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U series disequilibria: Insights into mantle melting and the timescales of magma differentiation
Author(s) -
Peate David W.,
Hawkesworth Chris J.
Publication year - 2005
Publication title -
reviews of geophysics
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 8.087
H-Index - 156
eISSN - 1944-9208
pISSN - 8755-1209
DOI - 10.1029/2004rg000154
Subject(s) - geology , mantle (geology) , igneous rock , subduction , upwelling , nuclide , geophysics , geochemistry , volcanism , tectonics , petrology , earth science , seismology , oceanography , physics , quantum mechanics
Several U series nuclides have half‐lives ( 230 Th, 76 kyr; 231 Pa, 33 kyr; and 226 Ra, 1.6 kyr) comparable to timescales of magmatic processes. We review the basic principles of extracting time information from U series nuclides and summarize variations in ( 230 Th/ 238 U), ( 226 Ra/ 230 Th), and ( 231 Pa/ 235 U) observed in magmas from mid‐ocean ridges, within‐plate settings, and subduction zones to contrast melt generation processes in different tectonic settings. U series disequilibria on melt and crystal phases of igneous rocks can provide temporal information on different stages in the magmatic history (melting duration, melt transport rates, magmatic crustal residence times, and timing of crystal growth) and potentially provide clues about the nature and mineralogy of mantle sources, mantle upwelling rates and porosity, fluid influences, and mechanisms of melt generation and transport. The subject is beginning to take a genuinely integrated approach to developing physically realistic quantitative models that offer increasingly exciting opportunities in the study of magmatic processes.