Oilfield Water and Favorable Petroleum Exploration Targets for the Triassic Baikouquan Formation in the Slope of Mahu Depression, Junggar Basin

<div>Pore types for different diagenetic phases: L: lithic clast; Q: quartz; F: feldspar. (a) Well X89, 2477.27 m: residual intergranular pore and dissolved pore development, primarily line contact between particles and surface crack development for quartz particles. (b) Well M23, 3641.29 m: strong compacted diagenesis, line contact between particles with a few residual intergranular pore. (c) Well MZ2, 4201.94 m: feldspar dissolved into intragranular pores. (d) Well M18, 3852.55 m: line contact between particles and feldspar dissolution.</div>

Geofluids

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Figure 2

Figure 2: Oilfield Water and Favorable Petroleum Exploration Targets for the Triassic Baikouquan Formation in the Slope of Mahu Depression, Junggar Basin 

Figure 2 | Oilfield Water and Favorable Petroleum Exploration Targets for the Triassic Baikouquan Formation in the Slope of Mahu Depression, Junggar Basin 