Zobrazeno 1 - 10
of 40
pro vyhledávání: '"J. C. Roddick"'
Publikováno v:
Geological Journal. 17:279-295
A Rb-Sr whole-rock isochron study indicates that the entire Donegal granite suite was emplaced into orthotectonic Caledonian (Dalradian) rocks over a short interval during mid-Silurian to earliest-Devonian times. The Thorr pluton, probably the earlie
Publikováno v:
Geological Society of America Bulletin. 108:101-116
Reverse-oblique overthrusting of high-grade Port aux Basques Gneiss over the lower-grade, supracrustal Windsor Point Group along the Cape Ray fault zone occurred during late Silurian to early Devonian time and is attributed to major oblique collision
Publikováno v:
The Journal of Geology. 103:711-717
The Stare Sedlo gneiss complex occurs as a roof pendant in the early Carboniferous Central Bohemian Pluton. Mylonitic tonalitic gneiss and amphibolite in the complex share a common foliation, which is discordant to the margins of the granitoid masses
Publikováno v:
Contributions to Mineralogy and Petrology. 120:212-222
Rb-Sr isotopic dating of phlogopite megacryst samples separated from Sturgeon Lake kimberlite, Saskatchewan, yields a crystallization age of 98±1 Ma (2 σ, MSWD=1.2; 87Sr/86Sr(t)=0.7059). The 40Ar/39Ar analyses of a phlogopite megacryst sample indic
Publikováno v:
Canadian Journal of Earth Sciences. 31:995-1001
An 40Ar/39Ar study of white micas from high-pressure metamorphic rocks of northern New Caledonia yielded cooling ages of 37 ± 1 Ma for both epidote and omphacite zone samples. Whole-rock samples from the lawsonite zone yielded ages in the range 44
Publikováno v:
Canadian Journal of Earth Sciences. 29:3-14
The Ag–Pb–Zn–Au vein and replacement deposits of the Kokanee Range, southeastern British Columbia, are hosted by the Middle Jurassic Nelson batholith and surrounding Cambrian to Triassic metasedimentary rocks in the hanging wall of the transcru
Publikováno v:
Canadian Journal of Earth Sciences. 28:754-761
The high-level McGerrigle Mountains plutonic complex consists of a compositionally diverse (gabbro to granite) hybrid suite at its northern end and a relatively homogeneous granite suite in its southern half. Field and geochemical evidence support fo
Publikováno v:
Contributions to Mineralogy and Petrology. 105:219-241
The Wild Bight Group (WBG) is a sequence of early and middle Ordovician volcanic, subvolcanic and epiclastic rocks, part of the Dunnage Tectonostratigraphic Zone of the Newfoundland Appalachians. A detailed geochemical and Nd-isotopic study of the vo