Research Article| March 01, 1969 Geological Time-Distance Rates: The Bubnoff Unit ALFRED G FISCHER ALFRED G FISCHER Department of Geological and Geophysical Sciences, Princeton University, Princeton, New Jersey Search for other works by this author on: GSW Google Scholar Author and Article Information ALFRED G FISCHER Department of Geological and Geophysical Sciences, Princeton University, Princeton, New Jersey Publisher: Geological Society of America Received: 02 Aug 1968 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1969, 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 (1969) 80 (3): 549–552. https://doi.org/10.1130/0016-7606(1969)80[549:GTRTBU]2.0.CO;2 Article history Received: 02 Aug 1968 First Online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn Email Permissions Search Site Citation ALFRED G FISCHER; Geological Time-Distance Rates: The Bubnoff Unit. GSA Bulletin 1969;; 80 (3): 549–552. doi: https://doi.org/10.1130/0016-7606(1969)80[549:GTRTBU]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 The Bubnoff unit (B), defined as 1micron/year = 1 mm/thousand years = 1m/million years, is proposed as a standard measure for geologic movements and increments. 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.
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Alfred G. Fischer (1969) studied this question.