Abstract
Sedimentary facies generated by repetitive burrow excavation and infilling commonly are massively bedded and generally are mottled skeletal packstones. Skeletal grains usually are well-preserved and coarser components are concentrated in burrow networks, pockets and patches. The coarse skeletal components of burrow-generated facies are a mixture of coarse bioclasts from the precursor facies and both the coarse and fine skeletal material introduced from the sediment surface. -from Authors
| Original language | English (US) |
|---|---|
| Pages (from-to) | 326-343 |
| Number of pages | 18 |
| Journal | Palaios |
| Volume | 6 |
| Issue number | 3 |
| DOIs | |
| State | Published - Jan 1 1991 |
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ASJC Scopus subject areas
- Ecology, Evolution, Behavior and Systematics
- Palaeontology
Cite this
Generation of sedimentary fabrics and facies by repetitive excavation and storm infilling of burrow networks, Holocene of south Florida and Caicos Platform, BWI. / Tedesco, L. P.; Wanless, Harold.
In: Palaios, Vol. 6, No. 3, 01.01.1991, p. 326-343.Research output: Contribution to journal › Article
}
TY - JOUR
T1 - Generation of sedimentary fabrics and facies by repetitive excavation and storm infilling of burrow networks, Holocene of south Florida and Caicos Platform, BWI
AU - Tedesco, L. P.
AU - Wanless, Harold
PY - 1991/1/1
Y1 - 1991/1/1
N2 - Sedimentary facies generated by repetitive burrow excavation and infilling commonly are massively bedded and generally are mottled skeletal packstones. Skeletal grains usually are well-preserved and coarser components are concentrated in burrow networks, pockets and patches. The coarse skeletal components of burrow-generated facies are a mixture of coarse bioclasts from the precursor facies and both the coarse and fine skeletal material introduced from the sediment surface. -from Authors
AB - Sedimentary facies generated by repetitive burrow excavation and infilling commonly are massively bedded and generally are mottled skeletal packstones. Skeletal grains usually are well-preserved and coarser components are concentrated in burrow networks, pockets and patches. The coarse skeletal components of burrow-generated facies are a mixture of coarse bioclasts from the precursor facies and both the coarse and fine skeletal material introduced from the sediment surface. -from Authors
UR - http://www.scopus.com/inward/record.url?scp=0026276877&partnerID=8YFLogxK
UR - http://www.scopus.com/inward/citedby.url?scp=0026276877&partnerID=8YFLogxK
U2 - 10.2307/3514912
DO - 10.2307/3514912
M3 - Article
AN - SCOPUS:0026276877
VL - 6
SP - 326
EP - 343
JO - Palaios
JF - Palaios
SN - 0883-1351
IS - 3
ER -