Age and palaeoenvironmental constraints on the genesis of the Yandi channel iron deposits, Marillana Formation, Pilbara, northwestern Australia*
Author:
Publisher
Wiley
Subject
General Earth and Planetary Sciences,Earth and Planetary Sciences (miscellaneous)
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1111/j.1400-0952.2004.01071.x/fullpdf
Reference81 articles.
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2. AlleyN. F. & BenbowM. C.1989. Late Eocene palynofloras from the Pidinga Formation, SADME Ooldea Range 6, eastern Eucla Basin . Geological Survey of South Australia Quarterly Geological Notes11, 2–12.
3. AlleyN. F., ClarkeJ. D. A., MacphailM. & TruswellE. M.1999. Sedimentary infillings and development of major Tertiary palaeodrainage systems of south‐central Australia . International Association of Sedimentologists Special Publication27, 337–366.
4. Alonso‐Zarsa, A. M. (2003) Palaeoenvironmental significance of palustrine carbonates and calcretes in the geological record Earth‐Science Reviews, 60, pp. 261 - 298.
5. Anand, R. R. and Paine, M. (2002) Regolith geology of the Yilgarn Craton, Western Australia: implications for exploration Australian Journal of Earth Sciences, 49, pp. 3 - 162.
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