Deep circulation in the Late Cretaceous: Oxygen isotope paleotemperatures from Inoceramus remains in D.S.D.P. cores

Authors :: Saltzman, ES
Barron, EJ
Source :: Saltzman, ES; & Barron, EJ. (1982). Deep circulation in the Late Cretaceous: Oxygen isotope paleotemperatures from Inoceramus remains in D.S.D.P. cores. Palaeogeography, Palaeoclimatology, Palaeoecology, 40(1-3), 167-181. doi: 10.1016/0031-0182(82)90088-8. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/1tp5p3pm
Publication Year :: 1982
Publisher :: eScholarship, University of California, 1982.

Language :: English
Database :: OpenAIRE
Journal :: Saltzman, ES; & Barron, EJ. (1982). Deep circulation in the Late Cretaceous: Oxygen isotope paleotemperatures from Inoceramus remains in D.S.D.P. cores. Palaeogeography, Palaeoclimatology, Palaeoecology, 40(1-3), 167-181. doi: 10.1016/0031-0182(82)90088-8. UC Irvine: Retrieved from: http://www.escholarship.org/uc/item/1tp5p3pm
Accession number :: edsair.od.......325..12d65ebc064e44309cab0502af225393
Full Text :: https://doi.org/10.1016/0031-0182(82)90088-8.

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