Textural Equilibrium in Magmatic Layers of the Lough Fee Ultramafic Intrusion, NW Connemara, Ireland: Implications for Adcumulus Mineral Growth
Author:
Publisher
Project Muse
Subject
General Earth and Planetary Sciences
Reference25 articles.
1. Younging directions in the Dawros Peridotite, Connemara;M Bennett;Journal of the Geological Society, London,1983
2. Contrasted metamorphic and structural evolution across a ductile/brittle displacement zone in NW Connemara;A Boyle;Geologische Rundschau,1991
3. On the identification of textural equilibrium in rocks using dihedral angle measurements;M Elliot;Geology,1997
4. Short-lived continental magmatic arc at Connemara, western Irish Caledonides: Implications for the age of the Grampian orogeny;A Friedrich;Geology,1999
Cited by 3 articles. 订阅此论文施引文献 订阅此论文施引文献,注册后可以免费订阅5篇论文的施引文献,订阅后可以查看论文全部施引文献
1. Timescales of magmatism and metamorphism in the Connemara Caledonides: insights from the thermal aureole of the Dawros–Currywongaun–Doughruagh Complex, western Ireland;Geological Magazine;2021-07-29
2. Grain Size Variations Record Segregation of Residual Melts in Slow‐Spreading Oceanic Crust (Atlantis Bank, 57°E Southwest Indian Ridge);Journal of Geophysical Research: Solid Earth;2021-04
3. Parental magma composition of the syntectonic Dawros Peridotite chromitites, NW Connemara, Ireland;Geological Magazine;2011-10-14
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