Tem po ral b-value vari a tions have been com pletely ob tained for the seis mic fault ing pro cess of the 4 March 2008 Taoyuan earth quake (ML = 5.2), south ern Tai wan. In ad di tion to trig ger ing sev eral hun dred after shocks, the mainshock was pre ceded by two groups of foreshocks (64 events) that clus tered along the nar row ma jor fault zone. A high b-value of ~1.25, es ti mated from t...