Red Sandstone Flooring

Create a stunning, durable, and versatile space with our Red Sandstone Flooring. Made with high-quality, natural red sandstone, our flooring offers a unique and elegant touch to any room. Its sturdy composition and timeless appeal make it a practical and long-lasting investment for your home or business.

Feature	Details
Material	Natural Sandstone
Surface Finished	Honed, Flamed, Bush-hammered, Nature, Mushroom, Swan 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
Finished	Honed, Split, Sandblasted, Sawn, Antiqued, Pineapple, etc.
Quality details	Polished degree: 95 degree or up. Thickness tolerance: +/-0.5mm. Diagonal tolerance: +/-1mm. Surface flatness tolerance: +/-0.3mm. Adjacent edge verticality tolerance: +/-0.5mm, Precise Cutting by infrared-ray-cut machine
Usage	For internal & external decoration and construction, Walling or flooring tile.
Edgeing	Full Bullnose, Half bullnose, Flat eased (eased edge), Bevel top, Radius Top, Laminated Countertop, Ogee Edge, DuPont, Edge, Beveled or others.
Size	Standard (But if you have special requirements, you can consult our CSA.)
Surface Finish	Polished, Flamed,Honed, Bush Hammered-sandblast, Chisselled.
Package	Fumigation wooden crates;Slab:fumigation wooden bundles
Payment	T/T 30% Deposite

 

Biological Red Sandstone Flooring Limestone

1. Structural Components

1.1 Particles

• Biochips:
• Primarily composed of shell fragments.
• The original shell structure is destroyed due to strong dissolution and refilling.
• Mostly bivalve shells; other biochips are rare.
• Sand Debris:
• Appears black under the microscope, round in shape, and poorly sorted.
• Some grains reach up to 1.3mm in size.
• Does not change color after being dyed by the mixed solution, indicating its mineral composition is dolomite and terrigenous mud.

1.2 Substrate

• Composed of powdered calcite.
• Uniform particle size of approximately 0.01mm.

2. Rock Structure

• The original sediments were supported by stucco.
• Unevenly distributed with stucco-filled gaps.
• No seabed cement present.

3. Naming

• Based on Dunham’s classification scheme, the original rock is classified as:
  Bioclastic Sand-Red Sandstone Flooring.

4. Diagenesis and Pore Evolution

4.1 Diagenesis

• Micrite Formation:
• Micrite jackets formed on the surface of shells.
• Dissolution:
• The rock underwent strong dissolution.
• The stucco matrix was corroded, forming irregular residues.
• Distinct dissolution traces are evident.
• Dolomite sand debris remains undissolved.
• Re-cementation:
• Two-stage fillers observed in the dissolved pores:
1. Early Stage: Granular, iron-free calcite, mainly found along pore walls and partially filling dissolved pores.
2. Late Stage: Iron-containing calcite, turning purple-red when dyed with the mixed solution.
• Mostly large, continuous crystal calcite with clear cleavage.
• The two-stage calcite likely serves as cement in the primary intergranular pores.
• Due to dissolution followed by re-cementation, the original rock structure is released, giving it the appearance of granular rock.