Zobrazeno 1 - 10
of 11
pro vyhledávání: '"Mark Smyk"'
Publikováno v:
Journal of Petrology.
The St. Ignace Island complex in Northern Ontario is a package of dominantly felsic rocks emplaced within the upper portions of the Osler Volcanic rocks of the ~1.1 Ga Midcontinent Rift System. The Osler volcanic rocks are predominantly tholeiitic ba
Publikováno v:
Geological Society, London, Special Publications. 518:43-65
Autor:
Wouter Bleeker, Robert Cundari, Michael R.M. Easton, Mark Smyk, Pete Hollings, Michael A. Hamilton
Publikováno v:
Canadian Journal of Earth Sciences. 58:1116-1131
The Midcontinent Rift System of North America is a ∼1.1 Ga large igneous province comprising mainly flood basalts and intrusive rocks. We present new data for the Pillar Lake Volcanics and Inspiration Sill from the northern edge of the Midcontinent
Publikováno v:
Geological Society of America Abstracts with Programs.
Publikováno v:
Precambrian Research. :269-279
New radiogenic isotope data are presented for intrusive rocks of the Mesoproterozoic Midcontinent Rift from the north shore of Lake Superior. These mafic rocks are amongst the older portions of the rift sequence and offer insights into the early deve
Publikováno v:
Precambrian Research. 183:553-571
The Midcontinent Rift (MCR) of North America comprises a series of basaltic sheets, flows and intrusive rocks emplaced in the Lake Superior region during the Mesoproterozoic. The mafic rocks preserved on the northern flank of Lake Superior represent
Autor:
R.M. Easton, Thomas Robert Hart, Carole Anne MacDonald, Mark Smyk, Pete Hollings, Larry M. Heaman
Publikováno v:
Canadian Journal of Earth Sciences. 44:1055-1086
The Midcontinent Rift in the Lake Superior region of North America is one of the best preserved examples of an aborted Precambrian intercontinental rift, one that hosts a diverse suite of rock types in addition to the well-studied and voluminous rift
Autor:
James M. Franklin, Mark Smyk
Publikováno v:
Canadian Journal of Earth Sciences. 44:1041-1053
A variety of metallic and non-metallic mineral deposit types occur within Archean and Proterozoic rocks in the area encompassing the Lake Nipigon Region Geoscience Initiative. Archean deposit types include Algoma-type banded iron formation-hosted iro
Autor:
David H. Watkinson, Mark Smyk
Publikováno v:
Canadian Journal of Earth Sciences. 27:1170-1181
The Archean volcano-sedimentary succession at Cobalt, Ontario, consists mainly of submarine andesitic flows and turbiditic interflow sedimentary rocks. Steeply dipping faults and large-scale, tight to isoclinar folds have developed in these basement