Skip navigation
  • Home
  • Browse
    • Communities
      & Collections
    • Browse Items by:
    • Publication Date
    • Author
    • Title
    • Subject
    • Department
  • Sign on to:
    • My MacSphere
    • Receive email
      updates
    • Edit Profile


McMaster University Home Page
  1. MacSphere
  2. Open Access Dissertations and Theses Community
  3. Open Access Dissertations and Theses
Please use this identifier to cite or link to this item: http://hdl.handle.net/11375/5907
Full metadata record
DC FieldValueLanguage
dc.contributor.advisorHowarth, P.J.en_US
dc.contributor.authorSpitzer, Roberten_US
dc.date.accessioned2014-06-18T16:33:24Z-
dc.date.available2014-06-18T16:33:24Z-
dc.date.created2009-07-28en_US
dc.date.issued1981-10en_US
dc.identifier.otheropendissertations/125en_US
dc.identifier.other1489en_US
dc.identifier.other913488en_US
dc.identifier.urihttp://hdl.handle.net/11375/5907-
dc.description.abstract<p>The use of Landsat and Seasat data for lineament and lithologic mapping has been evaluated for a study area in southeastern Ontario. Lineaments were identified and mapped from several Landsat products (i.e. DICS CCT's and transparencies, RBV and MSS imagery) and Seasat imagery. Interpreted lineament distributions were compared visually and statistically with fault and joint distributions recorded from the geologic maps of the area. Lineaments interpreted from enhanced (linear contrast stretch and 3X3 high pass filter) DICS summer and winter imagery were compared with mapped faults for a small site within the study area. Interpreted lineament length and intersection densities were compared visually and statistically with two aspects of the economic geology of the area. Discrimination of lithologies was attempted by interpreting textures and tones found on the imagery. The results of the lineament and lithologic mapping were compared with the hypothesized tectonic history of the area. It was determined that lineaments mapped from the remotely sensed data reflect the fault distribution as interpreted from the geologic map. However, lineaments identified on DICS winter imagery best reflect the fault distributions. Identification of lineaments was easier on winter imagery than summer imagery. The two computer enhancements did not aid in the identification of lineaments. A relationship between two lineament parameters and areas of mineralization was found. Lithologic discrimination from remotely sensed imagery proved difficult, although intrusive rocks were readily identifiable, particularly in the low grade metamorphic areas. Results from both the lineament and lithologic mapping provided information which is compatible with the tectonic history of the area.</p>en_US
dc.subjectGeographyen_US
dc.subjectGeographyen_US
dc.titleLandsat and Seasat data for lineament and lithologic mapping in southeastern Ontarioen_US
dc.typethesisen_US
dc.contributor.departmentGeographyen_US
dc.description.degreeMaster of Science (MS)en_US
Appears in Collections:Open Access Dissertations and Theses

Files in This Item:
File SizeFormat 
fulltext.pdf
Open Access
6.21 MBAdobe PDFView/Open
Show simple item record Statistics


Items in MacSphere are protected by copyright, with all rights reserved, unless otherwise indicated.

Sherman Centre for Digital Scholarship     McMaster University Libraries
©2022 McMaster University, 1280 Main Street West, Hamilton, Ontario L8S 4L8 | 905-525-9140 | Contact Us | Terms of Use & Privacy Policy | Feedback

Report Accessibility Issue