Microbially induced sedimentary structures - a new category within the classification of primary sedimentary structures-discussion

Journal of Sedimentary Research

Volumn 72, Issue 4, 2002, Pages 587-588

  Gingras, Murray K ^a  

^a UNIVERSITY OF NEW BRUNSWICK   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

MICROBIAL ACTIVITY; SEDIMENTARY STRUCTURE;

EID: 0036045032     PISSN: 15271404     EISSN: None     Source Type: Journal    
DOI: 10.1306/101401720587     Document Type: Article

References (16)

1. Wrinkle marks, an intertidal sedimentary structure due to aseismic soft- sediment loading
2. The role of wave reworking on the architecture of storm sandstone facies. Bell Island Group (Lower Ordovician), eastern Newfoundland
3. Estuarine deposits
4. The ichnology of modern and Pleistocene brackish-water deposits at Willapa Bay. Washington: Variability in estuarine settings
5. Wrinkle structures, microbially mediated sedimentary structures common in subtidal siliciclastic settings at the Proterozoic-Phanerozoic transition
6. Faziesuntersuchungen im Hettangium von Helmstedt (Niedersachsen)
7. Aspects of a middle Cambrian thanatotope on Öhlund
8. Multidirectional ripple marks rising from biological and sedimentological processes in modern lower supratidal deposits (Mellum Island, southern North Sea)
9. Microbially induced sedimentary structures-A new category within the classification of primary sedimentary structures
10. Matground structures and redox facies
11. Die Entstehung von Runzelmarken
12. Lithostratigraphy of the Cambrian-lower Ordovician Saint John group, Southern New Brunswick
13. Runzelmarken (wrinkle marks)
14. Trace fossils in a middle triassic mixed siliciclastic-carbonate marginal marine depositional system