Zobrazeno 1 - 10
of 20
pro vyhledávání: '"R J Wardle"'
Publikováno v:
Geological Journal. 18:195-222
The Precambrian sequences of the Avalon Zone in Canada (southeastern margin of the Appalachian Orogen) are interpreted as a Pan-African orogenic belt incorporated into the Appalachian Orogen during Palaeozoic times as its southeastern margin. The Pre
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2ec148ec55d4f1fa6eca9adc356630dc
https://doi.org/10.1002/gj.3350180302
https://doi.org/10.1002/gj.3350180302
Autor:
Ron M. Clowes, J.F. Lewry, Jeremy Hall, S. B. Lucas, Zoltán Hajnal, R J Wardle, Frederick A. Cook
Publikováno v:
Episodes. 22:3-20
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::432d9e19b36a8235da0556b391bc8b3a
https://doi.org/10.18814/epiiugs/1999/v22i1/002
https://doi.org/10.18814/epiiugs/1999/v22i1/002
Autor:
M. J. Van Kranendonk, R J Wardle
Publikováno v:
Canadian Journal of Earth Sciences. 34:1545-1565
Large variations in metamorphic grade over short distances, disparate orientations and diverse kinematics of contemporaneous structures, and a previously unexplained, 90° counterclockwise bend in the orogenic boundary of the amphibolite- to granulit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8d7fc48dd938a76871f1bb827f2ef633
https://doi.org/10.1139/e17-126
https://doi.org/10.1139/e17-126
Autor:
R. J. Wardle, M. J. Van Kranendonk
Publikováno v:
Geological Society, London, Special Publications. 112:137-153
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0b2a6a925bca0e0a9d64dc1b87be6ec0
https://doi.org/10.1144/gsl.sp.1996.112.01.08
https://doi.org/10.1144/gsl.sp.1996.112.01.08
Autor:
Martin J. Van Kranendonk, R J Wardle
Publikováno v:
Geological Society, London, Special Publications. 112:91-115
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fb22f46c239203bbf00cb3af7dc54684
https://doi.org/10.1144/gsl.sp.1996.112.01.06
https://doi.org/10.1144/gsl.sp.1996.112.01.06
Publikováno v:
Canadian Journal of Earth Sciences. 30:2315-2327
Major initial crust formation in the northeastern Grenville Province of Labrador occurred during the Labradorian orogeny (1710–1620 Ma) prior to re-deformation in the Grenvillian orogeny between 1050 and 950 Ma. The Goose Bay region includes severa
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b41e409a0f55663d1f3ae25e91f173c8
https://doi.org/10.1139/e93-201
https://doi.org/10.1139/e93-201
Autor:
L Godin, R Patey, M J Van Kranendonk, R J Wardle, F C Mengel, L Reid, R Churchill, L M Campbell, D Bridgwater, S Schwarz, B Ryan, D J Scott, A Haumann
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ca44e6d15bfec26d37c178535dbe0cad
https://doi.org/10.4095/203609
https://doi.org/10.4095/203609
Autor:
L Godin, M J Van Kranendonk, D J Scott, A Haumann, D Bridgwater, R Churchill, S Schwarz, B Ryan, R Patey, L Reid, R J Wardle, F C Mengel, L M Campbell
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::63d397dc9f96dd10e11d685fbc143f44
https://doi.org/10.4095/305842
https://doi.org/10.4095/305842
Publikováno v:
Canadian Journal of Earth Sciences
The Seal Lake Group of eastern Labrador unconformably overlies the 1273 ± 1 Ma (2σ) Harp Dyke Swarm. In its lower parts, the Seal Lake Group includes conglomerates, quartzites, and red-bed sediments, and both the lower and middle parts are intruded
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6b688e1a97a83207e7602d86dfe1a090
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:243231
http://gfzpublic.gfz-potsdam.de/pubman/item/escidoc:243231