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Ruby-bearing marbles of the Southern Ural Mountains are developed in the metamorphic perimeter of granites-gneisses domes where high grade metamorphic granitization and diaphthoresis have occurred.Geological research into the development and occurrence of ruby-bearing marbles indicate that they formed as a result of repeated transformation.Their substrate consisted of an organogenous marine limestone containing Visean faunal remains.Intensive Mg metasomatism of limestone during early progressive stages of metamorphism resulted in a substrate of dolomite composition containing faunal remains with a calcite composition.Increased temperature and pressure resulted in metamorphism of early Mg metasomatites,turning them into fine-grained marble containing Visean faunal remains.Tensional stresses near the intrusive domes resulted in dedolomitization of early Mg metasomatites,giving rise to light,coarse-grained calcite marbles having polygonal-grained structure.Such carbonaceous marbles became metamorphosed around the perimeter of granite-gneiss massifs.Their rheological properties allowed for plastic flow in these marbles into areas of tectonic neutrality,forming bodies of rheomorphic marbles,sometimes even among marbled limestone.Relict bodies of Mg metasomatites underwent boudinage and rotation.Flow cleavage occurred in axial blocks of inter-dome structures and in their steep walls.Therefore platy jointing(banding,pseudo-lamination)formed in the marbles.Thickness of the plates is from several millimeters to 2-3m.Calcite underwent recrystallization with extension of grain size in the central parts of plates,sometimes amounting to 15-25cm in cross-section.Ruby-bearing marbles consist of Mg-calcite.The rock is coarse-grained,with a panidiomorphic texture.Schistosity is often observed in the plane of cleavage.Mg-calcite marble occurs among and grades into background calcite marbles,which are controlled by cleavage of flowing.It is supposed that the ruby-bearing Mg-calcite marbles bodies are elongated in the direction of dip.Their formation is caused by recrystallization under the action of rising metamorphogenic fluids at high temperatures and higher pressures(amphibolitic and epidote-amphibolitic facies).Ruby-bearing marbles formed at the end of the prograde stage of metamorphism.The early retrograde stage of metamorphism is defined by a new wave of Mg metasomatism and formation of calcite-dolomitic marbles with a poikiloblastic texture from calcite or Mg-calcite marbles.Usually the boundaries of the bodies are clear,planar,and controlled by cleavage.Studies of small bodies have shown that they are elongated in the direction of dip.Usually they contain pink corundum and/or pink spinel;red corundum is replaced by red spinel.Thus the initial marine limestones were transformed into various marbles and completely lost their primary composition and bedding as a result of metamorphism,deformation,and metasomatic transformation.Ruby-spinel mineralization in marbles is controlled by cleavage.
Ruby-bearing marbles of the Southern Ural Mountains are developed in the metamorphic perimeter of granites-gneisses domes where high grade metamorphic granitization and diaphthoresis have occurred. Geological research into the development and occurrence of ruby-bearing marbles indicate that they formed as a result of repeated transformation. their substrate consisted of an organogenous marine limestone containing Visean faunal remains.Intensive Mg metasomatism of limestone during early progressive stages of metamorphism resulted in a substrate of dolomite composition containing faunal remains with a calcite composition. Increased temperature and pressure resulted in metamorphism of early Mg metasomatites, turning them into fine-grained marble containing Visean faunal remains. Permanent stresses near the intrusive domes resulted in dedolomitization of early Mg metasomatites, giving rise to light, coarse-grained calcite marbles having polygonal-grained structure. metamorphosed around the perimeter of granite-gneiss massifs. Their rheological properties allowed for plastic flow in these marbles into areas of tectonic neutrality, forming bodies of rheomorphic marbles, sometimes even among marbled limestone. Reflections bodies of Mg metasomatites underwent boudinage and rotation. Flow cleavage occurred in axial blocks of inter-dome structures and in their steep walls. Therefore platy jointing (banding, pseudo-lamination) formed in the marbles.Thickness of the plates is from several millimeters to 2-3m.Calcite underwent recrystallization with extension of grain size in the central parts of plates, sometimes amounting to 15-25 cm in cross-section. Ruby-bearing marbles consist of Mg-calcite. The rock is coarse-grained with a panidiomorphic texture. Schistosity is often observed in the plane of cleavage .Mg-calcite marble occurrence among and grades into background calcite marbles, which are controlled by cleavage of flowing. It is said that the ruby-bearing Mg-calcite marbles bodies are elongated in the direction of dip. their formation is caused by recrystallization under the action of rising metamorphogenic fluids at high temperatures and higher pressures (amphibolitic and epidote-amphibolitic facies) .Ruby-bearing marbles formed at the end of the prograde stage of metamorphism. The early retrograde stage of metamorphism is defined by a new wave of Mg metasomatism and formation of calcite-dolomitic marbles with a poikiloblastic texture from calcite or Mg-calcite marbles. Usually the boundaries of the bodies are clear, planar, and controlled by cleavage.Studies of small bodies have shown that they are elongated in the direction of dip. Usually they contain pink corundum and / or pink spinel; red corundum is replaced by red spinel.Thus the initial marine limestones were transformed into various marbles and completely lost their primary composition and bedding as a result of metamorphism, deformation, and metasomatic transformation. Ruby-spinel mineralization in mar bles is controlled by cleavage.