Research Article| January 01, 1971 Kyanite-, Staurolite-, and Garnet-Bearing Schists in the Setters Formation, Maryland Piedmont GEORGE W FISHER GEORGE W FISHER Department of Earth and Planetary Sciences, The Johns Hopkins University, Baltimore, Maryland 21218 Search for other works by this author on: GSW Google Scholar Author and Article Information GEORGE W FISHER Department of Earth and Planetary Sciences, The Johns Hopkins University, Baltimore, Maryland 21218 Publisher: Geological Society of America Received: 13 Aug 1970 First Online: 02 Mar 2017 Online ISSN: 1943-2674 Print ISSN: 0016-7606 Copyright © 1971, 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 (1971) 82 (1): 229–232. https://doi.org/10.1130/0016-7606(1971)82[229:KSAGSI]2.0.CO;2 Article history Received: 13 Aug 1970 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 GEORGE W FISHER; Kyanite-, Staurolite-, and Garnet-Bearing Schists in the Setters Formation, Maryland Piedmont. GSA Bulletin 1971;; 82 (1): 229–232. doi: https://doi.org/10.1130/0016-7606(1971)82[229:KSAGSI]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 Reconnaissance studies of the Setters Formation, the basal unit of the Glenarm Series, confirm early reports that kyanite, Staurolite, and abundant garnets occur in the schists at the top of the formation, and refute recent statements to the contrary. Kyanite, Staurolite, and garnet are most abundant in the Setters schist north of Texas, Maryland. South of that point, the schist contains little or no kyanite or Staurolite, and only rare garnet, possibly reflecting a change in sedimentary facies. 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.