Zobrazeno 1 - 6
of 6
pro vyhledávání: '"Lucian Rinke‐Hardekopf"'
Publikováno v:
The Depositional Record, Vol 8, Iss 2, Pp 754-785 (2022)
Abstract The McMurray Formation in McMurray Depocentre, Canada, is typically subdivided into stratigraphic units based on regionally mappable marine mudstones, the bases of which define flooding surfaces (bottom to top: Lower McMurray, C2, C1, B2, B1
Externí odkaz:
https://doaj.org/article/dfe3cfd2ed3b4790a6fdb46a6242e9ff
Publikováno v:
Geoscience Frontiers, Vol 12, Iss 2, Pp 877-892 (2021)
In the Lower Cretaceous McMurray-Clearwater succession of the intracontinental Alberta Foreland Basin, Canada, detrital zircon U-Pb geochronology samples (referred to herein as DZ samples) have been used to interpret the strata as representing a pale
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1abe994d3ac3b64e222fb4584df4478d
http://www.sciencedirect.com/science/article/pii/S1674987120302619
http://www.sciencedirect.com/science/article/pii/S1674987120302619
Publikováno v:
International Journal of Coal Geology. 204:18-33
Strata of the Lower Cretaceous McMurray Formation in the McMurray Sub-Basin (MSB) of Alberta and Saskatchewan, Canada, comprise marginal marine, tidal-fluvial, fluvial and interfluve deposits. In the Firebag Tributary located in the northeastern port
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b38e98b39026f84dc188e9c41c503e5f
https://doi.org/10.1016/j.coal.2019.01.011
https://doi.org/10.1016/j.coal.2019.01.011
Publikováno v:
Marine and Petroleum Geology. 91:622-630
Syn-sedimentary deformation and submarine channel initiation are both important processes influencing the stratigraphic development and reservoir properties of carbonate platforms. Based on a high-resolution 3D seismic dataset our study shows that pl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c26a04e246f811956828e65d99f5a1a7
https://doi.org/10.1016/j.marpetgeo.2017.12.034
https://doi.org/10.1016/j.marpetgeo.2017.12.034
Autor:
Lucian Rinke-Hardekopf, Murray K. Gingras, Shahin E. Dashtgard, S.W. Fietz, James A. MacEachern
Publikováno v:
Sedimentary Geology. 426:106028
Point bars are common in the fluvio-tidal transition of rivers, yet detailed characterization of their sedimentology and neoichnology is rarely reported. Herein, we present sedimentological and ichnological descriptions for a seaward translating poin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a0a7376861e138f086b2dd4a7ddd30b3
https://doi.org/10.1016/j.sedgeo.2021.106028
https://doi.org/10.1016/j.sedgeo.2021.106028
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4aee3f031ecb1ca6b90635ea1dba01f6
https://doi.org/10.1130/abs/2017am-300851
https://doi.org/10.1130/abs/2017am-300851