Page 63 - Introduction to Mineral Exploration
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46   A.M. EVANS & C.J. MOON



                  and the Environment  (1994) provides a good  geologist must be able to identify, or have iden-
                  introduction and a link with economics.     tified for him or her, every mineral in a possible
                  Sawkins’ Metal Deposits in Relation to Plate  orebody (see Chapter 2). This will help them to
                  Tectonics (second edition 1990, Springer    assess the full economic potential of any mate-
                  Verlag) gives an overview of the major struc-  rial to be mined from it and prevent them over-
                  tural controls on deposits.                 looking the presence of additional valuable
                                                              constituents or deleterious substances that
                                                              may render the deposit unworkable. There are
                  3.5  SUMMARY OF CHAPTERS 1, 2, AND 3        many techniques now available for compre-
                                                              hensive mineralogical examination of mineral
                  The general nature of ore, industrial minerals,  samples and these are discussed in section 2.2.
                  and orebodies are discussed in sections 1.1 and  However, such investigations must be quant-
                  1.2 and it is emphasized that these deposits  itative as well as qualitative; grain size and
                  must contain valuable constituents that can be  shape, relative mineral amounts, and the man-
                  economically recovered using suitable treat-  ner of interlocking must be determined.
                  ment. (Chapter 11 is largely devoted to a de-  The nature and morphology of mineral de-
                  tailed coverage of this principle.) In the past too  posits are very varied and only a restricted cov-
                  much interest in many mining circles has been  erage of these subjects can be given in this book
                  placed on the more glamorous metallic de-   (see section 3.1). The tyro is therefore strongly
                  posits and the general importance of industrial  recommended to acquire a broad knowledge of
                  minerals neglected (see section 1.2.2). The  these subjects from extended reading so that
                  value of both is governed by demand and     when he or she detects signs of mineralisation
                  supply (see section 1.2.3) and many factors in-  they may soon develop a working hypothesis of
                  cluding government action, recycling, and sub-  the nature of the particular beast they have
                  stitution play a part in determining their  come upon.
                  market prices. In section 1.3 the principal steps  Having recognized the tectonic setting of
                  involved in the exploration for, and develop-  an exploration region, models of the deposits
                  ment of, a mineral deposit are summarized   likely to be present, and particularly of those
                  and these are the subjects that are covered in  being sought, should be set up. Both empirical
                  more detail in the rest of this book. A sound  and genetic models are used, often in combina-
                  knowledge of these is necessary in choosing  tion, to show how the materials sought relate
                  exploration areas (see section 1.5.) leading to  to geological factors including geophysics and
                  the development of a rationale of mineral ex-  geochemistry. To understand how models are
                  ploration (see section 1.6).                constructed and used, unconformity-related
                    Economic mineral deposits are extremely   uranium deposits are discussed in some detail
                  variable in their mineralogy and grade and the  (see section 3.2.3).


                  3.6  APPENDIX: MINERAL DEPOSIT MODEL CLASSIFICATION OF COX AND SINGER (1986). ONLINE
                      LINKS CAN BE FOUND AT USGS (2004).

                  Mafic and ultramafic intrusions

                  A. Tectonically stable area; stratiform complexes
                  Stratiform deposits
                    Basal zone
                      Stillwater Ni-Cu                                                             1
                    Intermediate zone
                      Bushveld chromitite                                                          2a
                      Merensky Reef PGE                                                            2b
                    Upper zone
                      Bushveld Fe-Ti-V                                                             3
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