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Thrusting on the Tibetan plateau within the last 5 MaThe Lunpola basin, in the middle of the Tibetan plateau, contains about 4 km of nonmarine sediments deposited since early Cenozoic times. This remarkable structure, localized in the Bangong-Nujiang suture zone, has much to teach about how the plateau has developed. The strong evidence for young compression in the basin is emphasized.
Document ID
19890057881
Acquisition Source
Legacy CDMS
Document Type
Conference Proceedings
Authors
Burke, Kevin (Lunar and Planetary Inst. Houston, TX, United States)
Lucas, Lynette (Lunar and Planetary Institute; Houston, University TX, United States)
Date Acquired
August 14, 2013
Publication Date
January 1, 1989
Subject Category
Geophysics
Accession Number
89A45252
Funding Number(s)
CONTRACT_GRANT: NAG5-585
CONTRACT_GRANT: NASW-4066
Distribution Limits
Public
Copyright
Other

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