the type of thin pluton thats cuts across preexisting layers of rocks is Dike.
A pluton that cuts across existing rock layers is known as a cross-cutting pluton. This occurs when magma intrudes into pre-existing rock formations and solidifies, creating an igneous body that disrupts the original stratigraphy. The principle of cross-cutting relationships in geology states that the features that cut across others are younger than the rocks they intersect. Examples of such plutons include dikes and stocks.
The term for a tabular igneous pluton that is oriented discordantly to the bedding surfaces of adjacent sedimentary rocks is called a "dike." Dikes are typically vertical or steeply inclined and cut across pre-existing rock layers, contrasting with sills, which are parallel to the bedding.
A pluton will generally have larger crystals compared to a dyke. Plutons form from magma that cools slowly deep underground, allowing time for larger crystal growth. In contrast, dykes are formed from magma that intrudes and solidifies quickly in fractures near the surface, resulting in smaller crystals. Therefore, the slower cooling process of plutons leads to more substantial crystal development.
The French word for "Pluto" is "Pluton".
A pluton is a large body of igneous rock which has formed underground as rising magma has cooled.
A pluton that cuts across existing rock layers is known as a cross-cutting pluton. This occurs when magma intrudes into pre-existing rock formations and solidifies, creating an igneous body that disrupts the original stratigraphy. The principle of cross-cutting relationships in geology states that the features that cut across others are younger than the rocks they intersect. Examples of such plutons include dikes and stocks.
A mushroom-shaped pluton with a round top and flat bottom is called a "laccolith." It forms when magma intrudes between layers of sedimentary rock, causing the overlying strata to bulge upward, creating a mushroom-like shape. Laccoliths are typically associated with volcanic activity and can vary in size.
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)
An intrusive igneous body whose contacts are parallel to the bedding of the country rock. Also known as concordant injection; concordant pluton.
The term for a tabular igneous pluton that is oriented discordantly to the bedding surfaces of adjacent sedimentary rocks is called a "dike." Dikes are typically vertical or steeply inclined and cut across pre-existing rock layers, contrasting with sills, which are parallel to the bedding.
A pluton will generally have larger crystals compared to a dyke. Plutons form from magma that cools slowly deep underground, allowing time for larger crystal growth. In contrast, dykes are formed from magma that intrudes and solidifies quickly in fractures near the surface, resulting in smaller crystals. Therefore, the slower cooling process of plutons leads to more substantial crystal development.
A layer of cooled magma is called a pluton. Plutons form when magma intrudes into the Earth's crust and cools slowly underground, forming large bodies of igneous rock such as granite. They are commonly found in mountainous regions.
plutons that thin in one direction as compared with other two dimensions.common ones are dykes.
The French word for "Pluto" is "Pluton".
Pluton word comes from a latin word ''pluto''
A tabular discordant pluton is a large igneous intrusion that cuts across existing rock layers in a horizontal or nearly horizontal orientation. This type of pluton is also known as a sheet intrusion due to its tabular shape and discordant nature where it disrupts the surrounding rock layers. Tabular discordant plutons are typically formed when magma is injected into the Earth's crust and spreads laterally to create a flat or sheet-like body of intrusive rock.
The main types of plutons are batholiths, stocks, laccoliths, dikes, and sills. Batholiths are large intrusions exposed over a large area, while stocks are smaller intrusions. Laccoliths are mushroom-shaped intrusions, dikes are tabular intrusions that cut across existing rock layers, and sills are tabular intrusions that parallel existing rock layers.