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 11

The compositions of paragenetic marginal minerals; (a) pores; (b) K-feldspar; (c) kaolinite, and (d) chlorite.

(a)

(b)

(c)

(d)