiation and solidification of the Kilauea Iki lava lake in Hawaii, and found no analytically resolvable fractionation, indicating a lack of K-rich minerals in the crystallizing assemblage. The results suggest an average delta K-41 of -0.42 +/- 0.08 parts per thousand for the pristine mantle and of -0.42 +/- 0.07 parts per thousand for the BSE.

JOURNAL OF GEOPHYSICAL RESEARCH-SOLID EARTH (2021)

Article Geochemistry & Geophysics

Multistage mantle metasomatism deciphered by Mg-Sr-Nd-Pb isotopes in the Leucite Hills lamproites

Yang Sun, Fang-Zhen Teng, Kwan-Nang Pang, Ji-Feng Ying, Scott Kuehner

Summary: The study investigates the origin of EMI reservoir by analyzing the isotopic compositions of lamproites from Leucite Hills, Wyoming, USA, finding that at least two metasomatic events occurred in their mantle sources. The early metasomatic event led to the formation of EMI Sr-Nd-Pb isotopic signatures, while the recent carbonate metasomatism produced the light Mg isotopic signature and diluted the EMI Sr-Nd-Pb isotopic signatures. This study suggests that a combination of Mg and Sr-Nd-Pb isotopes could be an effective tool in deciphering multiple-stage metasomatic events in mantle sources.

CONTRIBUTIONS TO MINERALOGY AND PETROLOGY (2021)

Article Geochemistry & Geophysics

Evidence from HP/UHP metasediments for recycling of isotopically heterogeneous potassium into the mantle

Ze-Zhou Wang, Fang-Zhen Teng, Vincent Busigny, Sheng-Ao Liu

Summary: The study demonstrates that potassium isotopic signatures in subducting sediments, inherited from their protoliths, can be preserved to depths of at least 90 km along a cold geotherm gradient, indicating the potential for producing potassium isotope heterogeneity in the source regions of mantle-derived lavas.

AMERICAN MINERALOGIST (2022)

Article Geosciences, Multidisciplinary

High-precision and high-accuracy magnesium isotope analysis on multiple-collector inductively coupled plasma mass spectrometry using a critical mixture double spike technique

Yongsheng He, Ai-Ying Sun, Yin -Chu Zhang, Ru-Yi Yang, Shan Ke, Yang Wang, Fang-Zhen Teng

Summary: A new procedure for high precision and high accuracy Mg isotope analysis has been developed using a critical mixture double spike technique and multiple-collector inductively coupled plasma mass spectrometry. The accuracy is ensured by correcting errors arising from improper preparation of the double spike solutions and correcting mass bias offset based on Monte Carlo calculations. Doping experiments show that the method is robust to non-spectrum matrix effects.

SOLID EARTH SCIENCES (2022)

Article Geosciences, Multidisciplinary

High-precision potassium isotope analysis using the Nu Sapphire collision cell (CC)-MC-ICP-MS

Wenjun Li, Mengmeng Cui, Qiqi Pan, Jing Wang, Bingyu Gao, Shanke Liu, Meng Yuan, Benxun Su, Ye Zhao, Fang-Zhen Teng, Guilin Han

Summary: This study presents high-precision analyses of stable potassium (K) isotope ratio using advanced technology. The accuracy of the analyses is confirmed by measuring well-characterized geostandards. The findings suggest that stable K isotopes can be used as an indicator of ancient seawater composition and have various geological applications.

SCIENCE CHINA-EARTH SCIENCES (2022)

Article Geochemistry & Geophysics

Multi-mode chemical exchange in seafloor alteration revealed by lithium and potassium isotopes

Heng-Ci Tian, Fang-Zhen Teng, Xin-Yang Chen, Zi-Xiao Guo, Xiao-Tong Peng, Wei Yang, Yi-Lin Xiao

Summary: Elemental exchange during seafloor alteration has significant effects on the chemical compositions of seawater and oceanic crust, as well as global elemental cycling. This study investigates Li and K isotopic compositions in an altered pillow basalt from Mariana Trench, revealing large isotopic variations on a centimeter scale and providing evidence for multi-mode chemical exchange in oceanic basalts. This research enhances our understanding of seafloor alteration processes.

CHEMICAL GEOLOGY (2022)

Article Geochemistry & Geophysics

High-latitude climatic response across the Triassic-Jurassic boundary recorded by Mg-Cu-Zn isotopes

Kai -Chen Xing, Feng Wang, Fang-Zhen Teng, Wen-Liang Xu, Ming Li, Yue-Wu Sun, De-Bin Yang

Summary: The Triassic-Jurassic boundary is a crucial period for studying chemical weathering intensity and climatic change. In this study, Mg-Zn-Cu isotopic data from a terrestrial sedimentary section in the southern margin of the Junggar Basin in high latitude Asia are analyzed, revealing a reduced sedimentary environment and increasingly intensive chemical weathering across the boundary, responding to a warmer and more humid paleoclimate. This regional climatic change in high latitude areas can be linked to known global climate change during this period, providing new insights into the global pattern of climate change at the Triassic-Jurassic boundary.

CHEMICAL GEOLOGY (2022)

Article Geochemistry & Geophysics

Potassium isotope fractionation during chemical weathering in humid and arid Hawaiian regoliths

Wenshuai Li, Xiao-Ming Liu, Yan Hu, Fang-Zhen Teng, Oliver A. Chadwick

Summary: The controls on potassium (K) isotope fractionation during chemical weathering are evaluated using two regolith profiles developed over -350 kyr on the humid and arid sides of Kohala Mountain, Hawai'i. The findings suggest that potassium enrichment and loss occur in both regolith profiles, with the humid profile showing significant potassium enrichment in shallow horizons and loss in deeper horizons. The presence of K-bearing mineral aerosols in the humid regolith may explain the apparent contradiction between enrichment and loss. Climate, weathering, plant cycling, and the addition of marine and mineral aerosols all contribute to the potassium isotope composition in Hawaiian regoliths.

GEOCHIMICA ET COSMOCHIMICA ACTA (2022)

Article Geochemistry & Geophysics

Petrogenesis of the Paleogene potassium-rich volcanic rocks in the western Yangtze Craton, southeastern Tibetan Plateau

Hangshan Lei, Zhidan Zhao, Qian Ma, Fang-Zhen Teng, Shuangquan Zhang, Brian Cousens, Dong Liu, Di-Cheng Zhu, Qing Wang, Zhuang Miao, Yiyun Yang, Jingkai Wu

Summary: Paleogene potassium-rich volcanic rocks (PVRs) in the southeastern Tibetan Plateau are studied to understand their petrogenesis and geodynamic mechanism. The PVRs are found to originate from enriched lithospheric mantle, possibly replenished by a hybrid carbonate-silicic sediment. The formation of these volcanic rocks is closely associated with the delamination of the thickened lithosphere and asthenosphere upwelling.

LITHOS (2022)

Article Geochemistry & Geophysics

Iron isotope evidence for siderite precursors to iron oxide concretions from the Navajo Sandstone, Utah (USA)

Richard M. Kettler, Yongsheng He, Shan Ke, Fang-Zhen Teng, David B. Loope

Summary: The discovery of spherical accumulations of iron oxide mineralization on Mars has led to renewed interest in similar accumulations on Earth. This study focuses on the rinded iron oxide concretions found in the Navajo Sandstone and evaluates four different models for their formation. The authors measured the iron isotope values of different iron-bearing minerals and combined their data with published measurements to assess each model. The results suggest a complex process involving the transport and oxidation of iron in a closed system.

CHEMICAL GEOLOGY (2022)

Meeting Abstract Geochemistry & Geophysics

A Condensation Origin of Potassium and Rubidium Isotopic Variations in Carbonaceous Chondrites

N. X. Nie, X. -Y. Chen, T. Hopp, J. Y. Hu, Z. J. Zhang, F. -Z. Teng, A. Shahar, N. Dauphas

METEORITICS & PLANETARY SCIENCE (2021)

Article Geochemistry & Geophysics

Metasomatized mantle source of nascent oceanic crust in the Guaymas Basin, Gulf of California

Zhen-Min Ge, Xiao-Long Huang, Wei Xie, Tobias W. Hofig, Fan Yang, Yang Yu, S. Khogenkumar Singh

Summary: The mantle source composition of the nascent oceanic crust in the central part of the Gulf of California has been investigated using basaltic glass samples. These samples show trace element patterns similar to enriched mid-ocean ridge basalts, suggesting that the nascent oceanic crust in the Guaymas Basin might be generated through partial melting of a depleted mantle source metasomatized by subducted slab materials.

CHEMICAL GEOLOGY (2024)

Article Geochemistry & Geophysics

Effect of mineral growth rate on Zinc incorporation into calcite and aragonite

Jean-Michel Brazier, Katja E. Goetschl, Martin Dietzel, Vasileios Mavromatis

Summary: This study estimated the distribution coefficient of Zn2+ between calcite/aragonite and reactive fluids and found that the growth rate strongly influences D-Zn(2+) in both minerals. Additionally, a linear correlation was found between D-Zn(2+) and the saturation degree of the reactive fluid.

CHEMICAL GEOLOGY (2024)

Article Geochemistry & Geophysics

Miocene olivine leucitites in southern Tibet: Implications for the recycling of carbonates into the mantle during continental subduction

Ming Lei, Michele Lustrino, Jifeng Xu, Zhiqiang Kang, Zhengfu Guo, Jianlin Chen

Summary: This study presents a comprehensive geochronological, mineralogical, and geochemical analysis of olivine leucitites in the Maiga area of southern Tibet, suggesting that these rocks originate from a carbonated peridotite mantle source and highlighting the possibility of carbonates being recycled deep into the mantle during continental subduction.

CHEMICAL GEOLOGY (2024)

Article Geochemistry & Geophysics

Phosphate oxygen isotopes constrain Mesoproterozoic marine temperatures and the paucity of phosphorite

Yuntao Ye, Xiaomei Wang, Huajian Wang, Haifeng Fan, Zhigang Chen, Qingjun Guo, Ziteng Wang, Chaodong Wu, Donald E. Canfield, Shuichang Zhang

Summary: Phosphorus is an essential element for life and its cycle in the ocean is closely connected with the carbon and oxygen cycles. The study of phosphate oxygen isotopes can provide insights into various reactions related to phosphorus. By analyzing carbonate fluorapatite samples from the Mesoproterozoic Era in North China, it was found that the oxygen isotope values were lower compared to modern samples, indicating a warmer climate during that time period and a potential reason for the scarcity of phosphorite.

CHEMICAL GEOLOGY (2024)

Article Geochemistry & Geophysics

Preservation of organic C and N isotope signatures from water column to sediments in the anoxic and ferruginous Pavin lake

Vincent Busigny, Oanez Lebeau, Didier Jezeduel, Carine Chaduteau, Sean Crowe, Magali Ader

Summary: This study conducted high-precision Mo isotope research on hydrothermal metal sulfides from a porphyry copper deposit in Southwest China and found that different stages of mineralization have distinct Mo isotope compositions, providing valuable insights into the behavior of Mo isotopes in magmatic-hydrothermal systems.

CHEMICAL GEOLOGY (2024)

Article Geochemistry & Geophysics

Geochemical variations of anatectic melts in response to changes of P-T-H2O conditions: Implication for the relationship between dehydration and hydration melting in the Himalayan orogen

Min Ji, Xiao-Ying Gao, Yong-Fei Zheng, Bing Gong

Summary: The study examines the anatectic mechanisms in the Himalayan orogen, finding that pressure and temperature control the reaction, while water content mainly affects the solid-phase composition. Dehydration and hydration melting likely occur at different depths in the crust. This research provides important insights into the melting processes in collisional orogens.

CHEMICAL GEOLOGY (2024)