Tisch
The practice of mine geology not only improves the ability of integrating theory with practice, but also deepens the important content learned in class. Field practice is a powerful supplement and continuation of theoretical teaching. Through the connection between field observation and textbooks, we have deepened our understanding of some rocks, which can also be used in real life. The observation of geological structure not only better understood the formation of strata, but also realized the three-dimensional imagination in the classroom at that time, and no longer felt vague about some strata. The brain already has a picture of the stratum, so it is better to contact the boring knowledge and pictures in the textbook.
The two-day internship in mine geology is over, but I have learned a lot from it. From the field practice in these two days alone, it is not easy for geologists to find it. As college students majoring in mining engineering, it is conceivable that they may encounter difficulties in working in coal mines in the future, so they must be prepared for hardship now. Only in this way can we better adapt to the working environment, learn something and apply what we have learned. I would like to thank Mr. Yin Mingguang for his patient explanation and hard work during the internship. I hope to have this kind of internship in the future, which is very beneficial and necessary for us to master and consolidate knowledge.
In this internship, we learned in happiness, not only visited and browsed the beautiful scenery of mountains and rivers, but also increased our professional knowledge. So I hope the school can organize more practical internship activities. In the future, I will make full use of this internship opportunity to better understand and master what I have learned and strive for success!
extreme
Through this internship, I realized that the strata in this area were completely exposed. From the Mesozoic strata, except Cambrian, Ordovician, Triassic, Jurassic and Tertiary strata, other strata are well exposed. There are various types of rocks, including magmatic rocks, sedimentary rocks and metamorphic rocks. Magmatic activities in this area include plutonic intrusion, shallow intrusion and eruption. The rocks we see are basic rocks and acid rocks. As far as metamorphism and metamorphic rocks are concerned, metamorphism in this area is mainly regional metamorphism. The main metamorphic rocks are phyllite, marble and slate. Structurally, there are four folds and seven faults in this area. Two large faults almost divide this into three parts. From the perspective of regional development, this area has experienced many tectonic movements and formed four structural layers. Generally speaking, the tectonic movement in this area is strong.
After six days of practice, I learned a lot. Through the teacher's explanation, I learned a lot that I couldn't learn in class, including: how to judge the category and age of a stone by its color; How to distinguish the three major rocks; How to measure the direction of rocks and so on; In a word, after the internship, I have mastered the subject of engineering geology better and mastered the knowledge I have learned better.