Xiamen Ji Yuan Stone Co.,Ltd.
Pink Onyx Marble Slab
Pink Onyx Marble Slab
Expertly crafted from natural pink onyx, this marble slab is perfect for adding a touch of luxury to any space. With its unique veining and beautiful color, it adds an elegant and sophisticated look to countertops, backsplashes, and more. Elevate your design with this stunning and durable marble slab.
| Feature | Details |
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| Material: | Marble, Granite, Onyx, Travertine, Limestone, Sandstone, Quartzite etc.. |
| Application: | Exterior Wall Cladding, Interior Walls, Interior Floors, Shower Walls, Tub Surround Walls, Kitchen Counter Tops & Vanity Tops,Flooring Tiles, Slabs, Landscapes etc.. |
| Surface Finished: | Honed,Polished |
| Color: | Yellow,black,white,red,purple wood,green,grey,pink,rainbow etc |
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For pink onyx marble slab, its formation conditions are very harsh. Most of the jade comes from some high-temperature melted magma at several tens of kilometers underground, and these melted magma flow from the underground along its surface cracks to the surface of the earth, and after cooling, form hard stones, During the whole process, only a small amount of elements will slowly crystallize into hard jade or gemstone.
The formation of jade can be divided into the following important formation stages:
1. The dolomite depositional stage was in the late Mesoproterozoic, about a billion years from today. At the location of the Kunhua Mountains today, there used to be a shallow sea area here. In this sea, there are a lot of The carbonate deposits, which contain a large amount of magnesia dolomite, and this material is the main source of material for the formation of pink onyx marble slab.
2. In the metamorphic stage of jade, dolomite is metamorphic to dolomite marble due to the strong earth fold and fault activity.
3. Due to the strong fault activity and magma in the subsurface, a large amount of acid rocks intrude into dolomite marble along the fault zone. Due to the excessive remnants of some dolomite marble captive bodies and some tongue-shaped bodies at the top of the intrusion and magma into the body. After these liquids come into contact with hydrothermal fluids, diopside and forsterite are formed, and these innate material conditions are one of the material conditions in the formation of jade.
The formation of natural pink onyx marble slab is mainly caused by volcanic eruption and magma intrusion and then through the later hydrothermal action to form natural jade. These deposited items include biological remains and debris, which will become jade after certain chemical precipitation and epidermal leaching.
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