Glacier changes in the Karlik Shan, eastern Tien Shan, during 1971/72–2001/02
نویسندگان
چکیده
منابع مشابه
Structural framework of a major intracontinental orogenic termination zone: the easternmost
The Barkol Tagh and Karlik Tagh ranges of the easternmost Tien Shan are a natural laboratory for studying the fault architecture of an active termination zone of a major intracontinental mountain range. Barkol and Karlik Tagh and lesser ranges to the north are bounded by active thrust faults that locally deform Quaternary sediments. Major thrusts in Karlik Tagh connect along strike to the east ...
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Late Quaternary slip rates across the central Tien Shan, Kyrgyzstan, central Asia
[1] Slip rates across active faults and folds show that late Quaternary faulting is distributed across the central Tien Shan, not concentrated at its margins. Nearly every intermontane basin contains Neogene and Quaternary syntectonic strata deformed by Holocene north-south shortening on thrust or reverse faults. In a region that spans two thirds of the north-south width of the central Tien Sha...
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ژورنال
عنوان ژورنال: Annals of Glaciology
سال: 2009
ISSN: 0260-3055,1727-5644
DOI: 10.3189/172756410790595877