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R. Damian Nance
Ohio University
114Publications
34H-index
4,334Citations
Publications 115
Newest
#1Yvette D. Kuiper (Colorado School of Mines)H-Index: 8
#2R. Damian Nance (OU: Ohio University)H-Index: 34
Last.Rob A. Strachan (University of Portsmouth)H-Index: 36
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#2Nick M.W. RobertsH-Index: 24
Last.R. Damian NanceH-Index: 34
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Source
#1J. Brendan Murphy (St. Francis Xavier University)H-Index: 44
#2R. Damian Nance (OU: Ohio University)H-Index: 34
Last.Douglas A. ArchibaldH-Index: 1
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In northwest Donegal, Ireland, a large number of coeval appinitic (hornblende-plagioclase-rich) plutons and lamprophyre dykes occur around the Ardara pluton, a granitic satellite body and one of the oldest phases of the ca. 428–400 Ma composite Donegal Batholith. The appinite units form a bimodal (mafic–felsic) suite in which hornblende is the dominant mafic mineral and typically occurs as large prismatic phenocrysts within a finer grained matrix. Lamprophyre dykes are mafic in composition with ...
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#1J. Brendan MurphyH-Index: 44
#2J. M. CasasH-Index: 14
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Trabajo presentado en GSA Annual Meeting (The Geological Society of America), celebrado en Indianapolis, Indiana (Estados Unidos), del 4 al 7 de noviembre de 2018
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#1R. Damian NanceH-Index: 34
#2J. Brendan MurphyH-Index: 44
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#1Logan B. GablerH-Index: 1
#2R. Damian NanceH-Index: 34
Last.J. Brendan MurphyH-Index: 44
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Source
#1J. Brendan Murphy (St. Francis Xavier University)H-Index: 44
#2R. Damian Nance (OU: Ohio University)H-Index: 34
Last.Stephen T. JohnstonH-Index: 26
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