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New Constraints on Temperature, Oxygen Fugacity and H 2O of Subduction Zone Basalts Based on Olivine-Melt Equilibrium

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개인저자Pu, Xiaofei.
단체저자명University of Michigan. Earth and Environmental Sciences.
서명/저자사항New Constraints on Temperature, Oxygen Fugacity and H 2O of Subduction Zone Basalts Based on Olivine-Melt Equilibrium.
발행사항[S.l.] : University of Michigan., 2018
발행사항Ann Arbor : ProQuest Dissertations & Theses, 2018
형태사항516 p.
소장본 주기School code: 0127.
ISBN9780438125100
일반주기 Source: Dissertation Abstracts International, Volume: 79-12(E), Section: B.
Adviser: Rebecca Ann Lange.
요약Erupted basalts are windows into the deep Earth. This dissertation provides evidence that mantle-derived basalts grow their phenocrysts during rapid ascent to the surface, and that the most Mg-rich olivine in erupted samples approximates the fir
요약Chapter II develops a new olivine-melt thermometer based on the partitioning of Ni (DNiol/liq), and provides evidence that it is far less sensitive to the effects of pressure and dissolved H2O in the melt than DMgol/liq, which is the basis of mo
요약Chapter III investigates the sensitivity of DNiol/liq to dissolved H2O in basaltic melts through a series of olivine-melt equilibrium experiments. Four 1-bar experiments, one anhydrous experiment at 0.5 GPa, and five hydrous experiments at 0.5
요약Chapter IV applies the new Ni-based olivine-melt thermometer developed and tested in Chapter II and III to a set of mantle-derived, high-K melts that erupted within the Colima rift in western Mexico, where a mid-ocean spreading ridge is interact
요약Chapter V investigates the cause of the relatively high oxygen fugacity (fO2) of the pristine K-rich Colima lavas (Chapter IV). The pre-eruptive oxidation state (Fe3+/Fe2+ ratio), derived from olivine-melt Fe2+-Mg exchange equilibrium, indicate
일반주제명Environmental science.
언어영어
기본자료 저록Dissertation Abstracts International79-12B(E).
Dissertation Abstract International
대출바로가기http://www.riss.kr/pdu/ddodLink.do?id=T15000423

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