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These are rocks that have been altered by heat and pressure so much so that they become another
                 rock type. Often geologists can recognize the original rock that has been metamorphosed and will refer
                 to the rock as a “meta-sedimentary” rock or meta-volcanic. Though sometimes it is not possible to
                 confidently determine the original rock type.

                          Metamorphic rock from an Archean greenstone belt.
                 Rocks in old terranes, such as the Archean greenstone belts of Canada,
                 are often highly metamorphosed, while those of younger terranes may
                 not be as altered depending on their geologic setting.
                 Metamorphic rocks may often be labelled as “high grade” or “low grade
                 metamorphic”. These “grades” are are a reference to the temperature and
                 pressure  to  which  the  rock  was  exposed  based  on  it’s  texture  and
                 mineralogy  and  does  not  have  any  specific  economic  meaning.
                 However, metamorphic  processes  may  help  concentrate  economic
                 minerals.

                 Examples:
                 •  Red Lake Greenstone Belt: Gold
                 •  Broken Hill, Australia: Lead, Zinc, Silver
                 While there many, many more ways to classify rocks and mineral deposits, understanding the basics of
                 rock classification and mineral associations can go a long way in helping one understand the processes
                 involved and the descriptions of economic deposits published by geologists.
                 Home / Mineral Deposits / Porphyry Copper Deposits


                                                                        Bougainville Copper Ltd, Papua New
                                                                        Guinea looking across the pit - 1986



                                                                      Porphyry Copper Deposits

                                                                      Most of the
                                                                        world’s
                 copper  is  extracted  from  a  type  of  mineral  deposit  called  a  “porphyry
                 copper”.  If  you’ve  seen  a  picture  of  a  great  big  open-pit  mining
                 operation odds  are  that  it  was  a  porphyry  copper  deposit.  Some  of  the
                 biggest  man-made  holes  in  the  ground  are  porphyry  copper  mines:
                 Bingham  Copper  Mine,  Utah,  and  Chuquicamata  in  Chile,  and  two  of  the
                 largest.

                 A porphyry is not a rock type, but rock with a particular texture. This porphyritic rock has large feldspar
                 crystals in a finer grained matrix.
                 Today a porphyry is, if it’s talked about at all, associated with large-scale mining. However, not all
                 porphyries are mineralised; it is a general term to describe an igneous rock that has some large-grained
                 crystals (“phenocrysts”) within a fine-grained matrix.

                 How Are Porphyry Copper Deposits Formed?
                 The magma, which cools to form porphyry copper deposits, is created when two tectonic plates collide.
                 One plate is forced under the other in what is called a subduction zone. The porphyry forms at depth
                 below an active volcano. The magma cools in two stages; at first slowly cooling to form the large crystals





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