Abstract
Research Article| November 01, 1962 THREE-DIMENSIONAL SPECIFIC-GRAVITY VARIATION IN THE GLEN ALPINE STOCK, SIERRA NEVADA, CALIFORNIA E. W PEIKERT E. W PEIKERT DEPT. GEOLOGY, NORTHWESTERN UNIVERSITY, EVANSTON, ILL Search for other works by this author on: GSW Google Scholar Author and Article Information E. W PEIKERT DEPT. GEOLOGY, NORTHWESTERN UNIVERSITY, EVANSTON, ILL Publisher: Geological Society of America Received: 09 May 1962 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 (11): 1437–1442. https://doi.org/10.1130/0016-7606(1962)73[1437:TSVITG]2.0.CO;2 Article history Received: 09 May 1962 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 E. W PEIKERT; THREE-DIMENSIONAL SPECIFIC-GRAVITY VARIATION IN THE GLEN ALPINE STOCK, SIERRA NEVADA, CALIFORNIA. GSA Bulletin 1962;; 73 (11): 1437–1442. doi: https://doi.org/10.1130/0016-7606(1962)73[1437:TSVITG]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 Recent statistical developments permit evaluation of two-dimensional compositional variability in granitic plutons. These methods are extended to include the effect of vertical variation and are applied to analysis of specific gravity data from a small pluton in the Sierra Nevada, California. A strong positive correlation of this variable with elevation is established and suggests the importance of vertical compositional variation in granitic plutons. 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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