Geological Characteristics and Metallogenic Model of Super-Large Kounrad Porphyry Copper oft-com:office:smarttags" />
The Kounrad porphyry copper deposit was discovered 70 years ago in the Balkhash Metallogenic Belt of the Central Asian Metallogenic Domain. It is a typical super-large porphyry copper deposit developed under the tectonic environment of continental margin arc, with a metallogenic model of granodiorite. It is suggested that the metallogenesis of the deposit was controlled by the circular structure, and had a very close relation with the secondary quartzite and argillic alteration.oft-com:office:office" />