Feldspar Dissolution and Its Influence on Reservoirs: A Case Study of the Lower Triassic Baikouquan Formation in the Northwest Margin of the Junggar Basin, China

Figure 10

(a) Relationship between the feldspar dissolution and depth; (b) the content of illite-smectite mixed-layer clays and (c) kaolinite; type 1 includes lithofacies of A, B, C, and F in the classification of lithofacies in the study area. Type 2 includes lithofacies of C, E, and G in the classification of lithofacies in the study area.

(a)

(b)

(c)