Zobrazeno 1 - 10
of 85
pro vyhledávání: '"Guy Plint"'
Autor:
Michael J. Hay, A. Guy Plint
Publikováno v:
The Depositional Record, Vol 6, Iss 3, Pp 524-551 (2020)
Abstract After prograding for several hundred kilometres during Middle Cenomanian time, the Dunvegan delta complex in north‐west Alberta and adjacent British Columbia experienced stepwise transgression, commencing at about the Middle to Late Cenoma
Externí odkaz:
https://doaj.org/article/4f7d4447fbf44102b354c158415f9abf
Autor:
Lawrence Percival, Niels van Helmond, Guy Plint, Nina Papadomanolaki, Yue Gao, Steven Goderis, Philippe Claeys
The Cenomanian–Turonian Oceanic Anoxic Event (OAE 2: 94 Ma) marked one of the most severe episodes of climate and environmental change during the Cretaceous Period. The primary feature of this interval was widespread marine anoxia/euxinia, leading
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::01620b255174724cdf4ad1bd6f8b6c9a
https://doi.org/10.5194/egusphere-egu23-8959
https://doi.org/10.5194/egusphere-egu23-8959
Publikováno v:
Historical Biology. 35:403-429
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::77a29db98c8f43c99a595cbc3e9d615c
https://doi.org/10.1080/08912963.2022.2043294
https://doi.org/10.1080/08912963.2022.2043294
Autor:
A. Guy Plint, David Uličný, Stanislav Čech, Ireneusz Walaszczyk, Darren R. Gröcke, Jiří Laurin, Joel A. Shank, Ian Jarvis
Publikováno v:
Earth and Planetary Science Letters, 2022, Vol.578, pp.117323 [Peer Reviewed Journal]
Previous studies of Cretaceous sedimentary rocks have used multi-proxy correlation methods to suggest eustatic change, modulated by the c. 400 kyr long eccentricity rhythm. Although numerous authors have inferred eustatic changes on shorter timescale
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8d68e5938c827417f02cdcce93b5e028
http://dro.dur.ac.uk/35357/1/35357.pdf
http://dro.dur.ac.uk/35357/1/35357.pdf
Autor:
A. Guy Plint
Publikováno v:
The Sedimentary Record. 17:4-7
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9ecae535b62a504eb35a4c59ef65dce4
https://doi.org/10.2110/sedred.2019.4.4
https://doi.org/10.2110/sedred.2019.4.4
Autor:
A. Guy Plint
Publikováno v:
Geologia Croatica, Vol 56, Iss 1, Pp 39-68 (2003)
The early–mid Cenomanian Dunvegan Formation represents a largedelta complex that prograded at least 400 km from NW to SE. Aregional stratigraphy based on marine transgressive surfaces andequivalent subaerial interfluves allows the formation to be s
Externí odkaz:
https://doaj.org/article/4b39d4ec9133496f83d189e1ee8c7545
Autor:
A. Guy Plint, Michael A. Kreitner
Publikováno v:
Bulletin of Canadian Petroleum Geology. 67:71-116
The great Late Cenomanian transgression of the Greenhorn Sea is recorded in western Alberta and adjacacent British Columbia by shallow-marine deposits of the lower Kaskapau Formation that blanket underlying deltaic deposits of the Dunvegan Formation.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4f94748dcf89a6c61462c9f40954a2d1
https://doi.org/10.35767/gscpgbull.67.2.71
https://doi.org/10.35767/gscpgbull.67.2.71
Publikováno v:
Cretaceous Research. 128:104967
Numerous crocodylian swim tracks occur in the late Early Cretaceous and earliest Late Cretaceous of western North America, in coastal plain deposits marginal to the Cretaceous interior seaways. New assemblages from the lower Albian Gates Formation, w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6cbcb8dce71cb0df67cf249c55eca2f1
https://doi.org/10.1016/j.cretres.2021.104967
https://doi.org/10.1016/j.cretres.2021.104967
Publikováno v:
Bulletin of the American Museum of Natural History. Jun2017, Issue 414, p1-172. 6p.
Autor:
Jessica R. Krawetz, A. Guy Plint, Ireneusz Walaszczyk, Kathleen M. Vannelli, Robin A. Buckley
Publikováno v:
The Depositional Record. 4:4-58
In north-central Alberta and adjacent British Columbia, clastic strata of the middle to late Albian Peace River and Shaftesbury formations were deposited in alluvial to shallow marine environments across the foredeep of the Western Canada Foreland Ba
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4707c09392863b805f484996726590c6
https://doi.org/10.1002/dep2.37
https://doi.org/10.1002/dep2.37