|
Borehole
|
LPI
|
Liquefaction risk
|
GFI ranked by field observation (after Bray and Stewart 2000)
|
|---|
|
Analyzed results of Annan District with the PGA = 0.168g derived from TAI station
|
|
BH-A1
|
8.6
|
High
|
GF3
|
|
BH-A2
|
10.7
|
High
|
GF3
|
|
BH-A3
|
8.4
|
High
|
GF1
|
|
BH-A4
|
2.9
|
Low
|
GF3
|
|
BH-A5
|
5.0
|
Low
|
GF3
|
|
BH-A6
|
4.1
|
Low
|
GF3
|
|
Borehole
|
LPI
|
Liquefaction risk
|
GFI ranked by field observation (after Bray and Stewart 2000)
|
|---|
|
Analyzed results of Sinshih District with the PGA = 0.233g derived from SSH station
|
|
BH-S1
|
5.7
|
High
|
GF3
|
|
BH-S2
|
8.6
|
High
|
GF3
|
|
BH-S3
|
12.5
|
High
|
GF2
|
|
BH-S4
|
13.6
|
High
|
GF3
|
|
BH-S5
|
14.1
|
High
|
GF3
|
|
BH-S6
|
13.1
|
High
|
GF3
|
|
BH-S7
|
8.9
|
High
|
GF3
|
