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Volumn 39, Issue 6, 2002, Pages 933-942

Variation in plagioclase clouding intensity in Matachewan dykes: Evidence for the exhumation history of the northern margin of the Sudbury Igneous Complex

Author keywords

[No Author keywords available]

Indexed keywords

DEFORMATION; FELDSPAR; GRANITE; IMAGE ANALYSIS;

EID: 0035996109     PISSN: 00084077     EISSN: None     Source Type: Journal    
DOI: 10.1139/e02-003     Document Type: Article
Times cited : (12)

References (49)
  • 6
    • 0001829558 scopus 로고
    • Geology of the Levack gneiss complex, the northern footwall of the Sudbury structure, Ontario
    • Geological Survey of Canada, Paper 1994-C
    • (1994) Current research, part C , pp. 269-278
    • Card, K.D.1
  • 18
    • 0001034950 scopus 로고
    • Variations in paleomagnetic direction and feldspar clouding intensity across the Matachewan dyke swarm and their relevance to the Huronian
    • (1995) Canadian Mineralogist , vol.33 , pp. 935-937
    • Halls, H.C.1
  • 21
    • 0031972307 scopus 로고    scopus 로고
    • Uplift structure of the southern Kapuskasing zone from 2.45 Ga dike swarm displacement
    • (1998) Geology , vol.26 , pp. 67-70
    • Halls, H.C.1    Zhang, B.2
  • 23
    • 0030988884 scopus 로고    scopus 로고
    • Global mafic magmatism at 2.45 Ga: Remnants of an ancient large igneous province?
    • (1997) Geology , vol.25 , pp. 299-302
    • Heaman, L.M.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.