Electronic Supplement to
The 2015 M_w 6.4 Pishan Earthquake: Seismic Hazards of an Active Blind Wedge Thrust System at the Western Kunlun Range Front, Northwest Tibetan Plateau

by Tao Li, Jie Chen, Lihua Fang, Zhuxin Chen, Jessica A. Thompson, and Chengzao Jia

Table S2. Fault Area and Corresponding Moment Magnitude for Each Segment of the Hetian Fold Belt, Assuming Base of Seismicity Is Localized along the Lower Detachment Surface

Fold Name		Fold Length (km)	Fault Width (km)*	Fault Dip	Fault Area (km2)	Moment Magnitude
Guman	F1	80	10	18°	800	7.6
	F2	80	9	10°	720
	F3	80	11	8°	880
	Back thrust	80	3	19°	240
Yaheshtagh	F1	50	11	16°	550	7.5
	F2	50	15	8°	750
	F3	50	13	8°	650
	Back thrust	50	5	18°	250
East Slik		<33	3.3	22°	<110	<6.2

See Figures S2–S4 for the fold and fault names.

* The distance of fault segment from fault tip to its merging point with the lower detachment.

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