| Abstract: | These are considered similar if not synonymous when occurring in lime mudstone or syndepositional dolomite, especially in association with mudcracks and stromatolites. Compaction experiments indicate, however, that in the absence of early cementation, these vugs can be completely obliterated, whereas mudcracks and stromatolites remain relatively unchanged. -from Author |
| Genre: | Article |
| ProdID: | 70011285 |
| Citation Author: | Shinn, E. A. |
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| Citation End Page: | 628 |
| Citation Issue: | 2 |
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| Citation Language: | English |
| Citation Larger Work Title: | Journal of Sedimentary Petrology |
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| Citation Number Of Pages: | 10 |
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| Citation Search Results Text: | Birdseyes, fenestrae, shrinkage pores, and loferites: a reevaluation.; 1983; Article; Journal; Journal of Sedimentary Petrology; Shinn, E. A. |
| Citation Start Page: | 619 |
| Citation Volume: | 53 |
| Citation Year: | 1983 |
| Type: | citation/reference |
| Text: | Birdseyes, fenestrae, shrinkage pores, and loferites: a reevaluation.; 1983; Article; Journal; Journal of Sedimentary Petrology; Shinn, E. A. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sat, 1 Jan 1983 00:00 -0600 |
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