Research Article

Comprehensive Evaluation of the Hydrocarbon Preservation Conditions in the Complex Tectonic Area of the Southwestern Sichuan Basin, China

Table 1

Chemical characteristics of shallow and deep formation water in key wells in southwest Sichuan and its relationship with main control faults.

WellStratigraphic unitFaultExtension length (km)Fault displacement (m)Distance to main control fault (km)Mineralization (g/L)Water type

Woshen 1Cambrian bottomWo 213.6510000.40.84NaHCO3
Zhougong 1Zhou 237.7518200.653.58NaHCO3
Hanshen 12425.976001.22.35Na2SO4
Gong 2Gong 136.2120002.415.3NaHCO3
Gongshen 1Gong 136.2120003.174.1CaCl2

Zhougong 1Bottom of Upper PermianA20.947000.90.84NaHCO3
Ma 1B24.225001.43.58Na2SO4
Han 1C23.334501.50.878NaHCO3
Ta 6E17.791002.235.76CaCl2
Zi 7F38.92003.137.43CaCl2
Gong 2G15.7110003.46.08NaHCO3
Laolong 1H13.32003.6521.6CaCl2
Zi 2F38.92004.773.44CaCl2
Zi 9F38.92004.951.13CaCl2

Han 2Triassic bottomHan 205.831000.60.72NaHCO3
Ma 4Ma 59.304003.8541.43CaCl2
Han 5117.973000.830.81Na2SO4
Gaoxun 127.051001.16.65Na2SO4
Han 3Han 1220.676001.68.82CaCl2
Zhougong 2Zhou 248.299001.6216.66Na2SO4
Wo 1267.71002.119.75Na2SO4
Ma 12Ma 37.311004.146.68CaCl2