Active present faults of the Western segment of the Qilian Mountains (Northern Tiber)
https://doi.org/10.33623/0579-9406-2020-2-9-17
Abstract
The Qilian Mountains, as the northeastern margin of the Tibetan Plateau, absorbed the crustal shortening and accommodated the left-lateral displacement of the Altun Tagh fault. Detailed geomorphologic study of river valleys on the northern margin of the Qilian Mountains showed that since the late Pleistocene the crustal uplift rate of the northern Qilian Mountains has been greater than the central part. Due to the extension of the Tibetan plateau between the Changma fault and the Yumen fault the latest belt of faults and folds was formed on the northern margin of the Qilian Mountains. The study of the height of river terraces over the past 60 thousand years shows that the rate of vertical displacement along the Changma fault is 0,31±0,06 mm/a and its horizontal crustal shortening rate is 0,11±0,02 mm/a. The rate of vertical displacement along the northernmost Yumen fault is 0,33±0,02 mm/a and its horizontal crustal shortening rate is 0,53±0,03 mm/a. Active faults in the western segment of the northern Qilian Mountains account for 12% of the total crustal shortening in the Qilian Mountains. In addition, the crustal shortening rate of faults in the northern Qilian Mountains is much greater than the crustal shortening rate of faults inside the Qilian Mountains, which further indicates that since the Late Pleistocene the crustal uplift rate of the northern Qilian Mountains has been greater than the central Qilian Mountains.
About the Authors
Chen Zhidan
Московский государственный университет имени М.В. Ломоносова
Russian Federation
Russian Federation
N. V. Koronovsky
Московский государственный университет имени М.В. Ломоносова
Russian Federation
Russian Federation
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Review
For citations:
Zhidan Ch., Koronovsky N.V. Active present faults of the Western segment of the Qilian Mountains (Northern Tiber). Moscow University Bulletin. Series 4. Geology. 2020;(2):9-17. (In Russ.) https://doi.org/10.33623/0579-9406-2020-2-9-17
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