Geological structure of the Borokhudzir massif of the Central Dzungarian complex (South Dzungaria)
Authors:
Abstract
Widespread in the Dzungarian Alatau Hercynian granitoid intrusions are divided by many geologists into two complexes: the Central Dzungarian and the younger Lepsin, to which different metallogenic potential is attributed. 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 determinations of absolute age and diversity of material composition...
Область исследования:
(Archived) Without section
Funding:
None
References
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