| 词条 | Kunlun Fault |
| 释义 |
The Kunlun fault is a strike-slip fault to the north side of Tibet. Slippage along the {{convert|1500|km}} long fault has occurred at a constant rate for the last 40,000 years. This has resulted in a cumulative offset of more than {{convert|400|m}}.[1] The fault is seismically active, most recently causing the magnitude 7.8 2001 Kunlun earthquake.[2] References1. ^{{cite web | title = The Kunlun Fault | url = http://earthobservatory.nasa.gov/IOTD/view.php?id=871 | work = Earth Observatory | publisher = NASA | date = 2000-10-10 | accessdate = 2010-04-15}} {{-}}{{regional-geology-stub}}2. ^{{cite journal|last=Klinger|first=Y. |author2=Xu X. |author3=Taponnier P. |author4=Vand der Woierd J. |author5=Lasserre C. |author6=King G. |year=2005|title=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|journal=Bulletin of the Seismological Society of America|volume=95|issue=5|pages=1970–1987|doi=10.1785/0120040233|url=https://www.academia.edu/16922094/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|accessdate=15 June 2010|bibcode = 2005BuSSA..95.1970K }} 7 : Seismic faults of Asia|Strike-slip faults|Geology of Tibet|Geology of China|Kunlun Mountains|Tibetan Plateau|Supershear earthquakes |
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