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- W3132160111 abstract "To explore the tectonic relationship between the faults within the Eastern Kunlun Shan and Qaidam basin as well as the potential difference between the nature of the basement of the Eastern Kunlun Shan and the Qaidam basin, we investigate the characteristics (e.g. distribution, magnitude, occurrence depth) of earthquakes in the northern Tibetan plateau. Our result suggests that the nature of basement along the margins of the Qaidam basin is relatively similar to that of in the surrounding mountain belts, whereas at the center of the basin, the nature of basement of the Qaidam basin could be different from that of beneath the margins of the basin as well as in the surrounding mountain belts. This highlights that the upper crustal deformation in the northern Tibetan plateau could be more likely accommodated by the faults along the margins of the Qaidam basin and the fault systems in the surrounding mountain belts." @default.
- W3132160111 created "2021-03-01" @default.
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- W3132160111 date "2020-09-26" @default.
- W3132160111 modified "2023-09-27" @default.
- W3132160111 title "Tectonic Difference between the Qaidam Basin and the Eastern Kunlun Shan: Insight from Buffer Analysis of the Earthquakes and Faults in the North Tibet" @default.
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- W3132160111 doi "https://doi.org/10.1109/igarss39084.2020.9324070" @default.
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