Portal de Periódicos da CAPES

EARLY TERTIARY BENTONITE FROM THE SUBSURFACE OF CENTRAL DELAWARE

1962; Geological Society of America; Volume: 73; Issue: 3 Linguagem: Inglês

10.1130/0016-7606(1962)73[395

1943-2674

Robert Jordan, John K. Adams,

Invertebrate Taxonomy and Ecology

Research Article| March 01, 1962 EARLY TERTIARY BENTONITE FROM THE SUBSURFACE OF CENTRAL DELAWARE ROBERT R JORDAN; ROBERT R JORDAN UNIVERSITY OF DELAWARE, NEWARK, DELAWARE Search for other works by this author on: GSW Google Scholar JOHN K ADAMS JOHN K ADAMS UNIVERSITY OF DELAWARE, NEWARK, DELAWARE Search for other works by this author on: GSW Google Scholar Author and Article Information ROBERT R JORDAN UNIVERSITY OF DELAWARE, NEWARK, DELAWARE JOHN K ADAMS UNIVERSITY OF DELAWARE, NEWARK, DELAWARE Publisher: Geological Society of America Received: 10 May 1961 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1962, The Geological Society of America, Inc. Copyright is not claimed on any material prepared by U.S. government employees within the scope of their employment. GSA Bulletin (1962) 73 (3): 395–398. https://doi.org/10.1130/0016-7606(1962)73[395:ETBFTS]2.0.CO;2 Article history Received: 10 May 1961 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation ROBERT R JORDAN, JOHN K ADAMS; EARLY TERTIARY BENTONITE FROM THE SUBSURFACE OF CENTRAL DELAWARE. GSA Bulletin 1962;; 73 (3): 395–398. doi: https://doi.org/10.1130/0016-7606(1962)73[395:ETBFTS]2.0.CO;2 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu toolbar search search input Search input auto suggest filter your search All ContentBy SocietyGSA Bulletin Search Advanced Search Abstract A thin stratum of bentonite containing altered shards was found in a core taken near Dover, Delaware. The bentonite and adjacent sediments are described. The proximity of the bentonite to the Cretaceous-Tertiary boundary as indicated by planktonic Foraminifera suggests that it may be a useful stratigraphic marker. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not have access to this content, please speak to your institutional administrator if you feel you should have access.