Zobrazeno 1 - 10
of 157
pro vyhledávání: '"John W.F. Waldron"'
Autor:
Sean J. Loyd, Patrick Meister, Bo Liu, Kevin Nichols, Frank A. Corsetti, Robert Raiswell, William Berelson, Graham Shields, Mark Hounslow, John W.F. Waldron, Bayne Westrick-Snapp, Jamie Hoffman
Publikováno v:
EPIC3Geochimica et Cosmochimica Acta, Elsevier BV, 351, pp. 152-166, ISSN: 0016-7037
Early diagenesis of marine organic matter dramatically impacts Earth’s surface chemistry by changing the burial potential of carbon and promoting the formation of authigenic mineral phases including carbonate concretions. Marine sediment-hosted car
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cedf4f4a37f939144fd1719881cf52cd
https://doi.org/10.1016/j.gca.2023.04.022
https://doi.org/10.1016/j.gca.2023.04.022
Autor:
Lei Wu, J. Brendan Murphy, William J. Collins, John W.F. Waldron, Zheng-Xiang Li, Sergei A. Pisarevsky, Galen P. Halverson
Publikováno v:
GSA Bulletin. 134:2790-2808
The Paleozoic era begins with the final assembly of Gondwana and ends with the amalgamation of the supercontinent Pangea. Although this tectonic progression is generally well documented, one fundamental but under-studied phenomenon during this era is
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3ffa6f38da98b70d2ac230a2d5fc0374
https://doi.org/10.1130/b36158.1
https://doi.org/10.1130/b36158.1
Publikováno v:
Canadian Journal of Earth Sciences. 58:1103-1115
The ca. 355 Ma Fountain Lake Group in the Cobequid Highlands of Nova Scotia, is part of the transtensional basin fill that formed during dextral strike-slip motion between Avalonia and the Meguma terranes following the Acadian Orogeny. Paleomagnetic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::81b142960124335a42e8f8aad6157e6c
https://doi.org/10.1139/cjes-2020-0165
https://doi.org/10.1139/cjes-2020-0165
Autor:
Alex Zagorevski, Sandra M. Barr, Chris E. White, John W.F. Waldron, Cees R. van Staal, David I. Schofield
Publikováno v:
Gondwana Research. 98:212-243
West and East Ganderia in the northern Appalachians and Caledonides, respectively, represent a Gondwanan superterrane situated along the Tornquist margin of Amazonia prior to Furongian drift into the Iapetus Ocean, which opened the Rheic Ocean from w
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::be5dc8d2627e474ded2e362fc2c37f38
https://doi.org/10.1016/j.gr.2021.05.025
https://doi.org/10.1016/j.gr.2021.05.025
Autor:
John W.F. Waldron, Phil J.A. McCausland, Sandra M. Barr, David I. Schofield, Doug Reusch, Lei Wu
The Iapetus Ocean was the first ancient ocean to be identified following the development of plate tectonics; its history has been fundamental in relating orogenesis and plate motion. The ocean probably formed following 3-way rifting between Laurentia
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a103bcb4a5a4b9daa3863543b7f5f9cf
Autor:
Sandra M. Barr, Phil J.A. McCausland, Gregory R. Dunning, John W.F. Waldron, Halima S. Warsame, Chris E. White
Publikováno v:
Canadian Journal of Earth Sciences. 58:315-331
Paleomagnetic results and a U–Pb baddeleyite age from the Silurian Mavillette gabbroic sill in southwest Nova Scotia, Canada, provide new evidence about the Paleozoic tectonic evolution of the Meguma terrane. The Mavillette gabbro sill intruded ca.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::558ed3b3175e10271218d9b0ddfda210
https://doi.org/10.1139/cjes-2020-0089
https://doi.org/10.1139/cjes-2020-0089
Autor:
Sydney A. Lancaster, John W.F. Waldron
Publikováno v:
Geoscience Communication, Vol 3, Pp 249-262 (2020)
Boundary|Time|Surface was an ephemeral, site-specific sculpture created to draw attention to the construction of social, political, scientific, and aesthetic boundaries that divide the Earth; one such practice is the scientific subdivision of geologi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::fe5ae9225d8e2c285340d0c3667f7576
https://doi.org/10.5194/gc-3-249-2020
https://doi.org/10.5194/gc-3-249-2020
Autor:
William J. Collins, Lei Wu, Sergei Pisarevsky, Cecilio Quesada, J. Brendan Murphy, Simon Williams, Zheng-Xiang Li, John W.F. Waldron
Publikováno v:
GSA Bulletin. 133:625-646
The supercontinent Pangea formed by the subduction of the Iapetus and Rheic oceans between Gondwana, Laurentia, and Baltica during mid-to-late Paleozoic times. However, there remains much debate regarding how this amalgamation was achieved. Most pale
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::44f255ecc7686e95fd94d0f5368275c2
https://doi.org/10.1130/b35633.1
https://doi.org/10.1130/b35633.1
Autor:
Rhian Kendall, David I. Schofield, A. G. Leslie, John W.F. Waldron, Philip R. Wilby, R. Dartnall
Publikováno v:
Geological Society, London, Special Publications. 503:371-390
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9644a373bd3d86891464dab0024cf384
https://doi.org/10.1144/sp503-2020-9
https://doi.org/10.1144/sp503-2020-9
Publikováno v:
American Journal of Science. 320:450-477
The thrust front of the Northern Appalachians involves Ediacaran rift-related structures of the Laurentian margin that were re-worked in Taconic (Ordovician), Salinic (mainly Silurian) and Acadian (mainly Devonian) deformation events. Much of the thr
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1ef11fd322f100057d655c00df3995fc
https://doi.org/10.2475/05.2020.02
https://doi.org/10.2475/05.2020.02