Page 36 - Introduction to Mineral Exploration
P. 36

2: MINERALOGY OF ECONOMIC DEPOSITS  19
                                                          2



                               The Mineralogy of

                               Economic Deposits




                                            Anthony M. Evans








                 2.1  INTRODUCTION                            pegmatites and in the mill the ore is processed
                                                              to produce chemical grade spodumene and
                 Ore minerals are the minerals of economic    ceramic spodumene concentrates, mica and
                 interest for which the explorationist is search-  feldspar concentrates, and a quartz–feldspar
                 ing. They can be metallic or nonmetallic. Min-  mix marketed as sandspar. The amphibolite
                 eralogy is used to understand the relationships  host rock is crushed, sized, and sold as road
                 between the ore mineral and the uneconomic   aggregate. Of course such comprehensive ex-
                 host rock for their eventual separation.     ploitation of all the material mined is not
                   Economic mineral deposits consist of every  possible in isolated locations, but too often
                 gradation from bulk materials or aggregates, in  the potential of waste material is overlooked.
                 which most of the rock or mineral is of com-  A  comprehensive mineralogical examination
                 mercial value, to deposits of precious metals  of a mineral deposit and its waste rocks may
                 (gold, silver, PGM) from which only a few ppm  mean that additional valuable materials in
                 (or ppb in the case of diamond deposits) are  the deposit are identified and the presence of
                 separated and sold. The valuable mineral in one  deleterious substances detected. This may add
                 deposit may be a gangue mineral in another,  value if the project is ever brought to the pro-
                 e.g. quartz is valuable in silica sands, but is  duction stage and will help to avoid embarrass-
                 a gangue mineral in auriferous quartz veins.  ing undervaluation.
                 Thus the presentation of lists of ore and gangue  Ore minerals may be native metals (ele-
                 minerals without any provisos, as given in   ments), of which gold and silver are examples,
                 some textbooks, can be very misleading to the  or compounds of metals with sulfur, arsenic,
                 beginner. This may lead to an erroneous ap-  tellurium, etc., such as lead sulfide – the min-
                 proach to the examination of mineral deposits,  eral galena (PbS) – or they may be carbonates,
                 i.e. what is recovered and what is discarded?  silicates, borates, phosphates. There are few
                 An alternative question is, how can we process  common minerals that do not have an eco-
                 everything we are going to mine and market   nomic value in some mineralogical context or
                 the products at a profit? There are few mineral  other. Some of the more important ore min-
                 operations where everything is mined gain-   erals are listed in Table 2.1 and those which
                 fully. Fortunes can be made out of the waste  are often classified as gangue minerals in Table
                 left by previous mining and smelting opera-  2.2. Ore minerals may be classed as primary
                 tions, but not usually by the company that   (hypogene) or secondary (supergene). Hypogene
                 dumped it! A good example of a mine where    minerals were deposited during the original
                 everything is mined is at the King’s Mountain  period of rock formation or mineralisation.
                 Operation in the Tin–Spodumene Belt of North  Supergene minerals were formed during a later
                 Carolina. It is in the world’s most import-  period of mineralisation, usually associated
                 ant lithium-producing area (Kunasz 1982).    with weathering and other near-surface proc-
                 The spodumene occurs in micaceous granite–   esses, leading to precipitation of the secondary
   31   32   33   34   35   36   37   38   39   40   41