The nature and significance of magma chamber margins in ophiolites: examples from the Norwegian Caledonides
- 29 October 2002
- journal article
- Published by Elsevier
- Vol. 77 (1) , 100-112
- https://doi.org/10.1016/0012-821x(86)90136-6
Abstract
No abstract availableKeywords
This publication has 14 references indexed in Scilit:
- The origin of oceanic plagiogranites from the karmoy ophiolite, western NorwayContributions to Mineralogy and Petrology, 1984
- The structure of sheeted dikes and associated rocks in North Arm massif, Bay of Islands ophiolite complex, and the intrusive process at oceanic spreading centersCanadian Journal of Earth Sciences, 1983
- The base of a sheeted dyke complex, Oman ophiolite: implications for magma chambers at oceanic spreading axesJournal of the Geological Society, 1983
- Samail Ophiolite plutonic suite: Field relations, phase variation, cryptic variation and layering, and a model of a spreading ridge magma chamberJournal of Geophysical Research, 1981
- The Karmøy ophiolite, southwest NorwayGeology, 1979
- The Sheeted Dike Layer of the Betts Cove Ophiolite Complex does not Represent Spreading: Further DiscussionCanadian Journal of Earth Sciences, 1975
- The Sheeted Dike Layer of the Betts Cove Ophiolite Complex does not Represent Spreading: DiscussionCanadian Journal of Earth Sciences, 1974
- A Model for Oceanic Crystal Structure DevelopedGeophysical Journal International, 1974
- The Sheeted Dike Layer of the Betts Cove Ophiolite Complex does not Represent SpreadingCanadian Journal of Earth Sciences, 1974
- The Troodos Massif, Cyprus and other ophiolites as oceanic crust: evaluation and implicationsPhilosophical Transactions of the Royal Society of London. Series A, Mathematical and Physical Sciences, 1971