崑崙地震
崑崙断層(英語版)はユーラシアプレートに関係するチベット高原の東側の移動に適合する主要な左側の断層構造の一つである。この移動はインドプレートとユーラシアプレートの間の衝突に関連する不明瞭な地殻地帯の横向きの拡大による。
1 2 Li Li; Chen Yong (2002). “Preliminary report on the Ms 8.1 Kokoxili (Qinghai, China) earthquake of 14 November 2001”. Episodes 25 (2): 95–99. doi:10.18814/epiiugs/2002/v25i2/005.
↑ Klinger,Y.; Xu,X.; Tapponnier,P.; Van der Woerd,J.; Lasserre,C.; Geoffrey King,G. (2005). “High-Resolution Satellite Imagery Mapping of the Surface Rupture and Slip Distribution of the Mw _7.8, 14 November 2001 Kokoxili Earthquake, Kunlun Fault, Northern Tibet, China”. Bulletin of the Seismological Society of America 95 (5): 1970–1987. Bibcode: 2005BuSSA..95.1970K. doi:10.1785/0120040233. https://www.researchgate.net/publication/244485209.
1 2 Van Der Woerd J.; Meriaux, A.S.; Klinger, Y.; Ryerson, F.J.; Gaudemer, Y.; Tapponnier, P. (2002).
“The 14 November 2001, Mw 7.8 Kokoxili earthquake in northern Tibet (Qinghai Province, China)”. Seismological Research Letters 73 (2): 125–135. doi:10.1785/gssrl.73.2.125. http://eost.unistra.fr/fileadmin/upload/EOST/Jeromevdw/publications/vdWoerd_et_al._SRL2002.pdf.
↑ Liu, J. G.; Haselwimmer, C. E. (2006). “Co‐seismic ruptures found up to 60 km south of the Kunlun fault after 14 November 2001, Ms 8.1, Kokoxili earthquake using Landsat‐7 ETM+ imagery”. International Journal of Remote Sensing 27 (20): 4461–4470. doi:10.1080/01431160600784283.
↑ Fu B.; Lin A. (2003). “Spatial distribution of the surface rupture zone associated with the 2001 Ms 8.1 Central Kunlun earthquake, northern Tibet, revealed by satellite remote sensing data”.