Laura Bilenker

Assistant Professor

Auburn University

United States

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Laura Bilenker is an Assistant Professor at Auburn University, USA. Her research focuses on geochemistry, particularly in the areas of iron isotope measurements, iron oxide deposits, and the petrogenesis of altered peridotites. Recent articles authored by her explore various geochemical processes and mechanisms related to mineral deposits, providing insights into metal and ore fluid sources.

Articles (9)

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2023

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2022

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2022

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2022

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2021

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2020

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2020

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2020

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2020

Collaborators (4)

Dominique Weis

The University of British Columbia

CANADA

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Norikatsu Akizawa

Assistant Professor

University of Tokyo

JAPAN

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Esther Schwarzenbach

Professor in Mineralogy

University of Fribourg

SWITZERLAND

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Maria Alejandra Rodriguez Mustafa

University of Michigan

UNITED STATES

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Laura Bilenker

Research Interests

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Articles (9)

A Systematic Investigation of the Effects of Standard-Sample Concentration Mismatch during Fe Isotope Measurement by MC-ICP-MS

Geochemistry of serpentinized and multiphase altered Atlantis Massif peridotites (IODP Expedition 357): Petrogenesis and discrimination of melt-rock vs. fluid-rock processes

Formation of iron oxide–apatite deposits

The Mina Justa Iron Oxide Copper-Gold (IOCG) Deposit, Peru: Constraints on Metal and Ore Fluid Sources

Mineral chemistry and sulfur isotope geochemistry from tonalite-hosted, gold-bearing quartz veins at Hog Mountain, Southwestern Appalachians: Implications for gold precipitation mechanism, sulfur source, and genesis

A Continuum from Iron Oxide Copper-Gold to Iron Oxide-Apatite Deposits: Evidence from Fe and O Stable Isotopes and Trace Element Chemistry of Magnetite

A continuum from iron oxide copper-gold to iron oxide-apatite deposits: Evidence from fe and O stable isotopes and trace element chemistry of magnetite

Triple oxygen (δ<sup>18</sup>O, Δ<sup>17</sup>O), hydrogen (δ<sup>2</sup>H), and iron (δ<sup>56</sup>Fe) stable isotope signatures indicate a silicate magma source and magmatic-hydrothermal genesis for magnetite orebodies at El Laco, Chile

Triple Oxygen (δ18O, Δ17O), Hydrogen (δ2H), and Iron (δ56Fe) Stable Isotope Signatures Indicate a Silicate Magma Source and Magmatic-Hydrothermal Genesis for Magnetite Orebodies at El Laco, Chile

Collaborators (4)

Dominique Weis

Norikatsu Akizawa

Esther Schwarzenbach

Maria Alejandra Rodriguez Mustafa

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