Landsat linear features and mineral occurrences in Alaska
dc.contributor.author | Metz, P.A. | |
dc.date.accessioned | 2012-11-20T20:27:36Z | |
dc.date.available | 2012-11-20T20:27:36Z | |
dc.date.issued | 1983 | |
dc.identifier.citation | Metz, P.A., 1983, Landsat linear features and mineral occurrences in Alaska: University of Alaska Mineral Industry Research Laboratory Report No. 66, 83 p., 6 sheets. | en_US |
dc.identifier.uri | http://hdl.handle.net/11122/1123 | |
dc.description.abstract | In order to develop and better understanding of the regional structural controls of the metallic mineral deposits of Alaska, a detailed examination was made of the linear features and trends interpreted from Landsat imagery. In addition, local structural features and alteration zones were examined by ratio analysis of selected Landsat images. The linear trend analysis provided new regional structural data for previously proposed mineral deposit models and also provided new evidence for the extension of the existing models. Preliminary evidence also suggests linear intersection control of some types of mineral occurrences and that trend analysis may result in the definition of areas favorable for future mineral exploration. Ratio image analysis indicates that alteration zones and local structural features can be identified by use of Landsat imagery. Ratio image analysis for the definition of alteration zones must be used with caution, however, since the alteration associated with the various mineral deposits may not be differentiated by the technique. | en_US |
dc.description.sponsorship | This research was supported by a grant from the Mining and Mineral Resources Research Institute, Office of Surface Mining, U.S. Department of Interior. | en_US |
dc.publisher | University of Alaska Mineral Industry Research Laboratory | en_US |
dc.relation.ispartofseries | MIRL Report;no.66 | |
dc.title | Landsat linear features and mineral occurrences in Alaska | en_US |
dc.type | Technical Report | en_US |
refterms.dateFOA | 2020-01-24T15:01:38Z |