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Volumn 44, Issue 2, 2001, Pages 185-192

The paleomagnetism and geological significance of mesoproterozoic dyke swarms in the Central North China Craton

Author keywords

Apparent polar wander path; Magnetic inclination; Mesoproterozoic mafic dyke swarms; Paleomagnetism

Indexed keywords

DEFORMATION; GEOLOGY; MAGNETISM; METAMORPHIC ROCKS; ROTATION;

EID: 0035244138     PISSN: 10069313     EISSN: None     Source Type: Journal    
DOI: 10.1007/bf02879661     Document Type: Article
Times cited : (16)

References (19)
  • 3
    • 0022859877 scopus 로고
    • Paleomagnetism, structure and longitudinal correlation of middle Precambrian dykes from northwestern Ontario and Minnesota
    • (1985) Can. J. Earth Sci , vol.23 , pp. 142
    • Halls, H.C.1
  • 9
    • 0000595527 scopus 로고    scopus 로고
    • The formation mechanism and tectonic stress field of Mesoproterozoic mafic dyke swarms in the North China Craton
    • (in Chinese)
    • (1998) Geological Review , vol.44 , Issue.3 , pp. 309
    • Hou, G.1    Zhang, C.2    Qian, X.3
  • 13
    • 0000577286 scopus 로고
    • The magnetic fabric evidence of Late Precambrian mafic dyke swarms emplacement in North Shanxi and Wutai inlier
    • (in Chinese)
    • (1994) Geological Review , vol.40 , Issue.3 , pp. 245
    • Zhang, C.1    Hou, G.2    Qian, X.3
  • 19
    • 0028570985 scopus 로고
    • Magnetic fabric and post-orogenic uplift and cooling magnetizations in a Precambrian granulite terrain: The Datong-Huai'an region of the North China Shield
    • (1994) Tectonophysics , vol.234 , pp. 227
    • Zhang, J.1    Piper, J.D.A.2


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.