Stratigraphical boundary between the Pliocene and Pleistocene strata in the Boso peninsula, south Kanto, Japan

Ogose, S.

Journal of the Faculty of Science University of Tokyo, Section 2, Geology 9(2): 287-299

1954


ISSN/ISBN: 0040-8999
Accession: 020106385

Download citation:  
Text
  |  
BibTeX
  |  
RIS

Article/Abstract emailed within 1 workday
Payments are secure & encrypted
Powered by Stripe
Powered by PayPal

Abstract
"The Nagahama sand and gravel, i.e., the basal or marginal part of the Narita group is probably Pleistocene in age, while the Higasihigasa mud, sand and gravel which is a part of the basal or marginal beds of the Akimoto subgroup, may safely be considered to be Pliocene.. The writer can not determine exactly the age of the middle and upper divisions of the Akimoto subgroup in any way.".