Page 75 - Introduction to Mineral Exploration
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58   C.J. MOON & M.K.G. WHATELEY



                  TABLE 4.3  Examples of budget forecasting for a  less developed countries, in spite of the avail-
                  low cost project and a project requiring drilling.  ability of satellite information. Besides surface
                  Land costs are excluded.                    mapping familiar to most geologists, a number
                                                              of other sources of information on regional geo-
                  Project                        Cost in US$  logy are widely used in exploration.
                                                                An invaluable addition to surface regional
                  Low cost project cost
                  Time: 6 days @ US$200 per day     1200      geology is the use of regional geophysics (see
                  Hotels and meals for 2 nights     350       Chapter 7). Airborne magnetics, radiometrics,
                  Transport (vehicle hire)          200       and regional gravity data are available for much
                  Assays                            200       of the developed world and help in refining
                  Office staff time                  100       geological interpretation and, particularly, in
                  TOTAL                             2050      mapping deep structures. For example, a belt of
                                                              the Superior Province in northern Manitoba
                  Medium cost project                         which hosts a number of major nickel deposits,
                  20 boreholes @ 200 m                        including the large deposit at Thompson, can
                    each = 4000 m
                  4000 m at US$50 per meter      200,000      be clearly followed under Palaeozoic cover to
                  Overhead costs                 200,000      the south (Fig. 4.4). Regional seismic data are
                  TOTAL                          400,000      helpful but are usually only available if oil
                                                              companies donate them to the public domain.
                                                              Specially commissioned seismic surveys have
                                                              greatly helped in deciphering the subsurface
                                                              geology of the Witwatersrand Basin (see sec-
                  also include open-file material from geological  tion 14.5.4). Subsurface interpretations of
                  surveys and departments of mines, data from  geophysical information can be checked by
                  colleagues and from consultants with particu-  linking them with information from any avail-
                  lar expertise in the area concerned.        able deep drill hole logs.
                    Background geological information is avail-  Regional geochemical surveys (see section
                  able for most areas in the world although its  8.4) also provide much information in areas of
                  scale and quality vary considerably. In some  poor outcrop and have defined major litho-
                  parts of Europe geological maps are published  logical provinces covered by boulder clay in
                  at 1:50,000 and manuscript field sheets at   Finland.
                  1:10,000 are available. In less populated parts  The sources of information for mineral
                  of the world, such as Canada or Australia, the  occurrence localities are similar to those for
                  base cover is 1:250,000 with more detailed  regional geology. Geological surveys usually
                  areas at 1:100,000. For the mineral exploration  have the most comprehensive data base within
                  geologist the published geological data will  a country and much of this is normally
                  only be a beginning and he or she will interpret  published (e.g. the summary of UK mineral
                  the geology using the geological features   potential of Colman 2000). Many surveys have
                  defined in the deposit model. This is best   collated all the mineral occurrences within
                  achieved by starting with a synoptic view of  their country and the results are available as
                  the geology from satellite imagery. Unless the  maps, reports, or even on computerized data-
                  area is extensively vegetated this is likely to be  bases. Two useful types of maps are mineral
                  from Landsat or SPOT imagery (see Chapter 6).  occurrence maps and metallogenic maps, many
                  Landsat has the added advantage of highlight-  of which are now available in digital format.
                  ing areas of hydrothermal alteration within arid  The former type merely shows the location of
                  areas if processed correctly. In areas of dense  the occurrences whereas the latter attempts to
                  vegetation side-looking radar can be used. For  show the form of the deposit and associated
                  example, most of Amazonian Brazil has been  elements overlain on background geology using
                  mapped in this way. For smaller areas air   GIS (see section 9.2). Overlays of the mineral
                  photography provides better resolution often  prospects with geology will provide clues to re-
                  at considerably less cost, although air photo-  gional controls on mineralisation. At this point
                  graphs are still regarded as top secret in some  some economic input is required as it is often
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