Update on feldspar and oxide thermometry in the Adirondack Mountains, New York

Abstract

Research Article| February 01, 1980 Update on feldspar and oxide thermometry in the Adirondack Mountains, New York STEVEN R. BOHLEN; STEVEN R. BOHLEN 1Department of Geology and Mineralogy, University of Michigan, Ann Arbor, Michigan 48109. Present address: Institute of Geophysics and Planetary Physics, University of California, Los Angeles, Los Angeles, California 90024 Search for other works by this author on: GSW Google Scholar ERIC J. ESSENE; ERIC J. ESSENE 1Department of Geology and Mineralogy, University of Michigan, Ann Arbor, Michigan 48109. Present address: Institute of Geophysics and Planetary Physics, University of California, Los Angeles, Los Angeles, California 90024 Search for other works by this author on: GSW Google Scholar KAREN S. HOFFMAN KAREN S. HOFFMAN 1Department of Geology and Mineralogy, University of Michigan, Ann Arbor, Michigan 48109. Present address: Institute of Geophysics and Planetary Physics, University of California, Los Angeles, Los Angeles, California 90024 Search for other works by this author on: GSW Google Scholar GSA Bulletin (1980) 91 (2): 110–113. https://doi.org/10.1130/0016-7606(1980)91<110:UOFAOT>2.0.CO;2 Article history first online: 01 Jun 2017 Cite View This Citation Add to Citation Manager Share Icon Share Facebook Twitter LinkedIn MailTo Tools Icon Tools Get Permissions Search Site Citation STEVEN R. BOHLEN, ERIC J. ESSENE, KAREN S. HOFFMAN; Update on feldspar and oxide thermometry in the Adirondack Mountains, New York. GSA Bulletin 1980;; 91 (2): 110–113. doi: https://doi.org/10.1130/0016-7606(1980)91<110:UOFAOT>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 Recently obtained feldspar and oxide temperature data for orthogneiss and paragneiss in the Adirondack Mountains, New York, further constrain and generally support the regional thermometry previously established. Peak metamorphic temperatures were 700 to 750 °C throughout most of the Adirondack Highlands and 750 to 800 °C in the High Peaks region during the Granville metamorphic event. 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.