PorterGeo
SEARCH  GO BACK  SUMMARY  REFERENCES
Chekmar

Kazakhstan

Main commodities: Cu Zn Pb Ag
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 Chekmar volcanic hosted sulphide deposit is located 46 km to the north-east of Leninogorsk, in Kazakhstan. It is another of the deposits of the Rudny Altay district, and is associated with middle Devonian volcanics.

The host sequence is the 230 m thick Uspensk Suite which comprises, from the base,
i). spheroidal rhyolitic lava and lava-breccia;  ii). a 'spotted' unit of abundant tuffs and acid lava;  iii). a 'tuff-sediment' unit of irregularly alternating layers of tuffaceous sandstone, tuffaceous siltstone and other tuffaceous sediments.

The Uspensk Suite is overlain by the 250 m thick "Upper Suite" which is largely composed of felsic tuffs and rhyolitic flows with felsitic textures (Balychev, 1990).

Wallrock alteration comprises chlorite-sericite-quartz and silicification. The major structural feature in the deposit vicinity is an anticline with steep, 70 to 90° flanks. The main ore is present as stringer-impregnations, occurring as veins, rare disseminations and massive sulphide lenses.

The ore is composed of 10% Cu-Zn, 45% Pb-Zn and 45% polymetallic ore (Balychev, 1990). Chekmar is one of the "large" deposits of the Leninogorsk district.

The lower half of the orebody appears to be concentrated in the 'tuff-sediment' unit of the Uspensk Suite, where the alteration is predominantly chlorite-sericite-quartz, occasionally including the uppermost sections of the underlying 'spotted' unit. The upper section is hosted by silicified alteration in the basal sections of the Upper Suite felsic tuffs (Balychev, 1990).

The most recent source geological information used to prepare this summary was dated: 1996.    
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

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
 Experience
PGC Publishing
 Our books  &  bookshop
     Iron oxide copper-gold series
     Super-porphyry series
     Porhyry & Hydrothermal Cu-Au
 Ore deposit literature
 
 Contact  
 What's new
 Site map
 FacebookLinkedin