Weiqiang Li (0000-0003-2648-7630)

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Isotope geochemist. Expertise: Stable isotope geochemistry of Cu isotopes, Mg isotopes, and Fe isotopes; Radiogenic iostope geochemistry of U-Th-Pb system; Laser ablation technique and isotope spike technique. Area of interest: experimental determination of isotope fractionation factors; mineral deposits; Archean geology; Weathering and aqueous geochemistry.

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Nanjing University: Nanjing, Jiangsu Province, CN

2014-12-01 to present | Professor (School of Earth Sciences and Engineering)

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Weiqiang Li

https://orcid.org/0000-0003-2648-7630

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Employment (2)

Nanjing University: Nanjing, Jiangsu Province, CN

University of Wisconsin Madison: Madison, WI, US

Education and qualifications (1)

Macquarie University: Sydney, NSW, AU

Works (47)

Cu isotope systematics of conduit-type Cu–PGE mineralization in the Eastern Gabbro, Coldwell Complex, Canada

Dissolved Thorium Isotope Evidence for Export Productivity in the Subtropical North Pacific During the Late Quaternary

Fingerprinting hydrothermal fluids in porphyry Cu deposits using K and Mg isotopes

Isotopic fingerprinting of dissolved iron sources in the deep western Pacific since the late Miocene

Stable potassium isotope geochemistry and cosmochemistry,钾稳定同位素研究综述

Extracting Mg isotope signatures of ancient seawater from marine halite: A reconnaissance

On the coordination of Mg2+ in aragonite: Ab-initio absorption spectroscopy and isotope fractionation study

Termination of Cryogenian ironstone deposition by deep ocean euxinia

Isobaric Spike Method for Absolute Isotopic Ratio Determination by MC-ICP-MS

Transformation of amorphous precursor to crystalline carbonate: Insights from Mg isotopes in the dolomite-analogue mineral norsethite [BaMg(CO3)2]

Calibrating equilibrium Fe isotope fractionation factors between magnetite, garnet, amphibole, and biotite

Reactive iron isotope signatures of the East Asian dust particles: Implications for iron cycling in the deep North Pacific

Sn isotope fractionation during volatilization of Sn(IV) chloride: Laboratory experiments and quantum mechanical calculations

Conservative behavior of Mg isotopes in massive dolostones: From diagenesis to hydrothermal reworking

The Neoproterozoic “Blood Falls” in Tarim Craton and Their Possible Connection With Snowball Earth

Subglacial meltwater supported aerobic marine habitats during Snowball Earth

Geological cycling of potassium and the K isotopic response: insights from loess and shales

Effects of early diagenesis on Mg isotopes in dolomite: The roles of Mn(IV)-reduction and recrystallization

K isotopes as a tracer for continental weathering and geological K cycling

Mg isotope response to dolomitization in hinterland-attached carbonate platforms: Outlook of δ<sup>26</sup>Mg as a tracer of basin restriction and seawater Mg/Ca ratio

Zinc Isotope Fractionation during Sorption onto Al Oxides: Atomic Level Understanding from EXAFS

Corrigendum to “A redox-stratified ocean 3.2 billion years ago” [Earth Planet. Sci. Lett. (2015) 430 (43–53)] (S0012821X15005270)(10.1016/j.epsl.2015.08.007)

Origin of heavy Fe isotope compositions in high-silica igneous rocks: A rhyolite perspective

Potassium isotope fractionation between K-salts and saturated aqueous solutions at room temperature: Laboratory experiments and theoretical calculations

Resetting of Mg isotopes between calcite and dolomite during burial metamorphism: Outlook of Mg isotopes as geothermometer and seawater proxy

Updating the Geologic Barcodes for South China: Discovery of Late Archean Banded Iron Formations in the Yangtze Craton

Vital effects of K isotope fractionation in organisms: observations and a hypothesis

Iron Isotope Fractionations Reveal a Finite Bioavailable Fe Pool for Structural Fe(III) Reduction in Nontronite

Precise measurement of stable potassium isotope ratios using a single focusing collision cell multi-collector ICP-MS

A redox-stratified ocean 3.2 billion years ago

Atom exchange between aqueous Fe(II) and structural Fe in clay minerals

Erratum :Correction to atom exchange between aqueous Fe(II) and structural Fe in clay minerals (Environmental Science and Technology (2015) 49 (2786-2795) (DOI:10.1021/es504984q))

Experimental calibration of Mg isotope fractionation between dolomite and aqueous solution and its geological implications

Iron isotope fractionation in sediments of an oligotrophic freshwater lake

Biologically recycled continental iron is a major component in banded iron formations

Magnesium isotope fractionation between brucite [Mg(OH)2] and Mg aqueous species: Implications for silicate weathering and biogeochemical processes

An anoxic, Fe(II)-rich, U-poor ocean 3.46 billion years ago

Biological Fe oxidation controlled deposition of banded iron formation in the ca. 3770 Ma Isua Supracrustal Belt (West Greenland)

Contrasting behavior of oxygen and iron isotopes in banded iron formations revealed by in situ isotopic analysis

Magnesium isotope fractionation during precipitation of inorganic calcite under laboratory conditions

U-Th-Pb isotope data indicate phanerozoic age for oxidation of the 3.4 Ga Apex Basalt

Exchange and fractionation of Mg isotopes between epsomite and saturated MgSO4 solution

Copper isotopic zonation in the Northparkes porphyry Cu-Au deposit, SE Australia

Existing forms of REE in gold-bearing pyrite of the Jinshan gold deposit, Jiangxi Province, China

The Cu isotopic signature of granites from the Lachlan Fold Belt, SE Australia

Formation mechanisms of hydrocarbon reservoirs associated with volcanic and subvolcanic intrusive rocks: Examples in Mesozoic-Cenozoic basins of eastern China

Zircon SHRIMP dating for the Weiya pluton, Eastern Tianshan: Its geological implications