The 2002 Denali fault and 2001 Kunlun fault earthquakes: Complex rupture processes of two large strike-slip events

2004-12-01
We studied the source processes of two large continental earthquakes, the 3 November 2002 Denali fault earthquake and the 14 November 2001 Kunlun fault earthquake, associated with strike-slip faulting along ancient sutures. We inverted teleseismic P waveforms using a pulse-stripping method for multiple time windows with different focal mechanisms and derived composite source models. According to our results, the 2002 Denali fault earthquake began with initial thrusting (M-W 7.3) along a 40-km-long segment of the north-northwest-dipping Susitna Glacier fault and later ruptured a 300-km-lon-c-, segment along the Denali and Totschunda faults with a right-lateral strike-slip mechanism (M-W 7.7). In contrast, the 2001 Kunlun fault earthquake nucleated near an extensional step-over with a subevent pair consisting of 30-km-long strike-slip (M-W 6.9) event and 40-km-long normal (M-W 6.8) faulting event and later ruptured a 350-km-long seament along the Kunlun fault with a left-lateral strike-slip mechanism (M-W 7.7). Both earthquakes propagated primarily unilaterally to the east and released most of their energy along slip patches (asperities) far from the hypocenter locations. We find that both the Denali fault and Kunlun fault earthquakes had high-average rupture velocities of 3.2 km/sec and 3.4 km/sec. respectively. We also compared the Source properties of these two earthquakes with other strike-slip earthquakes. For scaling purposes, large strike-slip earthquakes were classified as interplate, oceanic intraplate, or continental intraplate events. By using this classification the Denali fault and Kunlun fault earthquakes have an Interplate signature that suggests overall weak faulting.
BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA

Suggestions

The Chios, Greece Earthquake of 23 July 1949: Seismological Reassessment and Tsunami Investigations
Melis, Nikolaos S.; Okal, Emile A.; Synolakis, Costas E.; Kalogeras, Ioannis S.; Kanoğlu, Utku (Springer Science and Business Media LLC, 2020-03-01)
We present a modern seismological reassessment of the Chios earthquake of 23 July 1949, one of the largest in the Central Aegean Sea. We relocate the event to the basin separating Chios and Lesvos, and confirm a normal faulting mechanism generally comparable to that of the recent Lesvos earthquake located at the Northern end of that basin. The seismic moment obtained from mantle surface waves, M-0=7x10(26) dyn cm, makes it second only to the 1956 Amorgos earthquake. We compile all available macroseismic dat...
A critical examination of near-field accelerograms from the sea of Marmara region earthquakes
Akkar, S; Gulkan, P (Seismological Society of America (SSA), 2002-02-01)
In 1999, Turkey was struck by two major earthquakes that occurred 86 days apart on the North Anatolian Fault system. Both earthquakes had right-lateral strike-slip mechanisms with moment magnitudes greater than 7. The number of strong-motion records obtained from the Kocaeli earthquake (17 August 1999, M-w 7.4) was 34. The second event, designated as the Bolu-Duzce earthquake (12 November 1999, M-w 7.2), triggered 20 instruments. Among the records that we have from these earthquakes, seven are from near-sou...
The 20th July 2017 Bodrum-Kos Tsunami Field Survey
Dogan, Gozde Guney; Annunziato, Alessandro; Papadopoulos, Gerassimos A.; GÜLER, HASAN GÖKHAN; Yalçıner, Ahmet Cevdet; Cakir, Tarik Eray; Sozdinler, Ceren Ozer; ULUTAŞ, ERGİN; Arikawa, Taro; Süzen, Mehmet Lütfi; Guler, Isikhan; Probst, Pamela; Kanoğlu, Utku; Synolakis, Costas (Springer Science and Business Media LLC, 2019-07-01)
The July 20, 2017 Bodrum-Kos Earthquake caused tsunami wave motions and damage in the south of Bodrum Peninsula, Turkey, and on Kos Island, Greece. Immediately after the earthquake, we conducted several post-tsunami field surveys including interviews in coastal zones impacted by the tsunami, i.e., the coastlines of Bodrum Peninsula, Karaada Islet and Akyaka Town in Gokova Bay, Turkey, and eastern Kos Island, Greece. We present observations and measurements to document the variation of the tsunami effects al...
The generating mechanisms of the August 17, 1999 Izmit bay (Turkey) tsunami: Regional (tectonic) and local (mass instabilities) causes
Tinti, S; Armigliato, A; Manucci, A; Pagnoni, G; Zaniboni, F; Yalçıner, Ahmet Cevdet; Altinok, Y (Elsevier BV, 2006-01-15)
The M-w=7.4 earthquake that affected the northwestern part of Turkey oil August 17, 1999, and in particular the gulf of Izmit, had dramatic consequences also as regards tsunami generation. The main cause of the earthquake was a dextral strike-slip rupture that took place along different segments of the western part of the North Anatolian Fault (WNAF). The rupture process involved not only a number of distinct strike-slip fault segments, but also dip-slip ancillary faults, connecting the main transcurrent se...
An overview of local site effects and the associated building damage in Adapazari during the 17 August 1999 Izmit earthquake
Bakır, Bahadır Sadık; Sucuoğlu, Haluk (Seismological Society of America (SSA), 2002-02-01)
Two major earthquakes occurred in Turkey along the North Anatolian fault in 1999. The first one, which occurred on 17 August 1999, had a moment magnitude of 7.4 and ruptured the 140-km segment of the fault in the Marmara region. Adapazari, a city with a population of 190,000, which is mostly located on a deep alluvial basin in the near field of the ruptured fault, was among the worst-affected urban areas in the earthquake-affected region. The distribution of damage over the city was highly nonuniform, indic...
Citation Formats
A. A. Özacar, “The 2002 Denali fault and 2001 Kunlun fault earthquakes: Complex rupture processes of two large strike-slip events,” BULLETIN OF THE SEISMOLOGICAL SOCIETY OF AMERICA, pp. 0–0, 2004, Accessed: 00, 2020. [Online]. Available: https://hdl.handle.net/11511/47505.