Jesse Reimink

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Assistant Professor

Pennsylvania State University

United States

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About

Jesse Reimink is an Assistant Professor at Pennsylvania State University in the United States. His research focuses on the tectonothermal history of ancient crustal formations, magmatic evolution, and geological processes as revealed through zircon and apatite petrochronology. Recent publications include studies on the early Earth's crust, continental growth, and the environmental significance of geochronological findings.

Recent Grants

Grant: Close

Development of a Simplified Cavity Thermal Ionization Source for Geoscience Applications

Open Date: 2018-05-01

Close Date: 2020-04-30

Grant: Close

Exploration of the Earliest Crust Forming Events on Earth

Open Date: 2015-09-15

Close Date: 2018-08-31

Jesse Reimink

Research Interests

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About

Recent Grants

Articles (18)

Eoarchean–Paleoproterozoic Tectonothermal History of the Acasta Gneiss Complex Constrained by Titanite and Apatite Petrochronology

Tephra zircon U-Pb geochronology of kimberlite maar sedimentary fills in subarctic Canada: Implications for Eocene paleoclimate and Late Cretaceous paleogeography

Thinning and Heating of Laramide Continental Lower Crust Recorded by Zircon Petrochronology

Subaerial weathering drove stabilization of continents

Extracting Meaningful Environmental and Age Information From a c. 2.4–2.2 Ga Peritidal Phosphorite: The Turee Creek Group, Western Australia

Snapshots of magmatic evolution revealed by zircon depth profiling

Earth’s Earliest Crust

U‐Th‐Pb and Trace Element Evaluation of Existing Titanite and Apatite LA‐ICP‐MS Reference Materials and Determination of 208Pb/232Th‐206Pb/238U Date Discordance in Archaean Accessory Phases

Quantifying the effect of late bombardment on terrestrial zircons

The crystal timekeeper zircon

A whole-lithosphere view of continental growth

Evaluating the Age Distribution of Exposed Crust in the Acasta Gneiss Complex Using Detrital Zircons in Pleistocene Eskers

Global zircon analysis records a gradual rise of continental crust throughout the Neoarchean

A comparison between zircons from the Acasta Gneiss Complex and the Jack Hills region

Tungsten Isotope Composition of Archean Crustal Reservoirs and Implications for Terrestrial μ182W Evolution

Titanium isotopes constrain a magmatic transition at the Hadean-Archean boundary in the Acasta Gneiss Complex

Hafnium isotopes in zircons document the gradual onset of mobile-lid tectonics

A cavity ion source for high-ionization efficiency neodymium isotope-ratio analyses in the geosciences

Collaborators (5)

Alberto Reyes

Andrea Mundl-Petermeier

Britta Jensen

Scott DuFrane

Joshua Davies

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