论文部分内容阅读
黄淮聚煤区系指鲁西、皖北和苏西北的广阔地带,东以郯庐断裂为界,南以肥中断裂为界,北至渤海,西至鲁、皖两省边界为界,是我国东部的一个重要聚煤区。其中尤以石炭二叠纪的煤发育最好,蕴藏量极为丰富,其聚煤规律的探讨,对于开发利用该地区丰富的煤炭资源,有着重要的意义。我们在华东区煤田预测的基础上,运用地壳波浪运动的理论,探讨了黄淮聚煤区的聚煤规律。由于我们对地壳波浪运动理论的学习还很肤浅,难免有不足与谬误处,敬请批评指正。
The Huanghuai Coal-gathering Area refers to the vast area of Luxi, North Anhui and Northwest of Suzhou. It is bordered by the Tanlu Fault in the east, and is divided by the Fatong Fault in the south. It borders on the Bohai Sea in the north and borders the Shandong and Anhui provinces in the west. An important coal gathering area in the east. The Carboniferous Permian, especially the best-developed coal with abundant reserves, is of great significance for exploiting and utilizing the abundant coal resources in this area. Based on the predictions of coalfields in East China, we used the theory of crustal wave motion to discuss the law of coal accumulation in the Huanghuai coal accumulation area. As we learn the theory of crustal wave motion is still superficial, it is inevitable that there are deficiencies and fallacies, please criticism correction.