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- W2334774462 abstract "Research Article| January 01, 1976 Fracture Patterns and Anisotropy of San Manuel Quartz Monzonite FRANCIS S. KENDORSKI; FRANCIS S. KENDORSKI Francis S. Kendorski is with Leeds, Hill and Jewett, Inc., San Francisco, California. Search for other works by this author on: GSW Google Scholar M. ASHRAF MAHTAB M. ASHRAF MAHTAB M. Ashraf Mahtab is with Acres Consulting Services, Ltd., Niagara Falls, Ontario, and formerly with Denver Mining Research Center, U.S. Bureau of Mines, Denver, Colorado. Search for other works by this author on: GSW Google Scholar Environmental and Engineering Geoscience (1976) xiii (1): 23–52. https://doi.org/10.2113/gseegeosci.xiii.1.23 Article history first online: 02 Mar 2017 Cite View This Citation Add to Citation Manager Share Icon Share Twitter LinkedIn Tools Icon Tools Get Permissions Search Site Citation FRANCIS S. KENDORSKI, M. ASHRAF MAHTAB; Fracture Patterns and Anisotropy of San Manuel Quartz Monzonite. Environmental and Engineering Geoscience 1976;; xiii (1): 23–52. doi: https://doi.org/10.2113/gseegeosci.xiii.1.23 Download citation file: Ris (Zotero) Refmanager EasyBib Bookends Mendeley Papers EndNote RefWorks BibTex toolbar search Search Dropdown Menu nav search search input Search input auto suggest search filter All ContentBy SocietyEnvironmental and Engineering Geoscience Search Advanced Search Abstract This report presents an interrelationship of the structure and anisotropy of the porphyry copper deposit of the San Manuel mine, Arizona. Analysis of orientations of the fractures mapped in the quartz monzonite of the ore body established the existence of an orthogonal fracture pattern. Oriented compression and Brazilian tension tests on the quartz monzonite showed that the mappable fracture pattern is reflected in planar weaknesses in the rock. Analysis of thin sections indicated that the existing microfractures controlled failure of the test specimens. These microfractures likely originated from fluid inclusion planes that were formed by stress relief.The fracture patterns mapped in the underground workings can be generalized as four sets: E–W and N–S, Both vertical; N. 80°E. to E–W, vertical; and horizontal. These sets are rotated up to 30°, with respect to both the depth and horizontal location in the mine. This suggests a location control within the pluton. Rock fractures are important controls on the mechanical behavior of rock masses and, if properly analyzed, are helpful in the design and safe operation of mining excavations. This content is PDF only. Please click on the PDF icon to access. First Page Preview Close Modal You do not currently have access to this article." @default.
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- W2334774462 title "Fracture Patterns and Anisotropy of San Manuel Quartz Monzonite" @default.
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