Study the Elastic Parameters of Sandy Conglomerate under Different Burial History and Petrophysical Modeling

Figure 3

Thin-section observation of compaction features of sandy conglomerates from Triassic Baikouquan Formation in the slope of the Mahu Sag. (a) Pseudomatrix formed by plastic grains deformed under pressure and (b) tight directional arrangement of plastic grains.

(a)

(b)