Zobrazeno 1 - 10
of 57
pro vyhledávání: '"C. Blaine Cecil"'
Autor:
C. Blaine Cecil, William A. DiMichele, Jeffrey M. Rahl, Frank T. Dulong, Lauren Michel, Scott D. Elrick
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 618:111521
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::467f4a82ea42033c2179f39c6a46a2d6
https://doi.org/10.1016/j.palaeo.2023.111521
https://doi.org/10.1016/j.palaeo.2023.111521
Publikováno v:
Journal of Sedimentary Research. 88:743-752
Among the numerous models that have been suggested for the primary and predominant source of silica for chert, we suggest that eolian dust is worthy of further considerations. Such considerations are supported by the common association of Phanerozoic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::330bb645f3bb59f9da22025847c99200
https://doi.org/10.2110/jsr.2018.39
https://doi.org/10.2110/jsr.2018.39
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8691ce644ddcb38c21b0e8278d335b80
https://doi.org/10.1130/abs/2019am-333685
https://doi.org/10.1130/abs/2019am-333685
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::954f9a9b08a01c554bc7d1fc9b6b6ff2
https://doi.org/10.1130/abs/2018am-318029
https://doi.org/10.1130/abs/2018am-318029
Autor:
C. Blaine Cecil
Publikováno v:
The Sedimentary Record. 13:4-10
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::24829465c1d6767cf794c8dd0b2931f0
https://doi.org/10.2110/sedred.2015.3.4
https://doi.org/10.2110/sedred.2015.3.4
Publikováno v:
Comptes Rendus Geoscience. 346:159-168
The Pennsylvanian portion of the Late Paleozoic Ice Age was characterized by stratigraphic repetition of chemical and siliciclastic rocks in the equatorial regions of the Pangean interior. Known as “cyclothems”, these stratigraphic successions ar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9854dc0f3396d36050b8f22275c0f01c
https://doi.org/10.1016/j.crte.2014.03.008
https://doi.org/10.1016/j.crte.2014.03.008
Autor:
Isabel P. Montañez, C. Blaine Cecil
Publikováno v:
International Journal of Coal Geology. 119:41-55
Nonmarine limestones are a key component of the upper Middle Pennsylvanian through lower Permian succession in the Appalachian Basin. Previous interpretations of their environments of deposition range from brackish coastal mudflats to hydrologically
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::da8360571e9fcae3dc26f345df0b0c5f
https://doi.org/10.1016/j.coal.2013.08.009
https://doi.org/10.1016/j.coal.2013.08.009
Autor:
Roberta Sirmons, William A. DiMichele, Viktoras Skema, C. Blaine Cecil, Hans Kerp, Nick Fedorko, Bascombe M. Blake
Publikováno v:
International Journal of Coal Geology. 119:56-78
The Dunkard Group is the youngest late Paleozoic rock unit in the Central Appalachian Basin. Its age, however, remains controversial. In its southern and western two-thirds the Dunkard is comprised largely of red beds, sandstone and siltstone channel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::40d3b744deceb090cc2995f685ec0db1
https://doi.org/10.1016/j.coal.2013.07.025
https://doi.org/10.1016/j.coal.2013.07.025
Autor:
C. Blaine Cecil
Publikováno v:
International Journal of Coal Geology. 119:21-31
Autocyclic and allocyclic processes controlled the lithostratigraphy of strata that accumulated in the central Appalachian foreland basin during the Pennsylvanian and the transition to the Permian. The transition strata, from bottom to top, include t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a826b64815945e4de7fc0ed5985e502e
https://doi.org/10.1016/j.coal.2013.07.012
https://doi.org/10.1016/j.coal.2013.07.012
Publikováno v:
International Journal of Coal Geology. 83:329-344
Wetland floras narrowly define perceptions of Pennsylvanian tropical ecosystems, the so-called Coal Age. Such wetlands reflect humid to perhumid climate, leading to characterizations of Pennsylvanian tropics as everwet, swampy. These views are biased
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e99ee933597bd51911200fa634b8bfac
https://doi.org/10.1016/j.coal.2010.01.007
https://doi.org/10.1016/j.coal.2010.01.007