Antigorit Kabaşon Taş
Category
                                
                            Brand
                                
                            Stock Code
                                KAB-22
                            Stock Quantity
                            
                                1
                            
                        Money Transfer
                                
                                    717,78 TL
                                                                            (%5,00 bank transfer discount)
                                                                    
                            
                                755,56 TL
                            
                        ANTIGORITE STONE PROPERTIES
 STONE DIAMETER: 16X12 MM
 WEIGHT: 3.52 GR 17.6 CRT
Antigorite Cabochon Stone
 Mineralogy
 Group: Serpentine (Silicates/ Phyllosilicates)
 Crystal System: Monoclinic
 Composition: Mg3(Si2O5)(OH)4
 Form/Habit: Usually massive or pseudomorphic. Minute crystals, typically flat, rarely elongated. Often bladed or fibrous.
 Hardness: 3.5-4
 Cleavage: Perfect
 Fracture: Splinter, Conchoidal
 Luster: Oily, Subvitreous
 Stripe: Greenish White
 Specific Gravity: 2.58-2.8
 Transparency: Translucent, Opaque
 RI: 1.530-1.575
 Color: Green, Green-blue, White, Brown, Black.
 antigorite stone
 Geology
 Antigorite is part of the Serpentine group. Its olive-green color and smooth or scaly appearance are the basis of its name, which, according to Best (2003), derives from the Latin serpentinus, meaning snake rock. Its origins lie in the metamorphic alterations of peridotite and pyroxene. Serpentines may also pseudomorphically replace other magnesium silicates. Antigorite Cabochon Stone
 Antigorite rock can be incomplete, causing the physical properties of serpentines to vary widely. Where it forms a significant portion of the land surface, the soils contain unusually high levels of clay. Antigorite is the most common serpentine polymorph formed during metamorphism of wet ultramafic rocks and is stable at temperatures exceeding 600 °C at depths of up to 60 km. Antigorite Cabochon Stone
 In contrast, antigorite, lizardite, and chrysotile typically form near the Earth's surface and decompose at relatively low temperatures, probably well below 400 °C. It has been suggested that chrysotile is never stable relative to either of the other two serpentine polymorphs.
 In the uppermost mantle of ocean basins, ultramafic rocks often contain abundant serpentine. Antigorite contains approximately 13% water by weight. Antigorite may play an important role in transporting water to the surface through subduction zones and subsequently releasing it to form magmas in island arcs. Antigorite Cabochon Stone. Some of the water may be transported to greater depths. Antigorite Cabochon Stone
 Soils derived from serpentine are toxic to many plants due to high levels of nickel, chromium, and cobalt. Areas of serpentine-derived soil will appear as open, scattered small trees, often with conifers, in scrubby strips and otherwise forested areas. The flora is often very diverse, with specialized slow-growing species. These areas are called serpentine wastelands. Antigorite Cabochon Stone
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								Muhteşem ürünler, harika paketleme, minik sevimli hediyeler ve çok hızlı kargolama için çok teşekkür ederim
							
							
																	H... K... | 29/07/2025
															
						
								Labradoritlerim görsellerden çok daha güzel ,çünkü gerçek doğal taş ve canlı. Mağazal iletişimi henüz satın almadan muhteşemdi,hızla elime geçen kargom ve şık paketlemeniz için de ayrıca teşekkürler .
							
							
																	Elif alnl | 17/04/2025
															
						
								Kullanımı kolay ve zevkli.
							
							
																	E... A... | 10/12/2024
															
						
								Ben siteyi beğendim.
							
							
																	NIKOLAY ZARUBIN | 03/10/2024
															
						
								Ben siteyi beğendim.
							
							
																	NIKOLAY ZARUBIN | 03/10/2024
															
						
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