et al.
The southern Koryak Upland located north and northwest of the Olyutor zone composed of Upper Cre-taceous siliceous–volcanogenic sequences (Bogdanov et al., 1987) hosts the Ukelayat trough (Central Koryak structural-facies zone) (Ermakov and Suprunenko, 1975). The trough is filled with highly deforme...
| Other Authors: | |
|---|---|
| Format: | Text |
| Language: | English |
| Published: |
|
| Subjects: | |
| Online Access: | http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.616.4720 http://earth.geology.yale.edu/~brandon/Eprints/Shapiro_etal2001_KamchatkaZirconFT.pdf |
| Summary: | The southern Koryak Upland located north and northwest of the Olyutor zone composed of Upper Cre-taceous siliceous–volcanogenic sequences (Bogdanov et al., 1987) hosts the Ukelayat trough (Central Koryak structural-facies zone) (Ermakov and Suprunenko, 1975). The trough is filled with highly deformed Upper Cretaceous and Lower Paleogene sandy–shaly sequences frequently of the flyschlike appearance (Ermakov |
|---|