Open AccessThe rift-to-drift transition in the southern North Atlantic: A stuttering start of the MORB machine?: COMMENT and REPLY: COMMENT
Author(s) -
James S. Beard
Publication year - 2008
Publication title -
geology
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 2.609
H-Index - 215
eISSN - 1943-2682
pISSN - 0091-7613
DOI - 10.1130/g24775c.1
Subject(s) - stuttering , rift , geology , oceanography , seismology , linguistics , tectonics , philosophy
[Jagoutz et al. (2007)][1] argue for a long history of alkaline to mid-oceanic ridge basalt (MORB)–type magmatism occurring during the transition from amagmatic to magmatic rifting at the Iberia-Newfoundland conjugate margin. U-Pb zircon ages suggest that magmatism spanned the range of 110–127
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