Zobrazeno 1 - 10 of 24 pro vyhledávání: '"Gregory C. Nadon"'
1
Reconstructing source-to-sink systems from detrital zircon core and rim ages
Autor: Li Liu, Daniel F. Stockli, Timothy F. Lawton, Jie Xu, Lisa D. Stockli, Majie Fan, Gregory C. Nadon
Publikováno v: Geology. 50:691-696
Grenville-age (1.3–0.9 Ga) zircons represent one of the most ubiquitous detrital zircon (DZ) age modes on Earth. In North America, given the widespread occurrence of Grenville basement, Grenville DZs are commonly viewed as nondiagnostic with regard
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::653b7bf4575e9965d1870221338646fb
https://doi.org/10.1130/g49904.1
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7
A paleopedologic and ichnologic perspective of the terrestrial Pennsylvanian landscape in the distal Appalachian Basin, U.S.A
Autor: Daniel I. Hembree, Gregory C. Nadon
Publikováno v: Palaeogeography, Palaeoclimatology, Palaeoecology. 312:138-166
The Conemaugh Group of southeastern Ohio contains numerous ichnofossil-bearing paleosols in both the lower Glenshaw and upper Casselman formations, which were deposited during the Kasimovian and Gzhelian (305–301 Ma) along the distal edge of the Ap
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::62afa89429da2dfd311dbf33c21f2bca
https://doi.org/10.1016/j.palaeo.2011.10.004
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8
Large, complex burrow systems from freshwater deposits of the Monongahela Group (Virgilian), Southeast Ohio, USA
Autor: Daniel I. Hembree, Michael R. King, Gregory C. Nadon
Publikováno v: Palaeogeography, Palaeoclimatology, Palaeoecology. 300:128-137
A large burrow complex is described from the Monongahela Group (Upper Pennsylvanian) in southeastern Ohio. The burrow complex consists of a branching network of elliptical to circular, horizontal tunnels, 1–18 cm in diameter, occurring on a single
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::37de9931242b24308c13e1aa7b7d9007
https://doi.org/10.1016/j.palaeo.2010.12.016
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9
Carbon isotopes support the presence of extensive land floras pre-dating the origin of vascular plants
Autor: Alexandru M. F. Tomescu, Lisa M. Pratt, Gregory C. Nadon, Paul K. Strother, Gar W. Rothwell
Publikováno v: Palaeogeography, Palaeoclimatology, Palaeoecology. 283:46-59
Multiple lines of evidence indicate that Earth's land masses became green some 2.7 Ga ago, about 1 billion years after the advent of life. About 2.2 billion years later, land plants abruptly appear in the fossil record and diversify marking the onset
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::6703ac154a76cdf6d768ee5ad63bd089
https://doi.org/10.1016/j.palaeo.2009.09.002
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10
Tectonic Control on the Sequence Stratigraphy of Nonmarine Retroarc Foreland Basin Fills: Insights from the Upper Jurassic of Central Utah, U.S.A
Autor: Xavier Roca, Gregory C. Nadon
Publikováno v: Journal of Sedimentary Research. 77:239-255
Continental successions of the North American Western Interior retroarc foreland basin provide an excellent opportunity to evaluate the tectonic controls on nonmarine sequence stratigraphy. The transition between the Upper Jurassic Brushy Basin Membe
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::003fcaae020551a5b312776df2ac5e09
https://doi.org/10.2110/jsr.2007.021
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