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Volumn 54, Issue 2-3, 2007, Pages 137-141

Geological evolution and metallogenesis of the Ordovician Macquarie arc, Lachlan Orogen New South Wales

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Indexed keywords


EID: 34147144206     PISSN: 08120099     EISSN: 14400952     Source Type: Journal    
DOI: 10.1080/08120090701221615     Document Type: Editorial
Times cited : (19)

References (21)
  • 1
    • 0042677069 scopus 로고
    • Geological setting of gold and copper deposits in the Parkes area, New South Wales
    • Clarke, I. and Sherwin, L. (1990) Geological setting of gold and copper deposits in the Parkes area, New South Wales. Records of the Geological Survey of New South Wales, 23:1
    • (1990) Records of the Geological Survey of New South Wales , vol.23 , Issue.1
    • Clarke, I.1    Sherwin, L.2
  • 3
    • 0032405593 scopus 로고    scopus 로고
    • Ordovician convergent-margin volcanism and tectonism in the Lachlan sector of east Gondwana
    • Glen, R. A., Walshe, J. L., Barron, L. M. and Watkins, J. J. (1998) Ordovician convergent-margin volcanism and tectonism in the Lachlan sector of east Gondwana. Geology, 26, pp. 751-754.
    • (1998) Geology , vol.26 , pp. 751-754
    • Glen, R.A.1    Walshe, J.L.2    Barron, L.M.3    Watkins, J.J.4
  • 8
    • 0002751286 scopus 로고
    • Palaeozoic plate tectonics in the southern Tasman Geosyncline
    • Oversby, B. (1971) Palaeozoic plate tectonics in the southern Tasman Geosyncline. Nature, 234, pp. 45-48.
    • (1971) Nature , vol.234 , pp. 45-48
    • Oversby, B.1
  • 9
    • 11544317911 scopus 로고
    • Geology and geochemistry of the Tantangara and Brindabella 1:100 000 sheet areas, New South Wales and Australian Capital Territory
    • Owen, M. and Wyborn, D. (1979) Geology and geochemistry of the Tantangara and Brindabella 1:100 000 sheet areas, New South Wales and Australian Capital Territory. Bureau of Mineral Resources Bulletin, 204
    • (1979) Bureau of Mineral Resources Bulletin , vol.204
    • Owen, M.1    Wyborn, D.2
  • 11
    • 0022007724 scopus 로고
    • Significance of clinopyroxene compositions from the Cudgegong volcanics and Toolamanang Volcanics: Cudgegong - Mudgee district, NSW Australia
    • Pemberton, J. and Offler, R. (1985) Significance of clinopyroxene compositions from the Cudgegong volcanics and Toolamanang Volcanics: Cudgegong - Mudgee district, NSW Australia. Mineralogical Magazine, 49, pp. 591-599.
    • (1985) Mineralogical Magazine , vol.49 , pp. 591-599
    • Pemberton, J.1    Offler, R.2
  • 13
    • 0020926249 scopus 로고
    • Tectonic relationships between the Late Ordovician and Late Silurian palaeogeographies of southeastern Australia
    • Powell McA, C. (1983) Tectonic relationships between the Late Ordovician and Late Silurian palaeogeographies of southeastern Australia. Journal of the Geological Society of Australia, 30, pp. 353-373.
    • (1983) Journal of the Geological Society of Australia , vol.30 , pp. 353-373
    • Powell, McA.C.1
  • 16
    • 84954916474 scopus 로고
    • A plate tectonic model of the Palaeozoic tectonic history of New South Wales
    • Scheibner, E. (1973) A plate tectonic model of the Palaeozoic tectonic history of New South Wales. Journal of the Geological Society of Australia, 20, pp. 405-426.
    • (1973) Journal of the Geological Society of Australia , vol.20 , pp. 405-426
    • Scheibner, E.1
  • 17
    • 0007721922 scopus 로고
    • Tectonic evolution of the Tasman Orogenic Zone, eastern Australia
    • Solomon, M. and Griffiths, J. R. (1972) Tectonic evolution of the Tasman Orogenic Zone, eastern Australia. Nature, 237, pp. 3-6.
    • (1972) Nature , vol.237 , pp. 3-6
    • Solomon, M.1    Griffiths, J.R.2
  • 21
    • 0027045898 scopus 로고
    • The tectonic significance of Ordovician magmatism in the eastern Lachlan Fold Belt
    • Wyborn, D. (1992) The tectonic significance of Ordovician magmatism in the eastern Lachlan Fold Belt. Tectonophysics, 214, pp. 287-303.
    • (1992) Tectonophysics , vol.214 , pp. 287-303
    • Wyborn, D.1


* 이 정보는 Elsevier사의 SCOPUS DB에서 KISTI가 분석하여 추출한 것입니다.