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area the
Nipissing diabase is deformed; outcrops are parallel to the fold axes of the Huronian sedimentary rocks. Nipissing diabase intrusions are east-northeast trending and are no wider than 460 m (1,510 ft).
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area 1,300 km (810 mi) to the northeast. The mantle source for the
Nipissing sills did not come from the mantle beneath the Southern Province that had generated the 2500– to 2450–million year old
228:
Palmer, H. C.; Ernst, R. E.; Buchan, K. L. (April 1, 2007). "Magnetic Fabric
Studies of the Nipissing sill province and Senneterre dykes, Canadian shield, and Implications for Emplacement".
214:
Ancient LIPS Reconstructed (2.50, 2.45, 2.22 & 2.10 Ga): The
Utility Of Precise Magmatic “Barcodes” And “Piercing Points” In Matching Ancient Continental Fragments
381:
Palmer, H.C.; Ernst, R.E.; Buchan, K.L. (2004). "Mapping Flow
Patterns in Nipissing sills of the Southern Province, Canadian shield: a Magnetic Fabric Study".
345:
Mineral
Deposits of Canada: A Synthesis of Major Deposit-Types, District Metallogeny, the Evolution of Geological Provinces, and Exploration Methods
342:
Ernst, Richard E. (January 1, 2007). "Large
Igneous Provinces in Canada Through Time and Their Metallognic Potential". In Goodfellow, W. D. (ed.).
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center 1,500 km (930 mi) away via the 2216–million year old
Senneterre dikes which form part of the radiating dike swarm.
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272:(submitted in conformity with the requirements for the degree of M.Sc. Graduate Department of Geology University of Toronto thesis)
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Differential Uplift of the
Archean Basement North of the Sudbury Basin: Petrographic Evidence from tahe Matachewan Dyke Swarm
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465:
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The
Nipissing sills in the Southern Province of the Superior craton are thought to originate from a radiating
88:. Nipissing sills intrude all the Huronian sediments and older basement rocks in the northern margin of the
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140:– fed the Nipissing sills; evidence shows the sills were laterally fed from a
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389:. American Geophysical Union, Spring Meeting 2004, abstract #GP34A-04: GP34A–04.
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293:""Sudbury Breccia" at Whitefish Falls, Ontario: Evidence for an Impact Origin"
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In 1911, Willett G. Miller named the Nipissing diabase type area at
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Parmenter, Andrew C.; Lee, Christopher B.; Coniglio, Mario (2002).
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355:, Mineral Deposits Division. pp. 929–937. Archived from
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20:
Nipissing sills associated with Ungava magmatic event
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132:. The 2217– to 2210–million year old
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297:Canadian Journal of Earth Sciences
236:(4). NRC Research Press: 507–528.
230:Canadian Journal of Earth Sciences
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353:Geological Association of Canada
476:Landforms of Nipissing District
408:Jambor, J. L. (December 1971).
92:; they were emplaced after the
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189:Engineering and Mining Journal
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471:Landforms of Sudbury District
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456:Igneous petrology of Ontario
383:AGU Spring Meeting Abstracts
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161:Volcanism of Eastern Canada
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100:of Huronian rocks, and are
10:
502:
481:Geology of Greater Sudbury
466:Paleoproterozoic magmatism
185:"Notes on the Cobalt Area"
183:Miller, Willet G. (1911).
136:– located under the
417:The Canadian Mineralogist
266:Siddom, James P. (1999).
410:"The Nipissing diabase"
21:
134:Ungava magmatic event
130:Matachewan dike swarm
19:
111:composition. In the
84:, which intrude the
395:2004AGUSMGP34A..04P
309:2002CaJES..39..971P
242:2007CaJES..44..507P
86:Huronian Supergroup
38: /
60:, also called the
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109:tholeiitic basalt
62:Nipissing diabase
42:47.400°N 79.683°W
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486:Mafic intrusions
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149:Cobalt, Ontario
138:Labrador Trough
74:Canadian Shield
70:Superior craton
58:Nipissing sills
47:47.400; -79.683
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434:September 8,
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199:September 8,
197:. Retrieved
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142:mantle plume
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117:Elliot Lake
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450:Categories
167:References
125:dike swarm
102:hornblende
429:0008-4476
195:: 645–649
366:June 12,
322:June 12,
276:June 12,
155:See also
94:faulting
391:Bibcode
305:Bibcode
238:Bibcode
115:–
113:Sudbury
98:folding
78:Ontario
72:of the
68:in the
33:79°41′W
30:47°24′N
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105:gabbro
82:Canada
413:(PDF)
360:(PDF)
349:(PDF)
66:sills
436:2024
425:ISSN
387:2004
368:2010
324:2010
278:2010
201:2024
96:and
56:The
313:doi
246:doi
107:of
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Text is available under the Creative Commons Attribution-ShareAlike License. Additional terms may apply.
