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dbr:Load_cast
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荷重痕 重荷模 Load cast Belastungsmarke Load cast
rdfs:comment
Een load cast of sedimentary flame structure is een sedimentaire structuur, die wordt gevormd als sedimentlagen met ongelijke dichtheid over elkaar worden afgezet (bijvoorbeeld zandlaagjes over kleilaagjes). De dichtere zandlaag zakt als het ware weg in de lichtere kleilaag. Hierdoor ontstaan naar beneden convexe bollingen in het tussen de twee lagen. Anders gezegd zal de onderliggende laag puntvormige uitstulpingen naar boven vertonen. 荷重痕（かじゅうこん、load structure,load cast）とは、まだ凝固していない堆積層の上に、流動性のある堆積物が積もった時に、上層の堆積物の重みで下層の面（層理面）に不均等荷重がかかり、めりこむようになる2次的な堆積構造の総称をいう。 新しく堆積した単層（地層）の底面で見られる痕跡であることから、底痕のひとつとして分類される。 Load casts are bulges, lumps, and lobes that can form on the bedding planes that separate the layers of sedimentary rocks. The lumps "hang down" from the upper layer into the lower layer, and typically form with fairly equal spacing. These features form during soft-sediment deformation shortly after sediment burial, before the sediments lithify. They can be created when a denser layer of sediment is deposited on top of a less-dense sediment. This arrangement is gravitationally unstable, which encourages formation of a Rayleigh-Taylor instability if the sediment becomes liquefied (for instance, by an imposed earthquake shock). Once the sediments can flow, the instability creates the "hanging" lobes and knobs of the load casts as plumes of the denser sediment descend into the less-dense laye 重荷模（英語：load cast）是指在沉積岩層的層理面上形成的團塊狀凸起結構。團塊從上層沉積岩底部“垂下”到下層沉積岩頂部，通常具有相等的間距。這些結構是在沉積物尚未石化之前，造成的軟沉積物變形。當密度較大的沉積物層沉積在密度較小的沉積物之上時，就會產生。尤其當沉積物液化時（例如地震），流動的沉積物，能從著密度較大的沉積物下降到密度較小的層中，而造荷重痕. Eine Belastungsmarke ist eine Deformation im unverfestigten Sediment. Diese recht häufige Struktur an der Bankunterseite ist die Folge einer Rayleigh-Taylor-Instabilität. Die Instabilität tritt auf, wenn eine Schicht mit höherer Dichte über einer Schicht mit geringerer Dichte liegt und das Sediment sich unter dem Einfluss von Druck verflüssigt. Als Auslöser für die Verflüssigung werden Erdbeben angesehen.
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dbo:abstract
重荷模（英語：load cast）是指在沉積岩層的層理面上形成的團塊狀凸起結構。團塊從上層沉積岩底部“垂下”到下層沉積岩頂部，通常具有相等的間距。這些結構是在沉積物尚未石化之前，造成的軟沉積物變形。當密度較大的沉積物層沉積在密度較小的沉積物之上時，就會產生。尤其當沉積物液化時（例如地震），流動的沉積物，能從著密度較大的沉積物下降到密度較小的層中，而造荷重痕. Eine Belastungsmarke ist eine Deformation im unverfestigten Sediment. Diese recht häufige Struktur an der Bankunterseite ist die Folge einer Rayleigh-Taylor-Instabilität. Die Instabilität tritt auf, wenn eine Schicht mit höherer Dichte über einer Schicht mit geringerer Dichte liegt und das Sediment sich unter dem Einfluss von Druck verflüssigt. Als Auslöser für die Verflüssigung werden Erdbeben angesehen. Een load cast of sedimentary flame structure is een sedimentaire structuur, die wordt gevormd als sedimentlagen met ongelijke dichtheid over elkaar worden afgezet (bijvoorbeeld zandlaagjes over kleilaagjes). De dichtere zandlaag zakt als het ware weg in de lichtere kleilaag. Hierdoor ontstaan naar beneden convexe bollingen in het tussen de twee lagen. Anders gezegd zal de onderliggende laag puntvormige uitstulpingen naar boven vertonen. Load casts onderscheiden zich van doordat ze slechts naar één kant werken: als op de (dichtere) zandlaag weer een (lichtere) kleilaag ligt zal dit grensvlak gewoon recht blijven. Omdat ze zich altijd aan de onderkant van de dichtere laag bevinden zijn load casts goed geschikt als top-bottomcriterium in sedimentaire gesteenten. 荷重痕（かじゅうこん、load structure,load cast）とは、まだ凝固していない堆積層の上に、流動性のある堆積物が積もった時に、上層の堆積物の重みで下層の面（層理面）に不均等荷重がかかり、めりこむようになる2次的な堆積構造の総称をいう。 新しく堆積した単層（地層）の底面で見られる痕跡であることから、底痕のひとつとして分類される。 Load casts are bulges, lumps, and lobes that can form on the bedding planes that separate the layers of sedimentary rocks. The lumps "hang down" from the upper layer into the lower layer, and typically form with fairly equal spacing. These features form during soft-sediment deformation shortly after sediment burial, before the sediments lithify. They can be created when a denser layer of sediment is deposited on top of a less-dense sediment. This arrangement is gravitationally unstable, which encourages formation of a Rayleigh-Taylor instability if the sediment becomes liquefied (for instance, by an imposed earthquake shock). Once the sediments can flow, the instability creates the "hanging" lobes and knobs of the load casts as plumes of the denser sediment descend into the less-dense layer. Load casts are a common kind of sole marking.
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