Changes in Fe oxidation rate in hydrothermal plumes as a potential driver of enhanced hydrothermal input to near‐ridge sediments during glacial terminations

Details
Venue

Earth Sciences Seminar rooms
University of Oxford, South Parks Road, Oxford, OX1 3AN

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Date
Fri 15th Nov 2019
Cost
Free
Time
12noon - 1pm
Booking required
No

Coogan et al. (2019) Chem. Geol.

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