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What is primary porosity? 


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Primary porosity refers to the inherent pore spaces within a rock that are formed during the initial sediment deposition process, before any post-genetic alterations occur. It is a crucial parameter influencing reservoir quality and productivity in hydrocarbon exploration . Factors affecting primary porosity include grain shape, size, sorting, packing, and orientation in sandstones . Understanding primary porosity is essential for predicting reservoir quality, as it directly impacts permeability and fluid flow within the rock matrix . In sandstones, primary porosity is influenced by various attributes like roundness, flatness, elongation, and grain packing texture, with grain-size distribution playing a significant role . The development of primary porosity in igneous rocks is also discussed, highlighting its importance in basement formations and its time- and scale-dependent nature .

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Primary porosity in igneous rocks is the initial pore space formed during magma cooling, classified into diffusive (Class D) and flow (Class F) features, influencing permeability and transport properties.
Primary porosity is inherent inter-granular porosity in rock formed during lithogenesis, distinct from secondary porosity created post-genesis by processes like fracturing or dissolution.
Book ChapterDOI
01 Jan 2023
Primary porosity is formed during sediment deposition, influenced by factors like grain shape, size, and packing. It is a key aspect of reservoir characterization and affects permeability.
Primary porosity in sandstone is crucial for predicting reservoir quality. It is influenced by grain shape, grain-size distribution, and packing texture, rather than mean grain size.

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