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Characteristic Features of the Volcanism of the Siberian Platform
File | Size | Format | ||
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vol17n4-452-457.pdf | 3.23 MB | Adobe PDF | View/Open |
Item Summary
dc.contributor.author | Sobolev, V.S. | |
dc.date.accessioned | 2009-01-26T05:39:54Z | |
dc.date.available | 2009-01-26T05:39:54Z | |
dc.date.issued | 1963-10 | |
dc.identifier.citation | Sobolev VS. 1963. Characteristic features of the volcanism of the Siberian platform. Pac Sci 17(4): 452-457. | |
dc.identifier.issn | 0030-8870 | |
dc.identifier.uri | http://hdl.handle.net/10125/4950 | |
dc.description.abstract | Widespead volcanism is characteristic of the Siberian platform, and was especially intense during uppermost Paleozoic and lower Mesozoic time. The Siberian traps, which occupy an area of more than 1,500,000 km^2, are best developed there. These are effusive and hypabyssal rocks of basalt-dolerite type, closely resembling trap rocks in other parts of the globe, especially the Karroo dolerires of South Africa. | |
dc.language.iso | en-US | |
dc.publisher | University of Hawai'i Press | |
dc.title | Characteristic Features of the Volcanism of the Siberian Platform | |
dc.type | Article | |
dc.type.dcmi | Text | |
Appears in Collections: |
Pacific Science Volume 17, Number 4, 1963 |
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