Isotopic and trace element constraints on the genesis of the Faeroe lava pile

Author:

Gariépy Clément,Ludden John,Brooks Christopher

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference48 articles.

1. Reconstruction of Pangea: breakup and dispersion of continents;Dietz,1970

2. Dynamic partial melting: its application to the petrogenesis of basalts erupted in Iceland, the Faeroe Islands, the Isle of Skye (Scotland) and the Troodos Massif (Cyprus);Wood;Geochim. Cosmochim. Acta,1979

3. Faeroe-Iceland plume: rare-earth evidence;Schilling;Earth Planet. Sci. Lett.,1974

4. Trace element variations in Faeroe basalts and their possible relationship to ocean floor spreading history;Bollinberg;Bull. Geol. Soc. Denmark,1975

5. 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 Scotland;Mattey;Mineral. Mag.,1977

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