论文部分内容阅读
在新疆阿克苏柯坪—巴楚314国道路碑标记1 145.5 km处二号硫磺沟发现了一种现代的特殊地质现象:这种现象的构造形态主要呈圆台状,其上部是块状灰岩或胶结程度较高的泥砾,下部由地层风化剥蚀物组成,它们像是从地面长出来的竹笋,所以就把这种特殊的地质现象称为泥笋。到目前为止,在该地区还没有人报道过这种现象。它是一种有成因和演变意义的地质现象。通过对其形成条件及过程的研究得出这种特殊地质现象的发育环境是水文过程和气候演变的记录。所以,对它们的研究,对研究当地现代气候具有一定意义。
A special geological phenomenon has been found in No.2 sulfur channel at the mark of 145.5 km from the Keping-Bachu 314 national road mark in Aksu, Xinjiang. The tectonic morphology of this phenomenon is mainly in the shape of a truncated cone with the upper part being massive limestone or The higher degree of cementation of mud, the lower part of the formation of weathering and erosion of the composition, they are like the emergence of bamboo shoots from the ground, so put this special geological phenomenon called mud shoots. So far, no one has reported this phenomenon in the area. It is a geological phenomenon that causes and evolves meaningfully. Through the study of its formation conditions and process, it is concluded that the developmental environment of this special geological phenomenon is a record of hydrological processes and climate evolution. Therefore, the research on them is of some significance to the study of the local modern climate.