Omai - Wernot Pit


Main commodities: Au
Our International
Study Tour Series
The last tour was
OzGold 2019
Our Global Perspective
Series books include:
Click Here
Super Porphyry Cu and Au

Click Here
IOCG Deposits - 70 papers
All available as eBOOKS
Remaining HARD COPIES on
sale. No hard copy book more than  AUD $44.00 (incl. GST)
Big discount all books !!!

The Omai gold deposit is one of the largest in South America.   It is located within Palaeoproterozoic rocks of the Guiana Shield in Guyana, 160 km SSW of Georgetown (#Location: 5 ° 26' 12"N, 58° 45' 45"W).

The Guiana Shield is the northern half of Amazon Craton, which was continuous with the West African Craton until the Atlantic Ocean opened about 115 Ma ago. The Amazon Craton has been divided into provinces based on age, structural, lithological and geophysical trends. The Proterozoic greenstone areas of Guyana are in the 2.2 Ga to 1.95 Ga Pastora-Amapa Province, and consist of metavolcanic and metasedimentary rocks. The greenstone belts of the province are the equivalents of the Birimian System in Africa.

The Omai deposit is hosted by the Palaeoproterozoic Barama-Mazaruni Supergroup (2.25 to 19.0 Ga) in the greenstone belt of the same name.   The supergroup is composed of alternating felsic, mafic and ultramafic volcanic flows interlayered with thick sedimentary units.   The base is dominated by tholeiitic basalts with assocaited mafic and ultramafic bodies and sills.   These are overlain by intermediate to felsic volcanics interlayered with immature clastic sediments.   There are also extensive syn- to late-tectonic calc-alkaline felsic to intermediate intrusions, ranging from granite to granodiorite, diorite, tonalite and adamellite.   One of these granites has been dated at 1945±45 Ma.

In the mine area the main hosts are mafic (massive to pillowed tholeiitic basalts) and intermediate (calc-alkaline andesites) volcanics, underlain by polygenic conglomerates (2 km thick sequence of poorly sorted cobble conglomerates with thin interlayered basalt flows) and overlain by finer grained sediments (siltstones, sandstones and greywackes).   The volcanics are cut by 2120±2 Ma quartz-feldspar porphyry and rhyolite dykes and by the 2094±6 Ma Omai granitoid (quartz-monzodiotire, granodiorite and diorite) stock, which is in turn cut by a variety of 2001±4 Ma mafic dykes and sills.

Both ductile and brittle shear zones are recognised and are broadly contemporaneous.   The former contain no mineralised veins, which are all developed within the competent rock of the mine area (eg. the Omai Stock, the porphyry and rhyolite dykes), although they may persist up to 10 m beyond the contact into the volcanics.

Six undeformed sub-vertical and sub-horizontal gold bearing vein sets have been delineated in two ore zones.   These represent a series of broadly contemporaneous crack and seal, laminated, brecciated and open space filling veins.   Veins range from a few mm's to 2 m in thickness and up to a maximum of 600 m in length, although the shallow veins may only be 10 m or less in extent.

The gangue is mainly quartz with subordinate carbonates, albite, sericite, chlorite, tourmaline, rutile and epidote, with a metallic paragenesis of Au-Ag-Te-W-Bi-Pb-Zn-Cu-Hg-Mo.   Wall rocks are altered to an assemblage including carbonates, sericite, silica, chlorite, albite, epidote, argillic minerals, pyrite and pyrrhotite.

The total mineable reserve at Omai (production+reserves) is ~130 tonnes of gold.

For detail consult the reference(s) listed below.

The most recent source geological information used to prepare this summary was dated: 1999.    
This description is a summary from published sources, the chief of which are listed below.
© Copyright Porter GeoConsultancy Pty Ltd.   Unauthorised copying, reproduction, storage or dissemination prohibited.


  References & Additional Information
   Selected References:
Voicu G, Bardoux M, Jebrak M, Crepeau R  1999 - Structural, mineralogical and geochemical studies of the Paleoproterozoic Omai gold deposit, Guyana: in    Econ. Geol.   v94 pp 1277-1304
Voicu G, Bardoux M, Stevenson R, Jebrak M  2000 - Nd and Sr isotope study of hydrothermal scheelite and host rocks at Omai, Guiana Shield: implications for ore fluid source and flow path during the formation of orogenic gold deposits: in    Mineralium Deposita   v35 pp 302-314

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 takes no responsibility what-so-ever for inaccurate or out of date data, information or interpretations.

Top | Search Again | PGC Home | Terms & Conditions

PGC Logo
Porter GeoConsultancy Pty Ltd
 International Study Tours
     Tour photo albums
 Ore deposit database
 Conferences & publications
PGC Publishing
 Our books  &  bookshop
     Iron oxide copper-gold series
     Super-porphyry series
     Porhyry & Hydrothermal Cu-Au
 Ore deposit literature
 What's new
 Site map