Deposit types/Gold

Orogenic gold (low-sulphide gold-quartz veins)

Gold in large, long quartz veins cutting metamorphosed volcanic and sedimentary rocks.

What it is

Gold in large, long quartz veins cutting metamorphosed volcanic and sedimentary rocks.1

How it forms

Compression builds faults and joints in mountain belts. Quartz veins fill them with a little pyrite and other sulphides and native gold.1

Host rocks

Greenstone belts and oceanic metasediments (volcanic rocks, greywacke, chert, shale) with late granites.1

Where it forms

Fault and joint systems formed by regional compression in continental-margin mobile belts and accreted terranes.1

How old

Precambrian to Tertiary1

Mines of this type

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Sources

  1. Mineral Deposit Models (Bulletin 1693, Cox and Singer, eds., 1986) US Geological Survey

From the Prospector Trails mining history dataset: each fact links to the source it was checked against. Figures are as the source gives them, in the money of their day. Not investment advice.

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Cover photos from Wikimedia Commons: Super Pit, Kalgoorlie by Kgbo, CC BY-SA 4.0. Pictures: Gold prospectors constructing a long box with a filter for panning gold. Process print after H.M. Paget, 1899., Henry Marriott Paget (Public Domain Mark 1.0); Kimberley, South Africa: miners and washing gear at the Bultfontein diamond mine. Woodburytype, 1888, after a photograph by Robert Harris., Harris, Robert, active 1881-1888. (Public Domain Mark 1.0); San Francisco, California: the Golden Gate bay area. Photograph, ca. 1880., Unknown (Wellcome Collection) (Public Domain Mark 1.0).