泥裂
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泥裂(英語:mud crack)是因泥質沉積物乾燥和收縮而形成的裂縫結構[1][2]。
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泥裂
Introduction
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延伸文章資訊
- 1mud crack - 泥裂痕,泥裂 - 國家教育研究院雙語詞彙
mud crack, 泥裂. 學術名詞 海洋地質學, mud crack, 泥裂痕,泥裂. 學術名詞 地球科學名詞, mud crack, 泥裂〔痕〕. 學術名詞 地理學名詞-兩岸地理學名詞
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發育在河灘、湖濱、海邊等泥質沉積物上,常可見到多角形的裂紋,稱為乾裂,又稱泥裂。在沉積岩層面上亦可見到乾裂,它是在沉積當時沉積物未固結即露出水面,受到日曬,水分 ...
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泥裂. 多角形的裂纹,又称干裂。 沉积物未固结即露出水面,受到日晒,水分蒸发,体积收缩而产生的。裂纹常具上宽下窄形态,其中被泥沙填充。 中文名泥裂.
- 4天天學普地|沉積構造——波痕、泥裂 - 每日頭條
指由岩層表面垂直向下的多邊形裂縫構造。裂縫在表層張開大,向下呈楔形尖滅。剛形成的泥裂其裂縫是空的;地質歷史中形成的 ...
- 5泥裂- 搜狗科学百科
泥裂是由泥质沉积物干燥收缩而形成的沉积结构。现代泥裂通常在河、湖、海等水体环境岸边或干涸的河床及干旱-半干旱区短期积水的低洼区出现,具有 ...