Major oxides for tektites and for conglomerate clast of the Upper Eocene ejecta-bearing layer of ODP Hole 150-904A (Table 1)

Evidence for the Chesapeake Bay Crater as the source for New Jersey continental margin ejecta is provided by fine-grained tektites and coarse-grained unmelted ejecta. The Upper Eocene ejecta deposit, now demonstrated to be part of the North American strewn field, occurs on the New Jersey continental...

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Bibliographic Details
Main Authors: McHugh, Cecilia M G, Snyder, Scott W, Miller, Kenneth G
Format: Dataset
Language:English
Published: PANGAEA 1998
Subjects:
FeO
ODP
Online Access:https://doi.pangaea.de/10.1594/PANGAEA.711490
https://doi.org/10.1594/PANGAEA.711490