Origin of authigenic Mn-Fe carbonates and pore-water evolution in marine sediments: Evidence from Cenozoic strata of the Arctic Ocean and Norwegian-Geenland Sea (ODP Leg 151)
2000 (English)In: JOURNAL OF SEDIMENTARY RESEARCH, ISSN 1073-130X, Vol. 70, no 3, p. 682-699Article in journal (Refereed) Published
Abstract [en]
Early diagenetic Mn-Fe carbonates, occurring in thin layers, nodules, and burrows, were recovered from Cenozoic silts and clays from the Arctic Ocean and the Norwegian-Greenland Sea during Ocean Drilling Program Leg 151, At Sites 909 (Fram Strait; Miocene
Place, publisher, year, edition, pages
2000. Vol. 70, no 3, p. 682-699
Keywords [en]
RARE-EARTH ELEMENT; OXYGEN-ISOTOPE FRACTIONATION; INTERSTITIAL WATERS; ORGANIC-MATTER; MARGIN; BURIAL; ENVIRONMENTS; DIAGENESIS; DOLOMITES; OXIDATION
Identifiers
URN: urn:nbn:se:uu:diva-37694OAI: oai:DiVA.org:uu-37694DiVA, id: diva2:65593
Note
Addresses: Chow N, Univ Manitoba, Dept Geol Sci, Winnipeg, MB R3T 2N2, Canada. Univ Manitoba, Dept Geol Sci, Winnipeg, MB R3T 2N2, Canada. Uppsala Univ, Inst Earth Sci, S-75236 Uppsala, Sweden. Univ Windsor, Dept Earth Sci, Windsor, ON N9B 3P4, Canada.
2006-12-022006-12-022011-01-14