Rates of magma ascent : constraints from mantle-derived xenoliths | Macquarie University ResearchOnline

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Title: Rates of magma ascent : constraints from mantle-derived xenoliths
Related: Dosseto, Anthony; Turner, Simon P. and Van Orman, James A.. Timescales of magmatic processes : from core to atmosphere, p.116-124
Publisher: Chichester, West Sussex, UK ; Hoboken, NJ : Wiley-Blackwell
Date: 2010
FoR/RFCD Code(s): 040200 Geochemistry
Author/Creator: O'Reilly, Suzanne Y
Author/Creator: Griffin, W. L
Description: Magmas carrying mantle xenoliths much reach the surface within a maximum of about 8 to 60 hours of picking up these dense fragments from depths of about 200 to 80km depth.
Description: 9 page(s)
Subject Keyword: 040200 Geochemistry
Resource Type: book chapter
Organisation: Macquarie University. National Key Centre for Geochemical Evolution and Metallogeny of Continents (GEMOC)

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