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MORRISON, STAN J., PARRY, W. T. (1988) Age and formation conditions of alteration associated with a collapse structure, Temple Mountain uranium district, Utah. Geological Society of America Bulletin, 100 (7) 1069-1077 doi:10.1130/0016-7606(1988)100<1069:aafcoa>2.3.co;2

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Reference TypeJournal (article/letter/editorial)
TitleAge and formation conditions of alteration associated with a collapse structure, Temple Mountain uranium district, Utah
JournalGeological Society of America Bulletin
AuthorsMORRISON, STAN J.Author
PARRY, W. T.Author
Year1988 (July)Volume100
Issue7
PublisherGeological Society of America
DOIdoi:10.1130/0016-7606(1988)100<1069:aafcoa>2.3.co;2Search in ResearchGate
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Mindat Ref. ID54551Long-form Identifiermindat:1:5:54551:6
GUID0
Full ReferenceMORRISON, STAN J., PARRY, W. T. (1988) Age and formation conditions of alteration associated with a collapse structure, Temple Mountain uranium district, Utah. Geological Society of America Bulletin, 100 (7) 1069-1077 doi:10.1130/0016-7606(1988)100<1069:aafcoa>2.3.co;2
Plain TextMORRISON, STAN J., PARRY, W. T. (1988) Age and formation conditions of alteration associated with a collapse structure, Temple Mountain uranium district, Utah. Geological Society of America Bulletin, 100 (7) 1069-1077 doi:10.1130/0016-7606(1988)1002.3.co;2
In(1988, July) Geological Society of America Bulletin Vol. 100 (7) Geological Society of America

Mineral Occurrences

LocalityMineral(s)
Temple Mountain Mining District, Emery County, Utah, USAβ“˜ Alunite

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BAKER, VICTOR R. (1988) Geological fluvial geomorphology. Geological Society of America Bulletin, 100 (8) 1157-1167 doi:10.1130/0016-7606(1988)100<1157:gfg>2.3.co;2
GUILBERT, J. M. (1988) 100 years of economic geology and GSA. Geological Society of America Bulletin, 100 (6) 811-817 doi:10.1130/0016-7606(1988)100<0811:yoegag>2.3.co;2
DUTRO, JR., J. THOMAS (1988) Paleontology and The Geological Society of America: The first 100 years. Geological Society of America Bulletin, 100 (10) 1528-1532 doi:10.1130/0016-7606(1988)100<1528:patgso>2.3.co;2
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