Geofluids / 2017 / Article / Tab 1

Research Article

The Early Cambrian Mianyang-Changning Intracratonic Sag and Its Control on Petroleum Accumulation in the Sichuan Basin, China

Table 1

The thickness of Sinian (Ediacaran)-Early Cambrian strata in wells across the intracratonic sag.

FormationWestern marginCenter of the Mianyang-Changning intracratonic sagEastern margin
LL-1# (m)W-28# (m)WS-1# (m)Z-4# (m)GSH-1# (m)ZS-1# (m)GS-17# (m)L-206# (m)GS-1# (m)PL-1# (m)

Lower CambrianLongwangmiao Fm.51811647621113892555.587124
Canglangpu Fm.88135182267196129214239.591.1191
Qiongzhusi Fm.223356578386459430398210.3157247
Maidiping Fm.24.5/53198/452850.6//

Ediacaran/SinianFourth member of Dengying Fm.223.532118/8139/29.1262.559
Third member of Dengying Fm.65.511764611No data67.1557

(For locations, see Figure 1.)

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