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Author content All content in this area was uploaded by Xuanhua Chen. Sketch map of the multi-core metallogenic system and distribution of porphyry CueMo deposits in the Central Asian metallogenic domain. The fault system is modified from Ren et al. The distribution of porphyry CueMo deposits is modified from Li et al. Regional geological sketch map of the western Balkhash metallogenic belt 1-Quaternary System; 2-Permian System; 3-CarboniferousePermian System undivided ; 4-Carboniferous System; 5-Devonian System; 6-Silurian System; 7-Precambrian System; 8-Triassic granitoids; 9-Permian granitoids; Carboniferous granitoids; Devonian granitoids; Ordovician granitoids; Precambrian granitoids; 14the Balkhash Lake area; thrust fault; dextral strike-slip fault; fault; locations of deposits studied in this paper.

Blank background of the whole procedure of analyses. A quartz vein from the East Kounrad WeMo deposit. Content uploaded by Xuanhua Chen. Author content All content in this area was uploaded by Xuanhua Chen on Apr 11, Re e Os geochronology of Cu and W e Mo deposits in the. Laboratory of Geological F ormations, K. Av ailable online 8 October Re e Os geochronology;. Porphyry Cu e Mo deposit;. Greisen W e Mo deposits;. The Balkhash metallogenic belt in Kazakhstan, in which.

Re e Os compositional analyses a nd Re e Os isotopic dating. Moly bdenites from the Borly porphy ry Cu. W e Mo deposits , and lower common Os contents 0. The molybdenites from the Borly porphyry Cu e Mo deposit. Institute of Geomechanics, Chinese Academy. Production and hosting by Elsevier B. Peer-review under responsibility of China Uni versity of Geosciences. Geoscience Frontiers 1 , e Re e Os dating of the molybdenites indicates that Cu e W e Mo. The Re e Os model and isochron ag es thus suggest.

Compared to the Junggar-East Tianshan porphyry Cu metallogenic belt in northwestern. China, the formation of the Cu e Mo metallogenesis in the Balkhash metallogenic belt occurred between.

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Production and hostin g by. The Balkh ash metal logenic be lt lies at t he inner m argin of t he. U-shaped Kaza khstan e T ianshan o rocline and th e core of the. Balkhash e Ju nggar oroge nic belt of the Ce ntral Asian meta llogenic. It is the main porphy ry copper. Aktogay Cu e M o deposit and the lar ge skarn Sayak Cu-p olymetall ic. Furth ermore, ther e are also porphy ry Borly. Molybdenite can provide information critical to understanding. Re e Os isotopic dating of molybdenites is. Based on the Re e Os dating of. East Tianshan porphyry Cu metallogenic belts in China. Geology of the Balkhash metallogenic belt in the.

The Central Asia n metalloge nic domain begi ns in the west in the. Ural Mountain s on the Euro-Asia bou ndary , and extends ea stwards. Qinghai, nor thern Gansu, western Inne r Mongolia, an d western. Mongolia to th e southern Sib eria region. In the latter area , it also. Asia Chen et al. Multi-stage and mu lti-type zone s of.

Geological ly, this domain ha s experienced the format ion of conti-. T he Central Asia n metallogenic d omain is world. He and Zhu, ; Z hu et al. The mineralizat ions of. The main body of the Central Asian metallogenic domain is the. Tsagaan Suvarga and Ouyu T olgoi in Mongolia; the. The Balkhash metallogenic belt is one of the cores of the. Central Asian metallogenic domain Zhu et al.

Devonian and Carboniferous e Permian volcano-magmatic arcs in. This metallogenic belt consists of. The former begins at the. Mointy block in the west, and extends eastwards via Aktogay to. Baotugu, western Junggar, Xinjiang, China. It is about km. The Borly porphyry Cu deposit and the quartz vein-. The Borly porphyry Cu deposit is situated in the Prioziorny district,. Dzhezkazgan Province, 60 km north of Balkhash City, and 45 km. It lies mainly in the southern. Mo ratio Z These include 1 a suite of lithic-crystal tuff, lava, and subvolcanic.

The Borlinskaya apophysis contains three petrofa-. These petrofacies are cut by a granodiorite.

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The intrusion of that rock. The youngest magmatic assemblage is the alkaline granite-. Zhaksitagalinsky complex Abdulin et al. The Akshatau W e Mo deposit. The Akshatau large-scale quartz vein-greisen W e Mo deposit. It is a disseminated quartz vein-greisen. As part of the Permian Akshatau metallogenic province, the. It occurs within Permian leucogranites of the Akshatau. The ore -forming process has mainly under-. The East Kounrad W e Mo deposit. The East Kounrad W e Mo deposit lies about 11 km east of the.

It is an underground-mined post-. It has reserves of e kt of Mo, with a grade of 0. The W e Mo mineralizations.