Pore Structure Differentiation between Deltaic and Epicontinental Tight Sandstones of the Upper Paleozoic in the Eastern Linxing Area, Ordos Basin, China

<div>Shape of fluid inclusions in coal-measure sandstones. (a) Hydrocarbon-bearing brine inclusions in quartz grain cracks; (b) carbon dioxide gaseous hydrocarbon inclusions in calcite fractures.</div>

Geofluids

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Figure 13

Figure 13: Pore Structure Differentiation between Deltaic and Epicontinental Tight Sandstones of the Upper Paleozoic in the Eastern Linxing Area, Ordos Basin, China 

Figure 13 | Pore Structure Differentiation between Deltaic and Epicontinental Tight Sandstones of the Upper Paleozoic in the Eastern Linxing Area, Ordos Basin, China 