The margin of the southern Qinshui Basin is confined by faulted fold belts, the enrichment region is formed in gentle slope area.
沁水盆地南部周缘被挤压性断裂褶皱带所围限，区内缓坡带形成煤层气富集区。
The margin of the southern Qinshui Basin is confined by faulted fold belts, the enrichment region is formed in gentle slope area.
沁水盆地南部周缘被挤压性断裂褶皱带所围限，区内缓坡带形成煤层气富集区。
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