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Kolar Gold Field
India
Main commodities: Au


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The Kolar Gold Field lies within a schist belt of the Archaean Dharwar Craton in Karnataka State, southern India (#Location; 12° 57' 31"N, 78° 15' 57"E).

The Kolar Schist Belt occuppies a north-south elongated area some 80 km long and 2 to 4 km in width in the eastern block of the Dharwar Craton.   It encloses an Archaean succession of volcanic dominated rocks composed mainly of 2.7 Ma mafic (komatiitic and lesser tholeiitic) metavolcanics, now represented by amphibolites.   A well foliated felsic unit is found along the eastern part of the belt with local xenoliths of granitoids, amphibolites and banded iron formation.   Banded iron formations are the only recognisable sedimentary components of the belt, and form prominent ridges within the schist belt, interbanded with amphibolites, and graphitic and sulphidic schists.

The belt is enclosed on both sides by foliated and sheared granitoids with tectonic contacts.   On the western side monzodioritic to granitic intrusives are 2630 to 2550 Ma in age, although some 3100 Ma granitic crust is also indicated.   The eastern granitoids are 2530 Ma granodioritic gneisses.

Two types of gold deposit are recognised in the Kolar gold field,  i). Gold-quartz-sulphide lodes, and  ii). gold quartz-calcite vein systems.   These deposit types are associated with all of the rock types in the schist belt.   The latter accounted for 90% of the gold production of the field.

Lodes are generally disposed parallel to the north-south trending foliation of the amphibolites and are localised within the fine grained schistose varieties of the amphibolites.

The quartz lodes, the best example of which is the 10 km long Champion reef, which comprises parallel and en echelon veins of quartz within sheared, schistose amphibolites.   The lode zones and individual veins pinch and swell both along strike and down dip and have gradational margins with the enclosing country rocks.   These reefs are typically around 2 m thick except where thickened by folding.

The sulphide lodes, the best example of which is the 2 km long and 1.6 m wide Oriental lode, which consist of alternating bands and layers of quartz, sulphides and silicates which have sharp contacts with the enclosing amphibolites and are associated with magnetite bearing ironstone and argillaceous sulphidic rocks.

The Kolar gold field has been systematically worked for over 200 years and has produced around 700 t of gold.

For detail see the reference(s) listed below.

The most recent source geological information used to prepare this decription was dated: 1988.    
This description is a summary from published sources, the chief of which are listed below.
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Kolar Gold Field

  References & Additional Information
   Selected References:
Mishra B, Panigrahi M K  1999 - Fluid evolution in the Kolar Gold Field: evidence from fluid inclusion studies : in    Mineralium Deposita   v34 pp 173-181
Siddaiah N S, Hanson G N, Rajamani V  1994 - Rare earth element evidence for syngenetic origin of an Archean stratiform Gold Sulfide deposit, Kolar Schist belt, South India: in    Econ. Geol.   v89 pp 1152-1566
Siddaiah N S, Rajamani V  1989 - The geologic setting, mineralogy, geochemistry, and genesis of Gold deposits of the Archean Kolar Schist Belt, India: in    Econ. Geol.   v84 pp 2155-2172


Porter GeoConsultancy Pty Ltd (PorterGeo) provides access to this database at no charge.   It is largely based on scientific papers and reports in the public domain, and was current when the sources consulted were published.   While PorterGeo endeavour to ensure the information was accurate at the time of compilation and subsequent updating, PorterGeo, its employees and servants:   i). do not warrant, or make any representation regarding the use, or results of the use of the information contained herein as to its correctness, accuracy, currency, or otherwise; and   ii). expressly disclaim all liability or responsibility to any person using the information or conclusions contained herein.

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