Analysis of Crustal Movement and Deformation in Mainland China Based on CMONOC Baseline Time Series

• Published in: Remote sensing (Basel, Switzerland) Vol. 13; no. 13; p. 2481
• Main Authors: Wu, Jicang, Song, Xinyou, Wu, Weiwei, Meng, Guojie, Ren, Yingying
• Format: Journal Article
• Language: English
• Published: Basel MDPI AG 25.06.2021
• Subjects: basins; China; CMONOC; Compression; crustal deformation; Data processing; Deformation; Earthquakes; Faults; Geology; GPS; linear strain rate; Remote sensing; Rigid blocks; Satellite observation; Seismic activity; shrinkage; Software; Tectonics; Time series; time series analysis; Trends; Central Asia; China
• DOI: 10.3390/rs13132481
• ISSN: 2072-4292

In this paper, we propose a method for the analysis of tectonic movement and crustal deformation by using GNSS baseline length change rates or baseline linear strain rates. The method is applied to daily coordinate solutions of continuous GNSS stations of the Crustal Movement Observation Network of China (CMONOC). The results show that: (a) The baseline linear strain rates are uneven in space, which is prominent in the Tianshan, Sichuan-Yunnan, Qinghai-Tibet Plateau, and Yanjing areas, with a maximum value of 1 × 10−7 a−1, and about two orders smaller in the South China block, the Northeast block, and the inner area of the Tarim basin, where the average baseline linear strain rates are 1.471 × 10−9 a−1, 2.242 × 10−9 a−1, and 3.056 × 10−9 a−1, respectively; (b) Active crustal deformation and strong earthquakes in the Xinjiang area are mainly located in the north and south sides of the Tianshan block; the compression deformations both inside the Tarim block and in the southern Tianshan fault zone are all increasing from east to west, and the Tarim block is not a completely “rigid block”, with the shrinkage rate in the west part at about 1~2 mm/a; (c) The principal directions of crustal deformation in the Xinjiang, Tibet, and Sichuan-Yunnan regions are generally in the north—south compression and east—west extension, indicating that the collision and wedging between the Indian and Eurasian plates are still the main source of tectonic movements in mainland China.