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These large concentrations are formed by regionally distributed reservoirs and cap rocks. .
In summary, tight sandstone gas reservoirs in China are characterized by sheet-like coal-measure source kitchens, widely distributed reservoirs, a close contact between source rocks and reservoirs, and 3D gas-bearing and partial accumulation.
The other is associated with deep tight gas reservoirs, mainly universal reservoir densification (L), stable tectonic settings (W), widely distributed reservoirs (D), and source rocks in a close contact with reservoirs (S).
"Densification accumulation" tight gas forms after reservoir densification under hydrocarbon generation expansive force (no buoyancy), and accumulates in depression and slope areas with the following controlling factors, effective source rocks (S), widely distributed reservoirs (D), stable tectonic settings (W), and universal reservoir densification (L).
Deep tight gas reservoirs are mainly controlled by effective source rocks positioned adjacent to reservoirs (S) and characterized by continuous hydrocarbon expulsion, widely distributed reservoirs (D), stable tectonic settings (W), and universal reservoir densification (L), with the development model shown by "T-LWDS" (T means time).
For the DA type, reservoir densification prior to the gas charging period (GCP) leads to accumulation in depressions and slopes largely due to hydrocarbon expansive forces without buoyancy, and critical controlling factors are effective source rocks (S), widely distributed reservoirs (D), stable tectonic settings (W) and universal densification of reservoirs (L).
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