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What is a tabular concordant intrusive structure?

A tabular concordant intrusive structure refers to a type of igneous intrusion where the orientation of the intrusive body is parallel to the existing layering or structures in the surrounding rock. This results in the intrusion appearing as a tabular or sheet-like feature that runs parallel to the rock layers. The intrusive body is typically discordant to the sedimentary or metamorphic layers but its orientation is concordant.


Intrusive igneous rock body that is tabular and concordant?

A sill is a type of intrusive igneous rock body that is tabular and concordant, meaning it is parallel to the layering of the surrounding rock. Sills are formed when magma is injected into existing rock layers and solidifies underground. They are often found in sedimentary rock formations.


Is an intrusive igneous rock body that is tabular and concordant parallel to adjacent sedimentary rocks?

This type of intrusive igneous rock body is called a sill. Sills are tabular igneous bodies that form parallel to the layering of existing sedimentary rocks. They are concordant, meaning they intrude along bedding planes without disrupting the original layering of the surrounding rocks.


A laccolith is an example of a?

A laccolith is an example of an igneous intrusion, which is a body of intrusive igneous rock that forms by magma uplifting and pushing overlying rock layers.


What is a tabular concordant pluton?

A tabular concordant pluton is a sill.A Sill is a flat concordant pluton. And a tabular means flat, like a table or tablet. Thus a sill is a tabular concordant pluton.In fact a the wikipedia article for "sill (geology)", as of the 01:33, 19 February 2009 update by Vsmith, read " a sill is a tabular pluton that has intruded between older layers of sedimentary rock, beds of volcanic lava or tuff, or even along the direction of foliation in metamorphic rock." - http://en.wikipedia.org/wiki/Sill_(geology)

Related Questions

What is an intrusive igneous rock body that is tabular and concordant.?

sill


What is a tabular concordant intrusive structure?

A tabular concordant intrusive structure refers to a type of igneous intrusion where the orientation of the intrusive body is parallel to the existing layering or structures in the surrounding rock. This results in the intrusion appearing as a tabular or sheet-like feature that runs parallel to the rock layers. The intrusive body is typically discordant to the sedimentary or metamorphic layers but its orientation is concordant.


Intrusive igneous rock body that is tabular and concordant?

A sill is a type of intrusive igneous rock body that is tabular and concordant, meaning it is parallel to the layering of the surrounding rock. Sills are formed when magma is injected into existing rock layers and solidifies underground. They are often found in sedimentary rock formations.


Is an intrusive igneous rock body that is tabular and concordant parallel to adjacent sedimentary rocks?

This type of intrusive igneous rock body is called a sill. Sills are tabular igneous bodies that form parallel to the layering of existing sedimentary rocks. They are concordant, meaning they intrude along bedding planes without disrupting the original layering of the surrounding rocks.


Which intrusive igneous body is typically tabular and concordant?

The intrusive igneous body that is typically tabular and concordant is known as a "sill." Sills form when magma intrudes between existing layers of rock, spreading horizontally and parallel to the bedding planes. This results in a flat, sheet-like structure that can vary in thickness and extent. Sills differ from dikes, which are discordant and cut across existing rock layers.


What is a concordant pluton that is the result of doming or arching?

An intrusive igneous body whose contacts are parallel to the bedding of the country rock. Also known as concordant injection; concordant pluton.


What is the geologic term for a tabular body of igneous rock that is parallel to the surrounding rock layers?

It's called a concordant igneous intrusion, or a sill.


What is the word sill?

a tabular body of intrusive igneous rock, ordinarily between beds of sedimentary rocks or layers of volcanic ejecta.


What are not examples of an intrusive igneous body?

Sills, dikes, and volcanic necks are not examples of an intrusive igneous body. These features are formed by igneous activity in the Earth's crust but are not considered intrusive bodies because they are typically narrow and tabular in shape, rather than larger and more massive like intrusive bodies such as batholiths or plutons.


A laccolith is an example of a?

A laccolith is an example of an igneous intrusion, which is a body of intrusive igneous rock that forms by magma uplifting and pushing overlying rock layers.


Is a stock a intrusive igneous body?

No it is not intrusive because of the difference in body heat and intrusive igneousStope is not an intrusive igneous body. apex


What is a tabular concordant pluton?

A tabular concordant pluton is a sill.A Sill is a flat concordant pluton. And a tabular means flat, like a table or tablet. Thus a sill is a tabular concordant pluton.In fact a the wikipedia article for "sill (geology)", as of the 01:33, 19 February 2009 update by Vsmith, read " a sill is a tabular pluton that has intruded between older layers of sedimentary rock, beds of volcanic lava or tuff, or even along the direction of foliation in metamorphic rock." - http://en.wikipedia.org/wiki/Sill_(geology)