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Jeff Vervoort, Ph.D.




Position:

Assistant Professor

Campus Address:

School of Earth & Environmental Sciences
Washington State University
P.O. Box 642812
Pullman, WA 99164-6376

Office:

Webster Physical Sciences 1048

Phone:

509-335-5597 (office)
509-335-6467 (lab)

E-mail:

vervoort@wsu.edu

Research interests:

Dr. Vervoort’s area of research is radiogenic isotope geochemistry and its application to solving geological and geochemical problems. Dr. Vervoort uses radiogenic isotopes in two different ways in his research: as natural isotopic tracers of sources and geological processes and as geochronometers to determine the ages of rocks and geological events.

 

Research statement:

My fundamental interest as a scientist is to understand the Earth from the perspective of geochemistry. Radiogenic isotopes are important tools that enable us to understand how the Earth formed and how it has evolved through its history.  Radiogenic isotopes also help constrain the geological processes that are operating on Earth today. To this end, I have worked on a wide range of earth and planetary materials including meteorites, igneous, metamorphic, and sedimentary rocks of all ages, modern sediments and volcanic rocks, and water samples.

Current research projects and areas of research include:

These research efforts center around the radiogenic isotope facility at WSU. My research group uses three facilities in SEES extensively in our research. These are: the radiogenic isotope clean laboratory to dissolve samples and perform chemical separations; the ThermoFinnigan Neptune MC-ICPMS for isotopic measurements; and the ThermoFinnigan Element2 HR-ICPMS in conjunction with the New Wave Nd-YAG 213nm laser ablation system for in situ U-Pb geochronology of zircons.  The radiogenic isotope facility at WSU is a full-service radiogenic isotope laboratory. We have the capability to perform chemical separations of several important isotope (Rb-Sr, Sm-Nd, Lu-Hf, and U-Pb) and elemental systems (e.g., HFSE, Ca, Cu, Fe, Mo). In conjunction with our calibrated Rb-Sr, Lu-Hf, and Sm-Nd isotopic spikes we can analyze the full range of earth and planetary materials from mud to meteorites and everything in between.

Courses:

Graduate Student:

Selected Publications:

 (*indicates graduate student or post-doctorate co-author)

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