Geological structure of the Borokhudzir massif of the Central Dzungarian complex (South Dzungaria)
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Abstract
Widespread in the Dzungarian Alatau Hercynian granitoid intrusions many geologists divide into two complexes: Central Dzungarian and younger Lepsin, which are attributed different metalliferousness. However, the attribution of specific massifs to one or another complex in many cases causes discussion and remains unresolved due to the lack of clear age boundaries for most of the large massifs, ambiguity of definitions of absolute age and diversity of material composition...
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References
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