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These keywords were added by machine and not by the authors. The only way to know is to prospect! Am J Sci 286:81–104, Slaughter J, Kerrick DM, Wall VJ (1975) Experimental and thermodynamic study of equilibria in the system CaO-MgO-SiO, Suzuki K (1977) Local equilibrium during the contact metamorphism of siliceous dolomites in Kasuga-mura, Gifu-ken, Japan. Contrib Mineralog Petrol 61:79–89, Tilley CE (1951) A note on the progressive metamorphism of siliceous limestones and dolomites. The types of Limestone are Chalk, Coquina, Fossiliferous Limestone, Lithographic Limestone, Oolitic Limestone, Travertine, Tufa whereas types of Dolomite are Boninite and Jasperoid. II : Migration of isotopic and reaction fronts around cooling plutons, Petrogenetic processes associated with intermediate and silicic magmatism in the Oslo rift, south-east Norway, On the mechanism of contact aureole formation in dolomitic country rock by the Adamello Intrusion (northern Italy), Flow and Transport During Contact Metamorphism and Hydrothermal Activity: Examples from the Oslo Rift, Age relations among Oslo Rift magmatic rocks: implications for tectonic and magmatic modelling, Mass estimates of cumulates and residues after anatexis in the Oslo graben, The Upper Carboniferous-Permian Oslo Rift; Basin Fill in Relation to Tectonic Development, By clicking accept or continuing to use the site, you agree to the terms outlined in our. The Glockner area of the Tauern window, Austria. As the rocks often also contain variable amounts of quartz they are sometimes referred to as siliceous dolomites and siliceous limestones. Limestones and dolomites. all limestone or dolomite. Proc Geol Soc Lond 1599:10 pp, Fernández-Caliani JC, Galán E (1998) Effects of fluid infiltraion on wollastonite genesis at the Mérida contact-metamorphic deposits, SW Spain. The porphyry copper deposits near Ely, Nevada, occur within at least six bodies of quartz monzonite porphyry, associated spatially with barren sills, plugs, and a large stock of porphyritic quartz monzonite. 2.3 Marble Group. Dolomite vs Limestone characteristics assist us … Skarns can form by regional, or contact metamorphism and therefore form in relatively high-temperature environments. Hardness – hard, although component mineral is soft (calcite is 3 on Moh’s scale of hardness) Over 10 million scientific documents at your fingertips. A related rock… 3. 2000: Industrial mineral quality of limestone: the effect of contact metamorphism on textural properties, brightness and geochemistry. Deposition of magnesian limestones by marine organisms. © 2020 Springer Nature Switzerland AG. Marble is a metamorphic rock that forms when limestone is subjected to the heat and pressure of metamorphism. The resulting rocks are classed under the group name of hornfels. The mineralized intrusive rocks were largely localized by the thrust-faulted contact between the Pennsylvanian Ely Limestone and the Mississippian Chainman Shale. Contact Metamorphism What is Contact Metamorphism . Pure marble is the result of metamorphism of a very pure limestone or dolomite. J Metamorph Geol 15:59–70, Jamtveit B, Dahlgren S, Austrheim H (1997) High grade contact metamorphism of calcareous rocks from the Oslo Rift, Southern Norway. J Petrol 33:693–728, Holness MB (1997) Fluid flow path and mechanisms of fluid infiltration in carbonates during contact metamorphism: the Beinn an Dubhaich aureole, Skye. Island Arc 9:400–416, Omori S, Liou JG, Zhang RY, Ogasawara Y (1998) Petrogenesis of impure dolomitic marble from the Dabie Mountains, Central China.

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