| Abstract: | Impsonite (asphaltic pyrobitumen) occurs as fracture-filling veins cutting massive sandstone in the frontal Ouachita Mountains near Page, Oklahoma. The Page impsonite formed from low-temperature alteration of crude oil. Mean maximum bitumen reflectance in oil immersion (Rmax) of seven samples is 1.41-1.96%. Mean apparent bireflectance of these samples is 0.15-0.54%. The Page deposit classifies at the upper end of epi-impsonite in the generic classification for solid bitumen, based on physical, chemical, and optical characteristics, and as post-oil with unlimited migration in the genetic classification for solid bitumen. ?? 1991. |
| Genre: | Article |
| ProdID: | 70015003 |
| Citation Author: | Cardott, B. J. |
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| Citation End Page: | 191 |
| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Organic Geochemistry |
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| Citation Number Of Pages: | 7 |
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| Citation Search Results Text: | Organic petrology of epi-impsonite at Page, Oklahoma, U.S.A.; 1991; Article; Journal; Organic Geochemistry; Cardott, B. J. |
| Citation Start Page: | 185 |
| Citation Volume: | 17 |
| Citation Year: | 1991 |
| Type: | citation/reference |
| Text: | Organic petrology of epi-impsonite at Page, Oklahoma, U.S.A.; 1991; Article; Journal; Organic Geochemistry; Cardott, B. J. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Tue, 1 Jan 1991 00:00 -0600 |
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