Cretaceous-Tertiary shortening, basin development, and volcanism in central Tibet
The geologic map pattern of the Qiangtang terrane in central Tibet defines a >600-km-long and up to 270-km-wide east-plunging structural culmination. It is characterized by early Mesozoic blueschist-bearing mélange and upper Paleozoic strata in the core
|Collections||ANU Research Publications|
|Source:||Geological Society of America Bulletin|
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