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Schafer, Charles T. (1974) The Mid-Atlantic Ridge Near 45 °N. XXII. Sedimentary Deposition and Lithogenesis on Mid-Atlantic Ridge Mountain Tops. Canadian Journal of Earth Sciences, 11 (8) 1157-1167 doi:10.1139/e74-109

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Reference TypeJournal (article/letter/editorial)
TitleThe Mid-Atlantic Ridge Near 45 °N. XXII. Sedimentary Deposition and Lithogenesis on Mid-Atlantic Ridge Mountain Tops
JournalCanadian Journal of Earth Sciences
AuthorsSchafer, Charles T.Author
Year1974 (August 1)Volume11
Issue8
PublisherCanadian Science Publishing
DOIdoi:10.1139/e74-109Search in ResearchGate
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Mindat Ref. ID474184Long-form Identifiermindat:1:5:474184:2
GUID0
Full ReferenceSchafer, Charles T. (1974) The Mid-Atlantic Ridge Near 45 °N. XXII. Sedimentary Deposition and Lithogenesis on Mid-Atlantic Ridge Mountain Tops. Canadian Journal of Earth Sciences, 11 (8) 1157-1167 doi:10.1139/e74-109
Plain TextSchafer, Charles T. (1974) The Mid-Atlantic Ridge Near 45 °N. XXII. Sedimentary Deposition and Lithogenesis on Mid-Atlantic Ridge Mountain Tops. Canadian Journal of Earth Sciences, 11 (8) 1157-1167 doi:10.1139/e74-109
In(1974, August) Canadian Journal of Earth Sciences Vol. 11 (8) Canadian Science Publishing
Abstract/Notes Bottom photographs and drilled rock cores collected on several mountain tops along the crest of the Mid-Atlantic Ridge near 45°N describe the sediment distribution, sediment dynamics and shallow stratigraphy of these sites. Lag pebble deposits and pebble waves indicate rapid changes in bottom current direction and velocities that may approach 100 cm/s (>2 knots) one meter above the bottom so that surface sediments are often not indicative of sediment and rock types sampled using shallow drilling techniques. Absolute dates (14C) of coralline limestone, which underlies coarse unconsolidated sediment at most drilling sites, suggest deposition and initial lithification of these deposits during a middle Wisconsin interstadial period.


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