Page 50 - Introduction to Mineral Exploration
P. 50

3




                                   Mineral Deposit

                            Geology and Models




                          Anthony M. Evans and Charles J. Moon








                 A detailed understanding of the geology of   has to be cut back to maintain a safe overall
                 mineral deposits is required to explore effec-  slope to the sides of the pit (see section 11.2.1).
                 tively for them. As this is beyond the scope  Before discussing the nature of ore bodies we
                 of this volume, only some key features are   must learn some of the terms used in describ-
                 discussed here as well as how a more advanced  ing them.
                 appreciation of mineral deposit geology may    If an orebody viewed in plan is longer in one
                 be used in exploration programs. For further  direction than the other we can designate this
                 detailed consideration of mineral deposit geo-  long dimension as its strike (Fig. 3.1). The
                 logy the reader is referred to the companion  inclination of the orebody perpendicular to the
                 volume in this series by Robb (2004) and refer-  strike will be its dip and the longest dimension
                 ences listed in section 3.4.                 of the orebody its axis. The plunge of the axis
                                                              is measured in the vertical plane ABC but its
                                                              pitch or rake can be measured in any other
                 3.1  NATURE AND MORPHOLOGY OF                plane, the usual choice being the plane contain-
                     OREBODIES                                ing the strike, although if the orebody is fault
                                                              controlled then the pitch may be measured in
                                                              the fault plane. The meanings of other terms
                 3.1.1 Size and shape of ore deposits
                                                              are self-evident from the figure.
                 The size, shape, and nature of ore deposits    It is possible to classify orebodies in the
                 affects the workable grade. Large, low grade  same way as we divide up igneous intrusions
                 deposits which occur at the surface can be   according to whether they are discordant or
                 worked by cheap open pit methods, whilst thin  concordant with the lithological banding (often
                 tabular vein deposits will necessitate more  bedding) in the enclosing rocks. Considering
                 expensive underground methods of extraction.  discordant orebodies first, this large class can be
                 Open pitting, aided by the savings from bulk  subdivided into those orebodies which have an
                 handling of large daily tonnages (say  >30 kt),  approximately regular shape and those which
                 has led to a trend towards the large scale mining  are thoroughly irregular in their outlines.
                 of low grade orebodies. As far as shape is con-
                 cerned, orebodies of regular shape can generally
                 be mined more cheaply than those of irregular  Discordant orebodies
                 shape, particularly when they include barren
                 zones. For an open pit mine the shape and    Regularly shaped bodies
                 attitude of an orebody will also determine how
                 much waste has to be removed during mining.  Tabular orebodies. These bodies are extensive
                 The waste will often include not only over-  in two dimensions, but have a restricted devel-
                 burden (waste rock above the orebody) but also  opment in their third dimension. In this class
                 waste rock around and in the orebody, which  we have veins (sometimes called fissure-veins)
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