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Igneous Rocks

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Part of the book series: Encyclopedia of Earth Sciences Series ((EESS))

Synonym

Magmatic rocks

Definition

Rocks resulting from the solidification of molten or partially molten material, called magma, which is generated inside Earth’s crust.

Introduction

Igneous rocks are classified into two types according to the settings in which they were formed:

  • Plutonic or intrusive : formed deep inside the Earth’s crust by the slow cooling and solidification of magma, which results in crystalline materials that are usually coarse grained, such as granite, gabbro, syenite, and diorite. As they rise to the upper crust, they can fragment and incorporate blocks of the host rocks, called xenoliths.

  • Volcanic or extrusive : formed at the Earth’s surface, around volcanic vents, by the ejection of lava, which may be explosive or not. The cooling is usually too rapid for the formation of coarse-grained mineral crystals, and glassy or fine-grained crystalline materials result; examples include rhyolites and basalts.

Another type of volcanic rocks are pyroclastic rocks ,...

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References

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Correspondence to Maria Heloisa Barros de Oliveira Frascá .

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© 2017 Springer International Publishing AG

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de Oliveira Frascá, M.H.B., Del Lama, E.A. (2017). Igneous Rocks. In: Bobrowsky, P., Marker, B. (eds) Encyclopedia of Engineering Geology. Encyclopedia of Earth Sciences Series. Springer, Cham. https://doi.org/10.1007/978-3-319-12127-7_166-1

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  • DOI: https://doi.org/10.1007/978-3-319-12127-7_166-1

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  • Publisher Name: Springer, Cham

  • Print ISBN: 978-3-319-12127-7

  • Online ISBN: 978-3-319-12127-7

  • eBook Packages: Springer Reference Earth and Environm. ScienceReference Module Physical and Materials ScienceReference Module Earth and Environmental Sciences

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