Electronic Supplement to by Xiwei Xu, Wenbin Chen, Wentao Ma, Guihua Yu, and Guihua Chen
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![]() | Photo 1. Surface rupture zone of Kunlunshan earthquake crossing Gelmod-Lhasa Road in N80°W direction at the 2894 km road marker, which consists of pure shear fractures, shear fractures, transtensional fractures, tension gashes, and mole tracks in en echelon pattern with a width of 10 m to 32 m (photo toward the west). |
Photo 2. A N80°W-trending pure shear fracture offset a shallow gully 3.9 m in a left-lateral sense and a mole track occurred at its eastern end just a few tens of meters west of the 2894 km road marker from Gelmod to Lhasa (photo toward the south). |
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![]() | Photo 3. N72-75ºE-trending shear fractures in left-lateral right-stepping and mole tracks in stepovers about 1 m high on the youngest terrace surface at outlet of Baladacaiqu Stream (photo toward the northwest). |
Photo 4. Left-lateral right-stepping N65ºE-trending transtensional fractures and low mole tracks in stepovers about a few decades of centimeters high at the eastern end of the northern branch of a restraining stepover 47 km east of Kunlunshan Pass (photo toward the northeast). |
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Photo 5. N45ºE-trending tension gash at the southwestern end of a N80ºE-trending pure shear fracture on the youngest terrace surface at outlet of Baladacaiqu Stream (photo toward the east).
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Photo 6. Two secondary surface rupture zones, consisting of shear fractures, transtensional fractures, tension gashes, and mole tracks, are arranged left-stepping to form a second-order pull-apart structure where tension gashes are well developed (photo toward the east). |
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Photo 7. Slicksides with a dip angle of 28° toward the east on the southern fault plane, showing left-lateral slip with a little reverse (vertical) component, just a few tens of meters west of the 2,894 km road marker from Lhasha to Gelmod (photo toward the south). |
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