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Black Marble, Green Marble, Red Marble
Black Marble, Green Marble, Red Marble
| Analysis Test Name | : | Chemical Analysis of CaO, SiO2,Al2O3,Fe2O3,MgO in Natural Stones | ||||||
| Analysis Test Code | : | 35-30-AA-30 | ||||||
| Analysis Test Method | : | TS EN 15309 | ||||||
| Barcode | Name Of Sample | Al2O3 % | CaO % | Fe2O3 % | MgO % | SiO2 % |
| 17-H-000730 | BLACK SWAP | 0.57 | 53.83 | 0.20 | 0.41 | 2.14 |
| The Analysis / Test Name | : | Determination Of the Pre technological Analysis | |||
| Test Name | Result | ||
| Cutting Stone Slab | Good | ||
| Cutting Edge, Corner | Good | ||
| Polishing Capabilitiy | Getting polished |
| The Analysis / Test Name | : | Determination Of the Hardnes | |||
| Test Name | Result | ||
| Hardness (Mohs) | 4 |
The Analysis / Test Name | : | Real Density, Apparent Density, Open Porosity and Total Porosity | |||||
| The Original Condition Of The Sample | As a Stone | ||||
| The Drying Temperature of Sample © | 110 | ||||
| Weight of the Sample(g) | 5,54 | ||||
| Volume of the Sample (cm3) | 2,04 | ||||
| Real Density (g/cm3 ) ( ASTM D5550-06) | 2,71 | ||||
| Analysis Test Name | : | Petrographic Analysis for Marble Group Natural Stones | |||||
| Analysis Test Method | : | TS EN 12407 | |||||
| MACROSCOBI DESCRIPTION | |||||||
| Color | : | Very Light Gray b ( According to N8 - Geologic Rock-Color Chart (2009) | |||||
| Texture | : | Massive | |||||
| Grain Size | : | Fine Grained | |||||
| Fractures | : | They compose of the thickness, their iner are filled with secondary (carbonate) mineral fillings | |||||
| MICROSCOBIC DESCRIPTION | |||||||
| Thin section made date | Number of this section | Thin section size (mm) | |||||
| 23.02.2017 | 1 | 28x48 | |||||
| Texture | : | Microcrystalline | |||||||||
| Composition | : | ||||||||||
| Carbonate minerals | : | with 100% ration, fine grained, xsenomorphic-hypidiomorphic, isometric, homogenously distributed isotropic. | |||||||||
| Discontinuousity | : | ||||||||||
| Filled Cracks and Veins | : | They vary between 0.16-1,2mm widthes, various lengths, their insides were filled with secondary carbonate (micro-mesocrystalline) minerals, homogeneously distributed; very little ratio of them are as stylolite shapes filled with opaques, their distribution are heterogeneous. | |||||||||
| Explanations | : | According to their chemical analysis results , for example they are composed of 98.11% of calcite and 1.89% of dolomite minerals. | |||||||||
| Being undergone the structural forces, the rock retains oftenly a breccia figure, with filled cracks of developed varios widths | |||||||||||
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