Zobrazeno 1 - 7
of 7
pro vyhledávání: '"Wilson S. McClung"'
Publikováno v:
Basin Research.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1db6fcf08830fef18c4f651a2c358e49
https://doi.org/10.1111/bre.12764
https://doi.org/10.1111/bre.12764
Autor:
Wilson S. McClung, Kenneth A. Eriksson
Publikováno v:
The Journal of Geology. 129:625-646
To date, all source-to-sink research has focused on the Phanerozoic and Proterozoic stratigraphic record. This study attempts to apply source-to-sink principles to the 2.8–3.0 Ga placer gol...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e2dbb1a656502e7420f8ebe7bc9034c1
https://doi.org/10.1086/716963
https://doi.org/10.1086/716963
Publikováno v:
Earth-Science Reviews. 188:176-189
Climates during the Paleozoic varied from greenhouse to transitional to icehouse and siliciclastic successions deposited during those times have stratigraphic architectures consistent with magnitudes and frequencies of sea-level fluctuations at the t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::70e2ac1d1029afac9b48aaa56e3f6273
https://doi.org/10.1016/j.earscirev.2018.11.010
https://doi.org/10.1016/j.earscirev.2018.11.010
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. 490:355-374
Subsurface mapping and facies and architectural element analysis on outcrop, combined with published detrital zircon geochronology and sandstone petrography, are used to reconstruct a source to sink system for two incised-valley fills in the Upper Mi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::53d932edc37e3effdb18435be936989f
https://doi.org/10.1016/j.palaeo.2017.11.013
https://doi.org/10.1016/j.palaeo.2017.11.013
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. :125-143
The supposition that the Late Devonian Gondwanan glaciation should be recorded in more temperate regions by black shales, incised valleys, and lowstand wedges is tested with reference to the Foreknobs Formation (late Frasnian to early Famennian) of t
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a0b80dd38537094e3c4501035c3be7d5
Publikováno v:
Palaeogeography, Palaeoclimatology, Palaeoecology. :104-125
The Foreknobs Formation (Upper Devonian; Upper Frasnian to basal Famennian) comprises the uppermost marine strata of the progradational “Catskill clastic wedge” of the south-central Appalachian Mountains (Virginia-West Virginia; USA). The Forekno
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::13e2d3de36c14854509c5f1ab14f29f7
Autor:
Richard J. Gleason, Samuel S. Dashevsky, John K. Costain, Wilson S. McClung, Joseph J. Lambiase
Publikováno v:
Geology. 8:447
Analysis of geothermal gradients determined in 65 exploratory holes in the Atlantic Coastal Plain indicates that in many areas temperatures exceed 40 °C at the base of the sediments. Water of such temperature, if it is available in sufficient quanti
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::87ea004578153658d7c3d45bf7cc9e6b
https://doi.org/10.1130/0091-7613(1980)8<447:mgrpot>2.0.co
https://doi.org/10.1130/0091-7613(1980)8<447:mgrpot>2.0.co