Geochemistry of diabase dikes from the Lewis Hills Massif, Bay of Islands ophiolite - Evidence for partial melting of oceanic crust in transform faults

Details Geochemistry of diabase dikes from the Lewis Hills Massif, Bay of Islands ophiolite - Evidence for partial melting of oceanic crust in transform faults Geochemistry of diabase dikes from the Lewis Hills Massif, Bay of Islands ophiolite - Evidence for partial melting of oceanic crust in transform faults

May 1986

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1986e%26psl..78...89e&link_type=ejournal

Earth and Planetary Science Letters (ISSN 0012-821X), vol. 78, no. 1, May 1986, p. 89-103.

Mathematics

Logic

7

Earth Crust, Geochemistry, Igneous Rocks, Massifs, Ocean Bottom, Rock Intrusions, Basalt, Geological Faults, Maps, Melting, Trace Elements

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