The Role of Allochtonous Terranes in Construction and Evolution of the Pacific Continental Margins (For North USSR)
 
    
    - Organization:
- The Australasian Institute of Mining and Metallurgy
- Pages:
- 4
- File Size:
- 383 KB
- Publication Date:
- Jan 1, 1987
Abstract
New geological and geophysical in vestigation including our detailed  field observation in different regions  of the Koryak upland testify that Nor- theastern Eurasia margin eastward of  the Ochotsk-Chukotka belt is composed  of a collage of allochtonous terranes arcs and sedimentary filling of back- arc basins, which bordered North East  Siberia and Chukotka (1)1). Ancient island are assemblages  are the most tipical for this region  (2-4; shown by heavy line). They are  marked by long (500-1000 km) volcanic  belts which become younger towards the  Pacific up the Latest Jurassic-Neocomi- an (2) to Late Cretaceous (3) and Pale- Gene (4).
Citation
APA: (1987) The Role of Allochtonous Terranes in Construction and Evolution of the Pacific Continental Margins (For North USSR)
MLA: The Role of Allochtonous Terranes in Construction and Evolution of the Pacific Continental Margins (For North USSR). The Australasian Institute of Mining and Metallurgy, 1987.
