Steep microbial boundstone-dominated platform margins : examples and implications

Autor: Kenter, J. A. M., Harris, P. M., Della Porta, G.

Seaward progradation of several kilometers has been documented mostly for leeward margin low-angle carbonate slope systems with a dominant platform top sediment source. However, steep and high-relief margins fronting deep basins can also prograde and

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=od_______266::82b096966b88b294fd408ad28201eea4
https://publishup.uni-potsdam.de/frontdoor/index/index/docId/13700

A method for grain separation for analysis of size distributions

Autor: Antoon Meesters, Den Berg, E. H., Kenter, J. A. M.

Publikováno v: Meesters, A G C A, van den Berg, E H & Kenter, J A M 1999, ' A method for grain separation for analysis of size distributions. ', pp. 34 .
None
Vrije Universiteit Amsterdam

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::1f23767409d702abba65dba7b1b56bc6
https://research.vu.nl/en/publications/a0ed0e41-f7a4-416b-9f0b-a9547c0936a3

The origin and nature of seismic reflections of sharp-based shoreface deposits (upper Jurassic Siliciclastics, northern France).

Autor: Braaksma, H., Drijkoningen, G. G., Filippidou, N., Kenter, J. A. M., Proust, J. N.

Publikováno v: Geophysical Prospecting; Mar2006, Vol. 54 Issue 2, p211-236, 26p, 1 Color Photograph, 1 Diagram, 13 Graphs

Note on a mid-Proterozoic stromatolite limestone, south of Grythyttan, Bergslagen, Sweden

Autor: Boekschoten, G. J., Raad, A. C. V. D., Kenter, J. A. M., John J.G. Reijmer

Publikováno v: Geologie en Mijnbouw, 67(2-4), 467-469. Koninklijk Nederlands Geologisch Mijnbouwkundig Genootschap
Scopus-Elsevier
Boekschoten, G J, Raad, A C V D, Kenter, J A M & Reymer, J J G 1988, ' Note on a mid-Proterozoic stromatolite limestone, south of Grythyttan, Bergslagen, Sweden ', Geologie en Mijnbouw, vol. 67, no. 2-4, pp. 467-469 .
Vrije Universiteit Amsterdam

Relatively well-preserved limestones are present in a sequence of volcanoclastics of mid-Proterozoic age; textures are characteristic for stromatolites. -from Authors

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::6c0cfe568618ae9c7ad42bc840df93f8
https://hdl.handle.net/1871.1/03b19cb5-6405-4976-b323-e22e79e9529a