Focal depth research of earthquakes in Mainland China: Implication for tectonics |
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Authors: | Guomin Zhang Suyun Wang Li Li Xiaodong Zhang Hongsheng Ma |
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Institution: | (1) Center for Analysis and Prediction, China Seismological Bureau, 100036 Beijing, China;(2) Geophysics Institute, China Seismological Bureau, 100081 Beijing, China |
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Abstract: | Focal depth data of earthquakes in Mainland China are processed and analyzed in this paper, as well as the relationship between
the focal depths and large-scale tectonic structures. As a basic parameter for earthquakes, focal depth is used to investigate
deep environment of seismogenic regions, tectonic backgrounds for concentration and release of seismic energy, the inner crustal
deformation and its mechanic features. Depth data of 31282 Ml⩾2.0 events with 1st class and 2nd class precision in Mainland China from Jan. 1, 1970 to May 31, 2000 are used to get spatial
features of earthquakes distributed with depth and to provide average depth for each grid area throughout China. Researches
show that the average depth (D) for all the earthquakes used in this paper is (16 ± 7) km, and (13 ± 6) km and (18 ± 8) km for the events in eastern China
and western China, respectively. The area with the deepest focal depth is located in southwest Xinjiang region, near the western
and southwestern ends of the Tarim Basin. The focal depth related to large-scale tectonic structures, for instance, D= (33
± 12), (21 ± 10), (14 ± 7), (11 ± 5) and (10±4) km in Tibet plateau block, Xinjiang block, North China, Northeastern China
and South China, respectively. The earth-quakes are deeper at the bounders of the integrated tectonic blocks, including the
southwestern and northern brims of the Tarim Basin, southern brim of the Zhunge’r Basin and that of the Alashan block, as
well as the eastern and western sides of the Edos block and the western brim of the Sichuan Basin. The earthquakes at the
newly ruptured belts are relatively shallower, for instance, at the southwestern Yunnan seismic belt and the Zhangjiakou-Bohai
seismic belt. The mechanic behavior, deformation and features for the crust and mantle structures are also discussed. |
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Keywords: | Mainland China focal depth |
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