The use of “immobile” trace elements to distinguish the palaeotectonic affinities of metabasalts: Applications to the Paleocene basalts of Mull and Skye, Northwest Scotland
- 28 October 2002
- journal article
- Published by Elsevier
- Vol. 39 (3) , 407-416
- https://doi.org/10.1016/0012-821x(78)90029-8
Abstract
No abstract availableKeywords
This publication has 26 references indexed in Scilit:
- Ophiolite origin investigated by discriminant analysis using Ti, Zr and YPublished by Elsevier ,2002
- Magma type and tectonic setting discrimination using immobile elementsPublished by Elsevier ,2002
- The diagnostic geochemistry, relative abundance, and spatial distribution of high-calcium, low-alkali olivine tholeiite dykes in the Lower Tertiary regional swarm of the Isle of Skye, NW ScotlandMineralogical Magazine, 1977
- Elemental mobility during zeolite facies metamorphism of the Tertiary basalts of eastern IcelandContributions to Mineralogy and Petrology, 1976
- The TiO2–K2O–P2O5 diagram: A method of discriminating between oceanic and non-oceanic basaltsEarth and Planetary Science Letters, 1975
- Tectonic setting of basic volcanic rocks determined using trace element analysesEarth and Planetary Science Letters, 1973
- Major Element Chemical Variation in the Eocene Lavas of the Isle of Skye, ScotlandJournal of Petrology, 1972
- Low-O18 Igneous Rocks from the Intrusive Complexes of Skye, Mull, and Ardnamurchan, Western ScotlandJournal of Petrology, 1971
- Rb, Sr, Y, Zr and Nb in some ocean floor basaltic rocksEarth and Planetary Science Letters, 1970
- Origin of Basalt Magmas: An Experimental Study of Natural and Synthetic Rock SystemsJournal of Petrology, 1962