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Lusi mud volcano, Indonesia

机译:印尼鲁斯泥火山

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摘要

Mud volcanoes are geological structures characterized by emission of argillaceous material on the land surface or under water. Usually, there is sufficient water and gas, which makes the sediment semiliquid and forces it up through the crustal openings as an outflowing mass of mud on the surface 1 . The formation of mud volcanoes is typically associated with geological settings where high sedimentation rates occur, for example, in compressional tectonic belts, submarine slopes and inverted back-arc basins.
机译:泥火山是地质结构,其特征是在土地表面或水下排放出泥质物质。通常,有足够的水和气体,这使沉积物成为半液体,并作为表面1上泥浆的流出物质,迫使其穿过地壳开口。泥火山的形成通常与高沉积速率的地质环境有关,例如在压缩构造带,海底斜坡和倒弧盆地中。

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