Fig. 9 in An Unusual Tasmanian Tertiary Basalt Sequence, Near Boat Harbour, Northwest Tasmania

Main Authors: Sutherland, F. L., Hendry, D. F., Barron, B. J., Matthews, W. L., Hollis, J. D.
Format: info Image Journal
Terbitan: , 1996
Subjects:
Online Access: https://zenodo.org/record/4659077
Daftar Isi:
  • Fig. 9. Comparative incompatible minor and trace element patterns envelopes (filled sections) for Cassidys Creek-Table Cape rocks, with nephelinites (left) and ne hawaiites-mugearites (right). Elemental abundances are normalised to primitive mantle values after Sun & McDonough (1989). Cassidys Creek nephelinites are contrasted with low Rb nephelinites from NE Tasmania (joined solid dots, data from Frey et al., 1978) and Barrington volcanic province, New South Wales (joined triangles, data from O'Reilly & Zhang, 1995). Cassidys Creek evolved rocks are contrasted with low Rb nepheline hawaiite from Table Cape (joined squares, data from Table 11). The Ba enriched Cassidys Creek ne mugearite (Analyses 8-9) are not plotted due to restricted incompatible element data.
  • Published as part of Sutherland, F. L., Hendry, D. F., Barron, B. J., Matthews, W. L. & Hollis, J. D., 1996, An Unusual Tasmanian Tertiary Basalt Sequence, Near Boat Harbour, Northwest Tasmania, pp. 131-161 in Records of the Australian Museum 48 (2) on page 141, DOI: 10.3853/j.0067-1975.48.1996.285, http://zenodo.org/record/4659059