Pore structure characteristics
of tight sandstones, including pore
types, connectivity, and morphological features, provides a basis
for selecting the “sweet spot” in tight sandstone reservoirs.
A variety of research methods, high-pressure mercury intrusion porosimetry,
cast thin sections, scanning electron microscopy, and fractal theory
were integrated to explore these parameters of tight sandstones from
the Chang 7 member of the Triassic Yanchang Formation in the Ordos
Basin, China. Results indicate that tight sandstones are defined by
three pore types with distinct fractal dimensions and corresponding
pore structure, which are combined pores, isolated grain pores, and
clay-dominated pores. The pore spaces of the three types gradually
evolve from the microscale to the nanoscale. Combined pores were formed
by dissolution pores connected to the surrounding pores and have been
distinguished by their irregular shape. Their connected paths are
multidirectional, resulting in better connectivity. Isolated grain
pores have a small number of poorly connected paths, which causes
weak connectivity. Clay-dominated pores have narrow and complex connected
paths, resulting in poor connectivity. From the combined pore to the
clay-dominated pore, the fractal dimensions of pore spaces decrease,
indicating that the heterogeneity of pore spaces is gradually weakened
whereas the heterogeneity of the flow characteristics is gradually
enhanced. On the basis of the proportions of the three pore types,
the tight sandstones can be genetically classified into a combined
pore type, an isolated grain pore type, and a clay-dominated pore
type. The differences in pore space and heterogeneity affect the distribution
of tight oil; therefore, sand bodies located near the source rock,
characterized by strong dissolution and dominated by the combined
pore type, are favorable zones for tight sandstone reservoirs.