The Activity of the Yaziba Fault on the Lower Reaches of the Jinsha River, Southwestern China: Indirect Evidence from Paleo Earthquakes and Ancient Landslides

Table 2

The 19 paleo earthquakes identified after analysis and screening.

Number	Dating method	Age (ka)	Time interval (ka)
D4	ESR	147
B2	TL	115	3.2
B1	ESR	113	0.2
D5	ESR	81	3.2
B3	ESR	56	2.5
S5	OSL	44.7	1.13
S4	TL	43.3	0.14
B6	ESR	29.59	1.371
S2	^14C	28	0.159
S1	^14C	24.58	0.342
MH-I	^36Cl	20.8	0.378
S6	TL	19.32	0.148
Y1	TL	15.69	0.363
D6	ESR	14.2	0.149
MH-II	^36Cl	13.2	0.1
S7	TL	11.63	0.157
D8	ESR	6.79	0.484
Y3	TL	5.75	0.104
S8	OSL	3.8	0.195

MH-I is the first event of the Mahu landslide; MH-II is the second event of the Mahu landslide.