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A Preliminary Note on Quaternary Glaciation in Western Hupeh

✍ Scribed by C. LI; Y. S. WU

Book ID
114927603
Publisher
Wiley (Blackwell Publishing)
Year
2009
Tongue
Chinese
Weight
152 KB
Volume
20
Category
Article
ISSN
1000-9515

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## Abstract The West Siberian Plain was formed by marine deposits that extended from the Mediterranean basin to the arctic. Tectonic action later produced a striking series of long straight NE–SW grabens in the southern part of the plain. Pleistocene advance of the Kara ice sheet onto the continent