Zobrazeno 1 - 10
of 37
pro vyhledávání: '"Robert P. Raeside"'
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Canadian Journal of Earth Sciences. 54:1165-1178
At Kellys Mountain, Cape Breton Island, Nova Scotia, the late Neoproterozoic Glen Tosh formation (a low-grade metapsammite–metapelite unit of the George River Metamorphic Suite) has been intruded by diorite, granodiorite, and granite plutons, and t
Publikováno v:
Atlantic Geology. 46:95-126
Late Neoproterozoic (680 Ma to 560 Ma) Avalonian rocks in the Mira terrane of southeastern Cape Breton Island have been metamorphosed inhomogeneously, at very low grade to low grade, as recorded in mafic volcanogenic rocks (metabasite). Local occurre
Autor:
Richard A. F. Grieve, Jean Pilon, Sandra M. Barr, Ian Spooner, Peir K. Pufahl, George Stevens, Jared R. Morrow, David W.A. McMullin, Robert P. Raeside, Cliff Stanley
Publikováno v:
Meteoritics & Planetary Science. 44:1193-1202
An approximately 0.4 km diameter elliptical structure formed in Devonian granite in southwestern Nova Scotia, herein named the Bloody Creek structure (BCS), is identified as a possible impact crater. Evidence for an impact origin is based on integrat
Publikováno v:
Quaternary International. 108:77-83
Paleoclimate records from northern British Columbia, southwestern Yukon, and adjacent Alaska suggest that Late Holocene climate may have been influenced by specific air mass circulation dynamics. The Aleutian lowpressure index (ALPI) is a measure of
Publikováno v:
Canadian Journal of Earth Sciences. 35:1252-1270
Geological correlations between Cape Breton Island and Newfoundland are apparent both in surface geology and at deeper crustal levels, based on similarities in Sm-Nd isotopic signatures. The Mira terrane of southeastern Cape Breton Island is part of
Autor:
Peter H. Reynolds, Robert P. Raeside, Sandra M. Barr, Gregory R. Dunning, Rebecca Anne Jamieson, Brent V. Miller
Publikováno v:
Geological Society of America Bulletin. 108:127-140
The Blair River Complex in northern Cape Breton Island, Nova Scotia, is interpreted to be an exposure of Grenvillian basement which formed the southeastern tip of a promontory on the proto-Atlantic continental margin of North America. U-Pb (zircon) d
Autor:
R.D. Dallmeyer, J. B. Murphy, Rebecca Anne Jamieson, J. D. Keppie, Sandra M. Barr, Robert P. Raeside
Publikováno v:
Geological Society of America Bulletin. 103:1376-1383
Autor:
Sandra M. Barr, Robert P. Raeside
Publikováno v:
Canadian Journal of Earth Sciences. 27:1371-1381
The Bras d'Or Terrane is defined in Cape Breton Island and consists of four distinctive components, (i) Low-pressure, regionally metamorphosed aluminous and calcareous gneiss of the Proterozoic Bras d'Or metamorphic suite is restricted to the southea
Publikováno v:
Canadian Journal of Earth Sciences. 27:1200-1208
U–Pb dates from zircon, titanite, and monazite in plutons of the Bras d'Or and Mira terranes of southern Cape Breton Island, combined with 40Ar/39Ar and other radiometric age data, indicate that the Bras d'Or and Mira terranes had separate magmatic