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long time and can be reactivated on numerous occasions. This results in individual lenses that are a
                 hundred  meters  thick  and  extend  hundred  meters  along  strike.   The  reactivation  also  causes  the
                 deposits to be zoned around the black smoker pipe, with a predictable distribution of sulphides.
                 The massive accumulations of sulphides show up very well in geophysical surveys because they are
                 both denser and more conductive than the surrounding rock, making VMS deposits a relatively easy
                 geophysical exploration targets.
                 The shape of the deposits makes VMS ideal for cheap open-pit mining methods because a large amount
                 of ore can be removed without having to remove very much waste rock. This is a much cheaper mining
                 method  than  when  ore  is  hosted  in  narrow  veins,  resulting  in  a  much  higher  ratio  of  waste  to  ore
                 removal..
                 VMS deposits often occur in clusters within a particularly small area (~10 km ) all related to the same
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                 event, since the metal-rich fluids may escape to the surface through many vents. The discovery of one
                 large VMS deposit may well mean that there are other targets nearby.
                 Almost any age of terrain can potentially host a VMS deposit. The oldest VMS style deposits are some 3.4
                 billion years old while the youngest are being deposited today in oceans including the Red Sea and the
                 western  Pacific  Ocean.  There  are  ~800  VMS  deposits  known  worldwide  with  about  350  of  those  in
                 Canada.  Worldwide  there  is  much  exploration  for  VMS-style  deposits,  particularly  in  the  remote
                 Canadian arctic.


                 Important Deposits
                 Flin Flon,Manitoba, Canada.

                                                                 Kidd Mine in Timmins, Ontario, Canada.

                                                                 The  Flin  Flon  Greenstone  Belt  are  ancient
                                                                 Precambrian  rocks  which  host  the  biggest
                                                                 concentration of VMS deposits in Canada. The
                                                                 ore  bodies  are  predominantly  zinc-copper
                                                                 with  significant  gold  and  silver.  Ore  bodies
                                                                 range in size from 100,000 tonnes to 60 million
                                                                 tonnes.
                                                                 One  of  the  largest  producers  is  Hudbay
                                                                 Minerals Inc. that was founded in 1927 to mine
                 the region. Their 777 Mine produces zinc, copper, gold and silver.

                 They are currently developing a new project at Snow Lake some 215km north of Flin Flon. In 2012 their
                 production figures included:
                 •  39,587 tonnes copper
                 •  80,866 tonnes zinc
                 •  101,059 ounces of silver and gold.
                 Kidd Mine, Timmins, Ontario, Canada
                 The mine is hosted in the Abitibi greenstone belt which is around 2.8 – 2.6 billion years old Kidd Mine is
                 operated by Xstrata and is one of the world’s deepest base metal mines. Opened as an open pit mine in
                 the 1960’s it’s currently mining at 2800m below ground. The main commodities are copper and zinc.

                 Gravity Surveys

                 Gravity Surveys – the basics
                 Gravity surveys measure minute variations in gravity. Gravity at every point on the surface of the earth
                 varies slightly depending on:
                 •  distance from the equator;



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