Conditions of the formation of hypabyssal granitoid intrusions using the example of the Sizindzha Massif, the Okhotsk-Chukotka volcanic belt

@article{Mishin2013ConditionsOT,
  title={Conditions of the formation of hypabyssal granitoid intrusions using the example of the Sizindzha Massif, the Okhotsk-Chukotka volcanic belt},
  author={L. F. Mishin},
  journal={Russian Journal of Pacific Geology},
  year={2013},
  volume={7},
  pages={16-25}
}
The Sizindzha hypabyssal intrusive massif located in the Kuidusun volcanic zone of the Okhotsk-Chukotka volcanic belt has been mapped and studied in detail. The complex of textural-petrographic features indicates the in situ formation of granitoids by the successive replacement of the host sedimentary rocks of the Verkhoyansk Complex and the medium-grained diorites (more rarely, gabbro) by later granites. It was established that the oldest fine-grained intermediate rocks observed as xenoliths… CONTINUE READING

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