In light of different metamorphism degrees, regional metamorphism can be divided into three zones of shallow, intermediate, and deep metamorphic, and the corresponding metamorphic grade is low, intermediate, and high grade.

What is the main factor that affect regional metamorphism?

Temperature, hydrostatic pressure, and shearing stress, together with the chemical activity of percolating pore fluids, are the major physical variables governing the process of regional metamorphism.

What is regional metamorphism?

Regional metamorphism is metamorphism that occurs over broad areas of the crust. Most regionally metamorphosed rocks occur in areas that have undergone deformation during an orogenic event resulting in mountain belts that have since been eroded to expose the metamorphic rocks.

How is regional metamorphism formed?

Regional metamorphism occurs when rocks are buried deep in the crust. This is commonly associated with convergent plate boundaries and the formation of mountain ranges. Because burial to 10 km to 20 km is required, the areas affected tend to be large. Most regional metamorphism takes place within continental crust.

Is regional metamorphism foliated?

Regional metamorphism occurs over large areas and generally does not show any relationship to igneous bodies. … Thus, regional metamorphism usually results in forming metamorphic rocks that are strongly foliated, such as slates, schists, and gniesses.

What are the different types of metamorphic zones?

Where does regional metamorphism occur?

As described above, regional metamorphism occurs when rocks are buried deep in the crust. This is commonly associated with convergent plate boundaries and the formation of mountain ranges. Because burial to 10 km to 20 km is required, the areas affected tend to be large.

What is regional metamorphism quizlet?

Regional Metamorphism Definition. A change in a large area of rock due to heat and pressure ( movements in the earths crust)

What rock is formed by regional metamorphism?

Most foliated metamorphic rocks—slate, phyllite, schist, and gneiss—are formed during regional metamorphism. As the rocks become heated at depth in the Earth during regional metamorphism they become ductile, which means they are relatively soft even though they are still solid.

Why is it called regional metamorphism?

In regional metamorphism, rocks that form closer to the margin of the tectonic plates, where the heat and pressure are greatest, often differ in their minerals and texture from those that form farther away. …

What are barrovian zones?

The sequence of metamorphic zones is called a metamorphic facies series, and the most common of these is Barrovian (called after George Barrow who first mentioned it in 1912). In this series of zones, both pressure and temperature increase gradually along the metamorphic gradient.

How are metamorphic belts formed?

Metamorphic belts are a consequence of thermal perturbations, due to low temperature with respect to pressure ratios (dT/dP) in oceanic trenches and high temperature with respect to pressure ratios (dT/dP) in arcs.

How is regional metamorphism is related to plate boundaries?

When rocks are buried deep in the crust, regional metamorphism occurs. This is commonly associated with the boundaries of convergent plate and mountain range formation. Because burial is required from 10 km to 20 km, the affected areas tend to be large. It happens in a much larger area.

What is regional metamorphism and contact metamorphism?

Metamorphism is the solid change in minerals and textures in a pre-existing rock (country rock) due to changing pressure / temperature conditions. Conversely, contact metamorphism usually occurs under higher temperature conditions associated with ignorant intrusions on a smaller scale. …

What causes regional metamorphism quizlet?

What causes regional metamorphism? Pressure builds up in rock that is buried deep below other rock formations or when large pieces of the Earth’s crust collide with each other.

Where do regional and contact metamorphism occur?

Most regional metamorphism takes place within continental crust. While rocks can be metamorphosed at depth in most areas, the potential for metamorphism is greatest in the roots of mountain ranges where there is a strong likelihood for burial of relatively young sedimentary rock to great depths.

What is regional contact?

What is metamorphism in geology?

Metamorphism is a process of mineral assemblage and texture variation that results from the physical-chemical changes of solid rocks, caused by factors such as crust movement, magma activity, or thermal fluid change in the earth. From: Unconventional Petroleum Geology, 2013.

Which are the three zones of metamorphism?

Commonly we call then low, middle, and high grade metamorphism, but geologically they are the greenschist facies, amphibolite facies, and granulite facies. Everything in Barrovian metamorphism is in reference to these three facies, or conditions of metamorphism.

What are the two classifications of metamorphic?

Metamorphic rocks are broadly classified as foliated or non-foliated.

Why does regional metamorphism usually occur within the continental crust?

Most regional metamorphism takes place within continental crust. … Because this metamorphism takes place at temperatures well below the temperature at which the rock originally formed (~1200°C), it is known as retrograde metamorphism.

What type of metamorphism occurs in subduction zones?

Subduction zone metamorphism is characterized by a low temperature, high-ultrahigh pressure metamorphic path through the zeolite, prehnite-pumpellyite, blueschist, and eclogite facies stability zones of subducted oceanic crust.

Where does regional metamorphism occur quizlet?

Regional metamorphism occurs over wide areas and results from both pressure and temperature generated at convergent plate margins during subduction and continental collision. When oceanic and continental plates collide, high pressure is produced as the oceanic plate is subducted.

What is a metamorphic rock quizlet?

Define Metamorphic rock. are rocks changed from one form to another by intense heat intense pressure or the action of watery hot fluids.

What is contact metamorphism quizlet?

Contact metamorphism occurs when the country rock is affected by heat from an intrusion. Igneous bodies are intrude at relatively shallow depth so contact metamorphism is described as high temperature, low pressure metamorphism. High temperatures lead to recrystallised, unfoliated rocks in an aureole. Metamorphic Grade.

What minerals form from regional metamorphism?

Typical mineral assemblages include heulandite, analcite, quartz with complex clay minerals (montmorillonite), micaceous phases such as chlorite and celadonite, and the potassium feldspar adularia. At higher grades of metamorphism, the zeolite laumonite and the feldspar albite dominate the mineral assemblage.

How are rocks altered by regional metamorphism?

Regional metamorphism takes place under high temperature and pressure conditions that may extend over large areas. Regional metamorphism results in intense alteration of the mineralogy and texture of rocks, usually to the point where original sedimentary structures are destroyed.