No. Contact metamorphism will most likely alter shale into hornfels. Phyllite is regionally metamorphosed slate, and slate is metamorphosed shale.
The rock has undergone metamorphism. Metamorphism is the process in which the mineral composition and texture of a rock change in response to heat, pressure, or chemical reactions. This can result in the formation of new minerals and changes in the rock's appearance and physical properties.
Metamorphic rocks change due to high temperature and pressure deep within the Earth's crust. These conditions cause the minerals within the rock to recrystallize, resulting in a new texture and sometimes new minerals forming. Additionally, the presence of fluids can also contribute to the chemical changes that occur during metamorphism.
Heat and pressure deep below Earth's surface change existing rock into metamorphic rock through a process called metamorphism. This process involves the recrystallization of minerals within the rock without melting it completely.
Yes, minerals in a rock can change the way they look through processes like weathering, erosion, and metamorphism. These processes can alter the color, texture, and composition of the minerals in the rock, leading to changes in its overall appearance.
Sedimentary, since the other two types involve extreme heat and/or metamorphism which could destroy any fossil evidence
Phyllite is a type of metamorphic rock that comes from adding heat, pressure, and/or chemically active fluids to slate. Slate is the parent, or originial, type of rock from which the phyllite forms. It could also be said that slate recrystallizes into phyllite. Slate is also a metamorphic rock that starts out as the sedimentary rock called shale. Therefore, phyllite comes from slate, which comes from shale. Phyllite is different from slate because it has been metamorphosed more. As a result, the straight lines/planes (called foliation) that slate breaks along, are absent in phyllite, which is distinctly wavy in appearance. If more metamorphism is applied to phyllite, it recrystallizes into schist.
If limestone undergoes contact metamorphism, it will typically turn into marble. Marble forms from the recrystallization of limestone under high temperature and pressure conditions.
Contact metamorphism generally occurs relatively close to the surface in a zone of contact between an intruding magma body and the country rock, which could be a sedimentary, igneous, or previously metamorphosed rock. Hornfels is a common resultant contact metamorphic rock.
Yes, slate, which is a fine-grained metamorphic rock formed from the metamorphism of shale, can further undergo metamorphism to transform into another metamorphic rock. The process of changing one metamorphic rock into another is known as metamorphic progression or metamorphic differentiation. If slate undergoes increased heat and pressure over time, it can undergo further metamorphism and transform into a different type of metamorphic rock. The specific type of rock it may transform into depends on the intensity of the metamorphic conditions. For example, if the temperature and pressure increase significantly, slate might progress to phyllite, schist, and eventually, if conditions are extreme, it could transform into gneiss. Metamorphic rocks form through the alteration of existing rocks (igneous, sedimentary, or other metamorphic rocks) due to heat, pressure, or chemically reactive fluids over geological time. The process of metamorphism involves changes in mineral composition, texture, and structure.
Rhyolite is an igneous, rock, of silica-rich composition (> 69% SiO2). The mineral assemblage is usually quartz, alkali feldspar and plagioclase (in a ratio > 1:2), Biotite and hornblende are common accessory minerals.
Under influence of pressure and temperature, a rock can change, the process is called deformation or metamorphism, the result is a metamorphic rock. This can happen to igneous rocks as well.
The rock has undergone metamorphism. Metamorphism is the process in which the mineral composition and texture of a rock change in response to heat, pressure, or chemical reactions. This can result in the formation of new minerals and changes in the rock's appearance and physical properties.
Igneous rock can become metamorphic rock through the pathways of regional metamorphism, where intense pressure and heat from tectonic forces transform the rock, or contact metamorphism, where it is altered by high temperatures from nearby magma intrusion.
Yes
Metamorphic rocks change due to high temperature and pressure deep within the Earth's crust. These conditions cause the minerals within the rock to recrystallize, resulting in a new texture and sometimes new minerals forming. Additionally, the presence of fluids can also contribute to the chemical changes that occur during metamorphism.
Directional pressure and high temperatures are two factors that could cause an igneous rock to metamorphose. Processes that lead to these factors could be tectonic plate movements, depth of burial, or proximity to an intrusive body.
Contact the supplier directly -= normally you will want the accounts team. Thye will ask for the reason for name change and could then ask for proof of identity.