Magnetic petrology of igneous intrusions: implications for exploration and magnetic interpretation

Author:

Clark David A.1

Affiliation:

1. CSIRO Exploration and MiningPO Box 136 North Ryde, NSW,2113.

Publisher

Informa UK Limited

Subject

Geology,Geophysics

Reference17 articles.

1. Blevin, P.L., 1996, Using magnetic susceptibility meters to interpret the oxidation state of granitic rocks: 13th Australian Geological Convention, Geological Society of Australia, Abstracts41, 40.

2. Chappell, B.W., White, A.J.R. and Hiñe, R., 1988, Granite provinces and basement terranes in the Lachlan Fold Belt, southeastern Australia: Australian Journal of Earth Sciences, 35, 505-521.

3. Clark, A.H. and Arancibia, O.N., 1996, The occurrence, paragenesis and implications of magnetite-rich alteration-mineralization in calc-alkaline porphyry copper deposits,inClark, A.H., Ed., Giant ore deposits - II, controls on the scale of orogenic magmatic-hydrothermal mineralization, Second Giant Ore Deposits Workshop, 583-640.

4. Dunlop, D.J. and Özdemir, Ö., 1997, Rock magnetism: fundamentals and frontiers: Cambridge University Press.

5. Frost, B.R., 1991a. Magnetic petrology: factors that control the occurrence of magnetite in crustal rocks,inLindsley, D.H., Ed., Oxide minerals: petrologic and magnetic significance: Reviews in Mineralogy,25, 489-509.

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