Abstract In October 2019, extremely impressive, fresh ruptures of the surface on the mud volcano of Mount Karabetova were discovered. The ruptures are represented by all the main kinematic types and demonstrate structural patterns that are characteristic of typically tectonic deformations. The total length of the ruptures from south to north is slightly less than 600 m. Repeated measurements showed high displacement rates ranging from 50 to 140 cm in three months. The fresh ruptures marked the further development of more ancient similar landforms. They are caused by the existing structure and can be interpreted as potentially hazardous objects on other mud volcanoes. It can be assumed that ruptures may result from increased pressure in the mud volcano chamber and can be a forecasting indication of an upcoming eruption.

中文翻译：

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塔曼半岛卡拉贝托娃山泥火山的近期构造破裂

摘要 2019 年 10 月，在卡拉别托娃山泥火山上发现了令人印象深刻的新地表破裂。破裂由所有主要运动学类型代表，并显示出典型构造变形特征的结构模式。南北断裂总长度略小于600 m。重复测量表明，三个月内发生了 50 至 140 厘米的高位移率。新的破裂标志着更古老的类似地貌的进一步发展。它们是由现有结构造成的，可以解释为其他泥火山上的潜在危险物体。可以假设破裂可能是由于泥火山室中的压力增加造成的，并且可以是即将爆发的预测迹象。