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26-32 occur in the ANHF zone were distributed in the blocks i-ii and 12, these samples have the similar chemical type of Na(Ca)HC[O.sub.3](S[O.sub.4]).
16-17 and 19 occur in the intersection of the LMSF, XSHF and ANHF zones where the extrusion stress increased yearly from 2004 to 2007 before the Wenchuan earthquake [40, 41].
(2) The concentrations of [K.sup.+] and S[O.sub.4.sup.2-] of the samples of the springs nos.16-17 and 19 in the intersection of LMSF, XSHF, and ANHF varied evidently, with the amplitude ranging from 19.3% to 59.6% before and after the Wenchuan earthquake which may be attributed to the interfusion of the deep fluids with high [K.sup.+] and S[O.sub.4.sup.2-] induced by the increased tectonic stress.