A Preliminary Study was Conducted on the Mineralization Model and Seismic Genesis of the Deposit from the Perspective of Carbon Element Accumulation in Lake Sediments

Starting from the perspective of sedimentology, this article conducts in-depth investigation and reflection on the long-term sedimentation of lakes and their final formation of landforms. The process of lake sedimentation is a typical quantitative process, and quantitative change will inevitably lead to qualitative change. The various phenomena of lake sedimentation indicate that a large amount of organic matter and sediment from the surface will be deposited into the lake. During the long-term sedimentation of the lake, a large amount of carbon element will be accumulated inside the lake. At the same time, there is a large number of dead fish deposits inside the lake. From the entire sedimentation process of the lake, this is a common phenomenon that continuously accumulates surface organic matter in low-lying areas, Lake sedimentation is an important pathway for carbon element aggregation. Based on this quantitative phenomenon, in-depth analysis and exploration have been conducted on how carbon elements evolve within the basin. In the long-term exploration, the author has found that there is an extremely close mutual relationship between the formation of minerals in sedimentary areas and earthquakes.