salt diapir
盐岩穹隆
diapir formation
穹隆形成
diapir structure
穹隆结构
diapir activity
穹隆活动
diapir rise
穹隆上升
diapir model
穹隆模型
diapir flow
穹隆流动
diapir theory
穹隆理论
diapir edge
穹隆边缘
diapir dynamics
穹隆动力学
a diapir can form when less dense material rises through denser layers.
当较轻的物质穿过较密的层时，会形成一个岩盐穹。
geologists study diapirs to understand the movement of earth's crust.
地质学家研究岩盐穹以了解地壳的运动。
diapirs are often associated with oil and gas deposits.
岩盐穹通常与石油和天然气储藏有关。
in some regions, diapirs create unique geological formations.
在某些地区，岩盐穹创造了独特的地质构造。
the study of diapirs helps in predicting volcanic activity.
对岩盐穹的研究有助于预测火山活动。
diapirs can influence the landscape over millions of years.
岩盐穹可以在数百万年内影响地形。
scientists discovered a large diapir in the arctic region.
科学家在北极地区发现了一个大型岩盐穹。
understanding diapirs is crucial for natural resource exploration.
理解岩盐穹对自然资源勘探至关重要。
diapirs can also affect local ecosystems and biodiversity.
岩盐穹也可以影响当地生态系统和生物多样性。
research on diapirs reveals insights into earth's geological history.
对岩盐穹的研究揭示了地球地质历史的见解。
salt diapir
盐岩穹隆
diapir formation
穹隆形成
diapir structure
穹隆结构
diapir activity
穹隆活动
diapir rise
穹隆上升
diapir model
穹隆模型
diapir flow
穹隆流动
diapir theory
穹隆理论
diapir edge
穹隆边缘
diapir dynamics
穹隆动力学
a diapir can form when less dense material rises through denser layers.
当较轻的物质穿过较密的层时，会形成一个岩盐穹。
geologists study diapirs to understand the movement of earth's crust.
地质学家研究岩盐穹以了解地壳的运动。
diapirs are often associated with oil and gas deposits.
岩盐穹通常与石油和天然气储藏有关。
in some regions, diapirs create unique geological formations.
在某些地区，岩盐穹创造了独特的地质构造。
the study of diapirs helps in predicting volcanic activity.
对岩盐穹的研究有助于预测火山活动。
diapirs can influence the landscape over millions of years.
岩盐穹可以在数百万年内影响地形。
scientists discovered a large diapir in the arctic region.
科学家在北极地区发现了一个大型岩盐穹。
understanding diapirs is crucial for natural resource exploration.
理解岩盐穹对自然资源勘探至关重要。
diapirs can also affect local ecosystems and biodiversity.
岩盐穹也可以影响当地生态系统和生物多样性。
research on diapirs reveals insights into earth's geological history.
对岩盐穹的研究揭示了地球地质历史的见解。
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