R
Roman A. Schmitt
Researcher at Oregon State University
Publications - 99
Citations - 3136
Roman A. Schmitt is an academic researcher from Oregon State University. The author has contributed to research in topics: Basalt & Chondrite. The author has an hindex of 35, co-authored 99 publications receiving 3057 citations.
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Cerium:A chemical tracer for paleo-oceanic redox conditions
TL;DR: Ce anomalies found in marine carbonates provide a sensitive indicator for the study of paleo-oceanic redox conditions as discussed by the authors, which can be used for deciphering some aspects of the paleo ocean chemistry, and is: log C Ce $ log α CePO 0 4 = 132 − 025 log P O 2 − 30 pH = −195 − 0 25 log P CO 2 + 150 log [Ca ++ ] The pH, which is related to PCO2, and PO2 are major factors for controlling the Ce concentration in seawater.
Book ChapterDOI
Abstracts of Contributed Papers
Richard C. Henry,J. E. Hesser,W. McClintock,J. Audouze,David N. Schramm,T. P. Kohman,J. M. Huey,G. A. Cowan,B. D. Donn,E. W. Chappelle,W. A. Payne,L. J. Stief,James G. Lawless,Etta Peterson,Keith A. Kvenvolden,G. Crozaz,D. Burnett,R. Walker,Stanton J. Peale,L. Husain,O. A. Schaeffer,L. D. Nguyen,G. Puil,M. de Saint Simon,Y. Yokoyama,P. M. Millman,Donald E. Brownlee,P. W. Hodge,T. Grjebine,Marvin W. Rowe,J. M. Herndon,D. E. Watson,E. E. Larson,William V. Boynton,Roman A. Schmitt,N. Carleton,W. Traub +36 more
TL;DR: The strength of the K line of singly ionized calcium has been measured for several hundred A-type stars within a few hundred parsecs of the Sun and for the A stars in several galactic star clusters as mentioned in this paper.
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Elemental abundances in stone meteorites
TL;DR: In this paper, instrumental neutron activation analyses of 103 chondrites and 17 achondrites were used to measure abundances of Na, Al, Sc, Cr, Mn, Fe, Co, and Cu.
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Chemical evidence for the genesis of the ureilites, the achondrite Chassigny and the nakhlites
TL;DR: In this paper, an investigation has been conducted of the ureilites and the achondrite Chassigny to elucidate differences in their petrogenesis, and the experimental studies reported include the determination of elemental abundances by instrumental neutron activation analysis.
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Elemental abundances in chondrules from unequilibrated chondrites: Evidence for chondrule origin by melting of pre-existing materials
TL;DR: The geometric mean composition of the whole-rock chondrule suites are almost indistinguishable from each other for many elements; chondrules are enriched in lithophile and depleted in siderophile elements in a pattern consistent with chond rule formation by melting of preexistent materials as discussed by the authors.