000			00595nab|a22002177a|4500
999			_c61789 _d61781
001			61789
003			MX-TxCIM
005			20200513170422.0
008			200503s2012||||xxu|||p|op||||00||0|eng|d
022			_a2169-9356 (Online)
024	8		_ahttps://doi.org/10.1029/2011JB008676
040			_aMX-TxCIM
041			_aeng
100	0		_aJin-Hyuck Choi _912739
245	1	0	_aRupture propagation inferred from damage patterns, slip distribution, and segmentation of the 1957 MW8.1 Gobi‐Altay earthquake rupture along the Bogd fault, Mongolia
260			_aUSA : _bWiley, _c2012.
500			_aPeer review
520			_aA detailed analysis of the rupture patterns and slip changes along the surface rupture associated with the 1957 Gobi‐Altay earthquake (MW= 8.1) in Mongolia, which occurred along the Bogd left‐lateral strike‐slip fault, was carried out to better understand segmentation and propagation. The major surface ruptures show a simple linear pattern, whereas minor ruptures along the major ruptures, which are concentrated at rupture step overs and tip zones, show complex patterns. In the latter case, their patterns strongly resemble the geometric and kinematic characteristics of previously reported mesoscale fault damage patterns. The geomorphologic offsets show that left‐lateral slip dominated with an average displacement of 3.5 to 4.0 m, but it decreased or transferred to dip‐slip components mainly at rupture step‐overs and tip zones. Abrupt changes of rupture patterns and slip distribution indicate that the coseismic surface rupture along the Bogd fault comprises three major segments from west to east, namely, the North‐Ih, East‐Ih, and North‐Baga Bogd segments, and a highly damaged eastern tip zone. Based on the location of the epicenter, as well as the asymmetrically distributed damage structures and slips, we infer that the surface rupture propagated eastward unilaterally through several segments and reached the easternmost step‐over, which acted as a tough barrier. The rupture finally terminated, producing a highly deformed tip damage zone developed to accommodate released stress. We argue that detailed analysis of damage patterns, slip distribution, and slip transfer can help us to better understand fault segmentation and rupture propagation.
546			_aText in English
650		7	_2AGROVOC _912740 _aEarthquakes
650		7	_2AGROVOC _912741 _aDamage
651		7	_2AGROVOC _912742 _aMongolia
700	0		_912743 _aKwangmin Jin
700	1		_912744 _aEnkhbayar, D.
700	1		_912745 _aDavvasambuu, B.
700	1		_912746 _aBayasgalan, B.
700	0		_912747 _aYoung-Seog Kim
773	0		_tJournal of Geophysical Research _gv. 117, no. B12 _dUSA : Wiley, 2012. _x2169-9356
942			_cJA _n0 _2ddc