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Details for article 5 of 14 found articles
| Title: |
Geologic structure of the South Okhotsk basin near Sakhalin |
| Author: |
Vasil'yev, B. I. Tuyezov, I. K. Yegorova, M. G. Podzorova, D. I. |
| Appeared in: |
International geology review |
| Paging: | Volume 19 (1977) nr. 1 pages 1-10 |
| Year: |
1977-01 |
| Contents: |
The region consists mainly of Neogene tuffogenic-sedimentary rocks overlainlocally by a well-developed cover of Quaternary deposits. In a number of places,older rocks crop out among the Neogene deposits. On the basis of the structuralfeatures of the rocks, their composition, and the presence of a large numberof fossil invertebrate burrows, including decapod medium-tailed crayfish, weconclude that the Neogene marine basin was shallow. Formation of the deep-waterSouth Okhotsk basin began at the end of the Pliocene and proceeded mainlyduring Quaternary time. The slope of the basin has a fundamentally similarstructure to that of the shelf. —Authors. |
| Publisher: |
Taylor & Francis |
| Source file: |
Elektronische Wetenschappelijke Tijdschriften |
Details for article 5 of 14 found articles
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