Birdseyes, fenestrae, shrinkage pores, and loferites: a reevaluation.
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
Citation Information
Publication Year | 1983 |
---|---|
Title | Birdseyes, fenestrae, shrinkage pores, and loferites: a reevaluation. |
Authors | E.A. Shinn |
Publication Type | Article |
Publication Subtype | Journal Article |
Series Title | Journal of Sedimentary Petrology |
Index ID | 70011285 |
Record Source | USGS Publications Warehouse |