In geology, a chonolith is a type of igneous rock intrusion (also known as pluton). Igneous rock intrusions are bodies of igneous rock that are formed by the crystallization of cooled magma below the Earth’s surface. These formations are termed intrusive rocks due the magma intruding rock layers but never reaching the earth’s surface. However, sometimes portions of plutons can become exposed at the Earth’s surface and thus the minerals can be observed since they are large enough. The different plutonic formations are named based on the different shapes that the cooled crystallized magma takes. However, all plutonic formations that have irregular shapes and do not share the same characteristics as other plutonic structures are termed chonoliths. Other plutonic structures that have specific
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| - Chonolith (en)
- Хонолит (ru)
- Хоноліти (uk)
- 畸形岩盘 (zh)
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| - Хонолит (от греч. κωνεύω — отливаю и греч. λίθος — камень) — интрузия неправильной формы, образовавшаяся в наиболее ослабленной зоне вмещающих пород, как бы заполняющая «пустоты» во вмещающей породе. Хонолиты обычно сложены гранитоидами. Зачастую хонолиты считают лакколитами неправильной формы. (ru)
- 畸形岩盘（英語：chonolith）是一種侵入火成岩。是由地下岩漿冷卻結晶形成的火成岩體。 由於岩漿侵入到岩層但未到達地球表面，所以被稱為侵入火成岩。 然而，有時部分岩體，經過構造作用被擡升，會暴露在地球表面，因此可以觀察到這些岩石中的礦物。侵入火成岩是根據冷卻後的結晶岩漿所表現的不同形狀而命名的。例如，岩脈，岩床，岩蓋等是具有特定形狀的侵入火成岩。但具有不規則形狀的侵入火成岩都被稱為畸形岩盘。 畸形岩盘一個獨特特徵是具有底板或基底，與其他類型的侵入火成岩不同。 (zh)
- Хоноліти (від грец. κωνεύω — відливаю і грец. λίθος — камінь) — інтрузивні тіла неправильної форми, що являють собою немов би магматичну відливку порожнини, яка виникла внаслідок переміщення блоків. (uk)
- In geology, a chonolith is a type of igneous rock intrusion (also known as pluton). Igneous rock intrusions are bodies of igneous rock that are formed by the crystallization of cooled magma below the Earth’s surface. These formations are termed intrusive rocks due the magma intruding rock layers but never reaching the earth’s surface. However, sometimes portions of plutons can become exposed at the Earth’s surface and thus the minerals can be observed since they are large enough. The different plutonic formations are named based on the different shapes that the cooled crystallized magma takes. However, all plutonic formations that have irregular shapes and do not share the same characteristics as other plutonic structures are termed chonoliths. Other plutonic structures that have specific (en)
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| - In geology, a chonolith is a type of igneous rock intrusion (also known as pluton). Igneous rock intrusions are bodies of igneous rock that are formed by the crystallization of cooled magma below the Earth’s surface. These formations are termed intrusive rocks due the magma intruding rock layers but never reaching the earth’s surface. However, sometimes portions of plutons can become exposed at the Earth’s surface and thus the minerals can be observed since they are large enough. The different plutonic formations are named based on the different shapes that the cooled crystallized magma takes. However, all plutonic formations that have irregular shapes and do not share the same characteristics as other plutonic structures are termed chonoliths. Other plutonic structures that have specific shapes include: dikes, sills, laccoliths and sheets. Another unique characteristic of chonoliths is that there is a floor or base present which is typically absent in other types of intrusions. (en)
- Хонолит (от греч. κωνεύω — отливаю и греч. λίθος — камень) — интрузия неправильной формы, образовавшаяся в наиболее ослабленной зоне вмещающих пород, как бы заполняющая «пустоты» во вмещающей породе. Хонолиты обычно сложены гранитоидами. Зачастую хонолиты считают лакколитами неправильной формы. (ru)
- 畸形岩盘（英語：chonolith）是一種侵入火成岩。是由地下岩漿冷卻結晶形成的火成岩體。 由於岩漿侵入到岩層但未到達地球表面，所以被稱為侵入火成岩。 然而，有時部分岩體，經過構造作用被擡升，會暴露在地球表面，因此可以觀察到這些岩石中的礦物。侵入火成岩是根據冷卻後的結晶岩漿所表現的不同形狀而命名的。例如，岩脈，岩床，岩蓋等是具有特定形狀的侵入火成岩。但具有不規則形狀的侵入火成岩都被稱為畸形岩盘。 畸形岩盘一個獨特特徵是具有底板或基底，與其他類型的侵入火成岩不同。 (zh)
- Хоноліти (від грец. κωνεύω — відливаю і грец. λίθος — камінь) — інтрузивні тіла неправильної форми, що являють собою немов би магматичну відливку порожнини, яка виникла внаслідок переміщення блоків. (uk)
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