1974
DOI: 10.1146/annurev.ea.02.050174.000325
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Iceland in Relation to the Mid-Atlantic Ridge

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Cited by 165 publications
(44 citation statements)
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“…(Walker in: Kristjansson 1974, Sch~ifer 1975. Dips appear to be steepest at depth Saemundsson, 1978, Pfilmason andSaemundsson, 1974). a) Volcanic activity, age and structure.…”
Section: Fig2mentioning
confidence: 98%
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“…(Walker in: Kristjansson 1974, Sch~ifer 1975. Dips appear to be steepest at depth Saemundsson, 1978, Pfilmason andSaemundsson, 1974). a) Volcanic activity, age and structure.…”
Section: Fig2mentioning
confidence: 98%
“…At 65°N where the western zone ends present activity, the E zone bends and an "anomalous" zone extends westward to Snaefellsnes. One interpretation is that the N part of the E rift developed about 4 Ma ago in older crust generated at the W zone, now extinct (Saemundsson 1974); the S part of the E rift appears to be even younger. Another view (Aronson and Saemundsson 1975, Sigurdsson et al 1978, Schilling et al 1978) is that at least the NE rift is much older.…”
Section: Fig2mentioning
confidence: 99%
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“…Les trois principaux modèles hydrodynamiques fournissant des explications sur l'origine des fluides hydrothermaux ainsi que sur le mécanisme énergétique responsable de la circulation de ces fluides sont les suivants: i) un modèle avec des cellules de convection (Palmason, 1967;Lister, 1972;Wolery et Sleep, 1976;Crane and Normark, 1977;Francheteau et al, 1979) ii) un modèle magmatique (Sangster, 1972;Solomon, 1976;Urabe et Sato, 1978; Litage des sulfures massifs concordants Sawkins et Kowalik, 1981;Bryndzia et al, 1983;Perfit et Fornari, 1983) et iii) un modèle avec aquifère (Hodgson et Lydon, 1977et Gibson et al, 1983.…”
Section: Mise En Garde/adviceunclassified