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Xiamen Ji Yuan Stone Co.,Ltd.

40mm Sandstone Paving

40mm Sandstone Paving

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As a product expert in the paving industry, trust our 40mm Sandstone Paving for its durable construction and timeless beauty. Made from high-quality sandstone, this paving is perfect for any outdoor space and will provide long-lasting appeal. Increase your property's value and enhance its appearance with our 40mm Sandstone Paving.

 

Feature Details
Materia Natural Sandstone
Surface Finished Honed,Flamed,Bush-hammered,Brushed,Nature,Mushroom,Sawn etc
Finished Products Floor tiles, Wall cladding, Countertops, Windowsills, Special-shaped tiles, Small slabs, Swimming pool, steps, wall panel, flooring, veneers, slabs, coping tiles, etc
Color Yellow,black,white,red,purple wood,green,grey,rainbow etc

       

      40mm Sandstone Paving: Composition & Formation

      1. Composition & Characteristics

      • 40mm sandstone paving is primarily composed of detrital quartz and feldspar.
      • Feldspar content can be significantly high, including orthoclase, plagioclase, and acid plagioclase.
      • The color is often red or yellow, influenced by the parent rock’s mineral composition.

      2. Formation Process

      • Requires feldspar-rich parent rocks such as granite and granite gneiss.
      • Formation is influenced by tectonic activity, paleogeography, and paleo-climatic conditions.
      • In regions with strong tectonic movements and granite basement uplifts, heavy erosion leads to thick sandstone deposits.

      Detrital 40mm Sandstone Paving

      1. Composition & Variability

      • Composed mainly of quartz and lithic fragments.
      • Lithic sandstone varies in composition depending on the parent rock.
      • Common feldspar types include plagioclase and potassium feldspar, but may also contain unstable basic plagioclase.

      2. Appearance & Formation

      • Typically darker in color, such as gray, gray-green, and gray-black, while lighter-colored varieties are rare.
      • Formed in depression zones or basins near structural uplift areas due to rapid erosion and accumulation of parent rock fragments.
      • Can originate from both terrestrial and marine environments.
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