Neodymium Evidence for Increased Circumpolar Deep Water Flow to the North Pacific During the Middle Miocene Climate Transition (2018)
Attributed to:
IODP Expedition 351, Philippine Sea: Neogene NW Pacific Deep Water Circulation
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1029/2017pa003309
Publication URI: http://dx.doi.org/10.1029/2017pa003309
Type: Journal Article/Review
Parent Publication: Paleoceanography and Paleoclimatology
Issue: 7
ISSN: 2572-4517