Birdseyes, fenestrae, shrinkage pores, and loferites: a reevaluation.
Journal of Sedimentary Petrology
By: E.A. Shinn
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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
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Birdseyes, fenestrae, shrinkage pores, and loferites: a reevaluation. |
| Series title | Journal of Sedimentary Petrology |
| Volume | 53 |
| Issue | 2 |
| Year Published | 1983 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Journal of Sedimentary Petrology |
| First page | 619 |
| Last page | 628 |
| Google Analytic Metrics | Metrics page |