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Showing posts with label Suture Zone. Show all posts
Showing posts with label Suture Zone. Show all posts

Thursday, April 28, 2011

Gold Producing Metallogenic Provinces and Epochs (MPE)

There are many metallogenic provinces and epochs (MPE) that can be traced through the formations of various rocks including those particular places and times when gold was deposited. There are at least eight of these episodes that can be found in the Appalachian Mountains of southern Québec. These MPE's can range all the way from the Grenville orogeny that occurred around 1.2 million years ago, and can be traced to different types of orogenies and mineralization to the end of the Permian era. 

A map of selected worldwide ore deposits of metals.
By KVDP


The different MPE's can be directly related to specific orogeny like the Grenvillian or any other orogenic event that has happened in the history of the world. An MPE can be found anywhere on the face of the earth. That means you had better know the geological history of the area where you are prospecting, and remember that some orogenic events left more gold behind them than others.

MPE's are usually associated with a suture zone where one tectonic plate has collided with another. In the case of an oceanic plate colliding with the continental plate the oceanic plate is subducted beneath the continental plate, and about 20 km inside account metal plate there should be a line of granitic intrusions.

The subduction zone acts as a giant heat engine melting the material that has been dragged downward by subduction causing it to become heated to the point the material is melted.  The subducted material is also saturated with water that lowers the melting point of the material, and supplies the water that at depths of kilometers beneath the surface of the earth becomes super heated water that is capable of dissolving many minerals that when they reach the right environment through the action of the superheated hydrothermal fluid are deposited as ore.

A subduction zone.
By A.J. Stern


Searching around in the area that has been intruded one is apt to find gold in the aura of contact metamorphism that is associated with the granitic intrusions. In this case gold is often associated with scheelite, an ore of tungsten in the form of tungsten carbonate. This occurrence is often found where the granite has intruded through an older layer of carbonate rocks such as limestone or dolomite where it forms a skarn..

On the oceanic side of the subduction zone are found many metal sulfide deposits where this whole deposits are usually found in small amounts, but there can also be some really huge deposits of sulfide that are formed this way. These are the result of sulfide deposits that are laid down by black smokers found on spreading centers located on the bottom of the ocean. These deposits are laid down very much like plums in a pudding at the scattered across the bottom of the ocean.

A black smoker at a spreading center at the bottom of the ocean. NOAA


As these deposits are carried away from the spreading center by the action of more magma being injected they cover the ocean bottom with spots where they are eventually subducted beneath a continental plate where they are often reactivated to form secondary mineral deposits sometimes in quantities large enough to form ore deposits.

MPE's are where ore deposits are typically found, and in many cases are considered to be the primary source of mineralization, and they eventually break down to form detrital mineral deposits.

Sunday, January 16, 2011

The Geologic Framework of a Gold Bearing Suture Zone: Part One

The estimated abundance of gold in the earth’s crust is 4x10-3 milligram per kilogram meaning this is the average amount of gold found in every kilogram found in the earth’s crust.  Although gold can be found virtually every place on earth the trick is to find it where it has been concentrated by geological processes to make it profitable to mine.  The necessary conditions are found in several places on earth that within reason have similar conditions that are called by several different names.  One of the most common names is “Gold Belt” another is “Gold Province.”  Names like these are used to define primary deposits of gold that have been deposited by the action of hot salt brines that are in excess of 100o C that deposit their dissolved gold either when its temperature drops below a certain point, or encounters conditions that cause the chemical precipitation of gold by reacting with other rocks.

A map showing modern tectonic plates.

Gold is also deposited when it has been eroded from the rock where it was primarily deposited as detritus in the beds of streams or a similar environment.  In this form gold is called “Placer or alluvial gold.”  Aside from being found in stream sediments it can also be found in sandstone or conglomerate that are really nothing other then fossilized sedimentary deposits.  The largest known deposit of gold is in one of these fossilized conglomerate deposits, the Witwatersrand in South Africa.  The mines here are the deepest on earth some of them are in excess of 13,000 feet deep.

Tectonic Plate boundaries.

Primary gold deposits accompanied by placer deposits are found mainly in suture zones where one tectonic plate collides with another.  In some cases the oceanic plate is subducted beneath a continent with little affect.  In other cases two continental land masses collide throwing up ranges of great mountains.  There are several examples of this on earth today.  The grand daddy of all mountain ranges caused by such a collision is the Himalayas caused by the collision of two continents, the Asian and the Indian plates.  Between these plates there used to be an ocean called the Tethys Sea that vanished when the collision occurred.  Other examples of similar mountain ranges can be found all over the face of the earth, some of the more recent are: the Appalachians, the Alps, the Andes, the Rockies to name a few of many.

A suture zone is depicted in this series of charts.

Because of the nature of this subject it will require several separate articles to treat it as it should be.  The next article in this series will explain how mineral deposits are emplaced in a suture zone including gold.