Zobrazeno 1 - 10
of 12
pro vyhledávání: '"Larry J. Hulbert"'
Autor:
D. Graham Pearson, Bruce A. Kjarsgaard, Larry J. Hulbert, Bill Davis, Stephen W. Parman, Pedro Waterton, Andrew J. Locock
Publikováno v:
Lithos. :114-130
The Proterozoic spans the longest portion of earth's history, yet in contrast to the Archaean, the record of komatiites and related high MgO igneous rocks from this Eon is sparse. This paper describes the pristine Palaeoproterozoic Winnipegosis Komat
Publikováno v:
Lithos. :242-258
The 1.27 Ga Coppermine continental flood basalt (CFB) province in northern Canada represents the extrusive manifestation of the 2.7 Mkm2 Mackenzie large igneous province (LIP) that includes the Mackenzie dyke swarm and the Muskox layered intrusion. N
Publikováno v:
Journal of Petrology. 49:1255-1295
Platinum-group element (PGE: Os, Ir, Ru, Pt, Pd) and Re^Os isotope systematics determined for the entire preserved stratigraphy of the 1 27 Ga Muskox intrusion provide an exceptional view of magma chamber processes and mineralization in the main plut
Autor:
C. Michael Lesher, Thomas Menard, Tullis C. Onstott, Larry J. Hulbert, Harold H. Stowell, David P. Price, James R. Pickell
Publikováno v:
Economic Geology. 91:1394-1413
The Namew Lake Fe-Ni-Cu sulfide deposit, 60 km south of Flin Flon, Manitoba, is hosted by an undifferentiated metapyroxenite sill enclosed within Early Proterozoic orthogneisses and covered by Paleozoic sedimentary rocks. The Namew Lake pyroxenite co
Publikováno v:
Journal of Petrology. 37:317-359
Previous magnetic fabric studies of the giant, radiating, 1.27 Ga Mackenzie dyke swarm concluded that flow patterns within the dykes support the concept of a mantle plume that is centred beneath the swarm focus and supplies magma to overlying flood b
Autor:
Larry J. Hulbert, Mary F. Horan, R.I Grauch, Raymond M. Coveney, James B. Murowchick, John W. Morgan
Publikováno v:
Geochimica et Cosmochimica Acta. 58:257-265
Rhenium and osmium abundances and osmium isotopic compositions were determined by negative thermal ionization mass spectrometry for samples of Devonian black shale and an associated Ni-enriched sulfide layer from the Yukon Territory, Canada. The same
Autor:
O. M. Burnham, Larry J. Hulbert, C. M. Lesher, Monecke Thomas, Richard J. Goldfarb, Erin E. Marsh, Reid R. Keays, J. P. Golightly, D. Layton-Matthews, David C. Peck
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d24ecf1385f0a98116a8239d027b50b3
https://doi.org/10.5382/sp.15.2.09
https://doi.org/10.5382/sp.15.2.09
Publikováno v:
Economic Geology. 77:1296-1306
The lower zone of the Potgietersrus limb of the Bushveld Complex consists of a succession of ultramafic rocks, at least 1,600 m thick, that can be subdivided into 37 cyclic units. Ni, Cu, and Pt mineralization is developed at two levels in the sequen
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