laccolith formation
岩床形成
laccolith intrusion
岩床侵入
laccolith structure
岩床结构
laccolith geology
岩床地质
laccolith feature
岩床特征
laccolith rock
岩床岩石
laccolith study
岩床研究
laccolith example
岩床示例
laccolith type
岩床类型
laccolith occurrence
岩床出现
a laccolith forms when magma intrudes between layers of rock.
当岩浆介入岩石层之间时,会形成一个岩盖。
the study of laccoliths can reveal important geological history.
对岩盖的研究可以揭示重要的地质历史。
laccoliths are often associated with volcanic activity.
岩盖通常与火山活动有关。
geologists often examine laccoliths to understand magma movement.
地质学家经常研究岩盖以了解岩浆的运动。
the formation of a laccolith can create unique landforms.
岩盖的形成可以创造独特的地貌。
we found a large laccolith during our field study.
在我们的实地研究中发现了一个大型岩盖。
understanding laccoliths helps in predicting volcanic eruptions.
理解岩盖有助于预测火山喷发。
laccoliths can vary greatly in size and shape.
岩盖的大小和形状可以有很大差异。
many national parks feature impressive laccolith formations.
许多国家公园展示了令人印象深刻的岩盖形成。
scientists are researching the relationship between laccoliths and earthquakes.
科学家们正在研究岩盖与地震之间的关系。
laccolith formation
岩床形成
laccolith intrusion
岩床侵入
laccolith structure
岩床结构
laccolith geology
岩床地质
laccolith feature
岩床特征
laccolith rock
岩床岩石
laccolith study
岩床研究
laccolith example
岩床示例
laccolith type
岩床类型
laccolith occurrence
岩床出现
a laccolith forms when magma intrudes between layers of rock.
当岩浆介入岩石层之间时,会形成一个岩盖。
the study of laccoliths can reveal important geological history.
对岩盖的研究可以揭示重要的地质历史。
laccoliths are often associated with volcanic activity.
岩盖通常与火山活动有关。
geologists often examine laccoliths to understand magma movement.
地质学家经常研究岩盖以了解岩浆的运动。
the formation of a laccolith can create unique landforms.
岩盖的形成可以创造独特的地貌。
we found a large laccolith during our field study.
在我们的实地研究中发现了一个大型岩盖。
understanding laccoliths helps in predicting volcanic eruptions.
理解岩盖有助于预测火山喷发。
laccoliths can vary greatly in size and shape.
岩盖的大小和形状可以有很大差异。
many national parks feature impressive laccolith formations.
许多国家公园展示了令人印象深刻的岩盖形成。
scientists are researching the relationship between laccoliths and earthquakes.
科学家们正在研究岩盖与地震之间的关系。
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