Whitman College
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From Proto-Earth to Modern Earth: Constraints from experimental petrology

The fundamental differentiation of the Earth was into a Fe-Ni-rich metallic core and a surrounding silicate mantle. The study of the mantle abundances of these siderophile elements, together with knowledge of their metal-silicate partition coefficients as a function of physico-chemical variables such as temperature, pressure and oxygen fugacity, may shed light on how core formation occurred, and on how the Earth accreted. The most likely scenarios will be discussed considering interactions between coexisting silicate, sulfide and metal phases.  
 

Wednesday, November 20, 2019 at 7:30 pm

Hall of Science, Brattain Auditorium
810 East Isaacs, Walla Walla, WA 99362

Event Type

Speaker

Audience

Faculty, Staff, Students, General Public

Departments

Academic, Sciences & Mathematics, Geology

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