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shale    音標拼音: [ʃ'el]
n. 頁巖,泥板巖

頁岩,泥板岩

shale
n 1: a sedimentary rock formed by the deposition of successive
layers of clay

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英文字典中文字典相關資料:
  • Shale - Wikipedia
    Shale is a fine-grained, clastic sedimentary rock formed from mud that is a mix of flakes of clay minerals (hydrous aluminium phyllosilicates, e g , kaolin, Al 2 Si 2 O 5 (OH) 4) and tiny fragments (silt -sized particles) of other minerals, especially quartz and calcite [1] Shale is characterized by its tendency to split into thin layers (laminae) less than one centimeter in thickness This
  • Shale | Formation, Composition, Sedimentary | Britannica
    Shale, any of a group of fine-grained, laminated sedimentary rocks consisting of silt- and clay-sized particles Shale is the most abundant of the sedimentary rocks, accounting for roughly 70 percent of this rock type in the crust of the Earth
  • Shale: Sedimentary Rock - Pictures, Definition More
    Shale is the most abundant sedimentary rock It is found in sedimentary basins worldwide
  • Shale: Composition, Formation, Uses, Types – Geology In
    Shale is the most common sedimentary rock type, constituting approximately 70% of exposed sedimentary rock on Earth Shale is characterized by its laminated structure, with thin, parallel layers resulting from the alignment of clay minerals during deposition
  • Shale: Formation, Composition, Properties, Varieties Fossils
    Below is a fully detailed and globally relevant overview of shale, including its formation, composition, properties, varieties, fossil content, economic significance, and geological role
  • Shale geology: characteristics, formation, uses - ZME Science
    Shale is a fine-grained sedimentary rock, composed mostly of clay particles and other minerals such as quartz and calcite It is formed of many thim mineral layers and is typically characterized
  • Shale: Formation, Types, Uses in Energy and Industry
    Shale is one of the most common types of sedimentary rock primarily composed of clay and silt particles It forms through the compaction of these fine particles over millions of years in calm environments such as deep ocean floors, lakes, and riverbeds





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