Zobrazeno 1 - 10 of 33 pro vyhledávání: '"E R W Neale"'
1
Post-Ophiolite Unconformity, Tilt Cove – Betts Cove Area, Newfoundland
Autor: H. D. Upadhyay, E. R. W. Neale, B. F. Kean
Publikováno v: Canadian Journal of Earth Sciences. 12:880-886
Subaerial sediments and silicic and mafic lavas of the Cape St. John Group in northern Newfoundland, were originally interpreted as younger than the Betts Cove ophiolite suite and the Lower Ordovician (Arenig) Snooks Arm pillow lavas and oceanic sedi
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::7c0089612b84380b1144d98092d3eeaa
https://doi.org/10.1139/e75-077
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2
On the tectonic regimes of ophiolite genesis
Autor: H.D. Upadhyay, E R W Neale
Publikováno v: Earth and Planetary Science Letters. 43:93-102
Ophiolites and their associated rocks are examined in terms of field relationships and petrochemistry. Many pre-obduction plagiogranite and dioritic dykes in the ophiolites of southern Quebec, Vourinos, California, Oregon and Newfoundland are judged
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::cdb7fbf6480f42e9069fd6a283501f59
https://doi.org/10.1016/0012-821x(79)90158-4
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5
The Northeastward Termination of the Appalachian Orogen
Autor: Harold Williams, M. J. Kennedy, E. R. W. Neale
Publikováno v: The Ocean Basins and Margins ISBN: 9781468430356
The Appalachian orogen is a northeast-trending belt of deformed rocks that lies southeast of the Canadian Shield and Interior Platform of central North America (Fig. 1). The northernmost part of the orogen is bounded to the east by the Atlantic Ocean
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::b2feb69b214e4e5b34f8384a2d33ba5a
https://doi.org/10.1007/978-1-4684-3033-2_4
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