p. 257−265
2423-396X
Vol.27/No.2
pyroxene andesite> dacite) were more weathered than those on the plutonic parent rocks (alkali granite, granodiorite, monzodiorite, syenite, pyroxene diorite). Ba and CIA weathering indices predicted weathering trend such as MFW ternary plot, and it seems these two weathering indices are the most suitable weathering indices after W index (or MFW ternary plot) in this semiarid region. Ca, Na and K elements are presented in chemical weathering formulas of these two indices. These elements are in the feldspar minerals structures which are the most mineral in the earth crust.]]>
p. 266−281
2423-396X
Vol.27/No.2
p. 282−291
2423-396X
Vol.27/No.2
p. 292−303
2423-396X
Vol.27/No.2
p. 304−312
2423-396X
Vol.27/No.2
p. 313−327
2423-396X
Vol.27/No.2
p. 328−341
2423-396X
Vol.27/No.2
p. 342−350
2423-396X
Vol.27/No.2
p. 351−362
2423-396X
Vol.27/No.2
p. 363−372
2423-396X
Vol.27/No.2
p. 373−380
2423-396X
Vol.27/No.2
p. 381−393
2423-396X
Vol.27/No.2
p. 394−405
2423-396X
Vol.27/No.2
p. 406−414
2423-396X
Vol.27/No.2
p. 415−421
2423-396X
Vol.27/No.2
p. 422−431
2423-396X
Vol.27/No.2
p. 432−440
2423-396X
Vol.27/No.2
p. 441−451
2423-396X
Vol.27/No.2
p. 452−461
2423-396X
Vol.27/No.2
p. −
2423-396X
Vol.27/No.2