Late Eocene-early Oligocene carbonate sedimentation in the deep sea.
Publication
, Journal Article
Thunell, RC; Corliss, BH
Published in: Terminal Eocene events
1986
Calcium carbonate accumulation rate patterns for the late Eocene-early Oligocene interval in 12 DSDP sites show inter- and intra-basin variations. In general, the observed changes in carbonate accumulation rates follow the patterns established for fluctuations in the position of the CCD across the Eocene/Oligocene boundary. Variability may best be explained by changes in surface water productivity and bottom water circulation patterns. -from Authors
Duke Scholars
Published In
Terminal Eocene events
Publication Date
1986
Start / End Page
363 / 380
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Thunell, R. C., & Corliss, B. H. (1986). Late Eocene-early Oligocene carbonate sedimentation in the deep sea. Terminal Eocene Events, 363–380.
Thunell, R. C., and B. H. Corliss. “Late Eocene-early Oligocene carbonate sedimentation in the deep sea.” Terminal Eocene Events, 1986, 363–80.
Thunell RC, Corliss BH. Late Eocene-early Oligocene carbonate sedimentation in the deep sea. Terminal Eocene events. 1986;363–80.
Thunell, R. C., and B. H. Corliss. “Late Eocene-early Oligocene carbonate sedimentation in the deep sea.” Terminal Eocene Events, 1986, pp. 363–80.
Thunell RC, Corliss BH. Late Eocene-early Oligocene carbonate sedimentation in the deep sea. Terminal Eocene events. 1986;363–380.
Published In
Terminal Eocene events
Publication Date
1986
Start / End Page
363 / 380