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CBM reservoir accumulation depends on the preservation conditions resulting from tectonic uplift.
The main controlling factors of composite tight gas reservoir accumulation can thus be classified into two subsidiary sets.
Tight sandstone gas reservoirs are also distributed across large areas and are positioned vertically adjacent to source rocks, which is a key to tight sandstone gas reservoir accumulation.
Therefore, the E2 s mixed siliciclastic carbonate sediments in the central Bohai Sea had good geological conditions for high-quality reservoir accumulation, and it is prospective for exploration and development.
By analyzing the relationship between the tectonic evolution and reservoir accumulation, the aim is to clarify the genetic mechanism of the unsteady reservoir and then make suggestions for the field development.
The first phase of hydrocarbon reservoir charging was distributed across the whole region, whereas the second phase of the hydrocarbon reservoir accumulation was mainly distributed near the sub-sags and mainly in the hydrocarbon generation layers.
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The genetic mechanisms of composite tight gas reservoirs are thus a recombination of conventional tight and deep tight gas reservoir accumulations, resulting in the complex gas water relationships and full gas-bearing properties.
A lot of research into tectonics, sedimentology, reservoir, oil accumulation, and exploration has been undertaken in the Qingxi Sag and the South Uplift (Yang et al. 2004; Wang et al. 2005; Sun et al. 2006; Pan et al. 2007).
As the distances from source rocks to reservoirs increases, the accumulation dynamics for the reservoirs decrease and the hydrocarbon-filling degree decreases as well.
All types of reservoirs with high accumulation dynamics can accumulate hydrocarbon.
In the following case studies, each primary lacustrine source rock in the major basins will be characterized in detail for their lithofacies association, reservoir and hydrocarbon accumulation, and "Hybrid Play" potential.
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