鲁西南平原,地势平坦,阔野千里。菏泽市位于鲁西南中部一京九铁路与新石铁路的交汇处,是华北重要的交通枢纽之一。荷泽市地处聊考断裂带南段东侧和菏泽断裂带的西段,根据区域地壳稳定性评价结果,属不稳定地区和次不稳定地区。地表为第四纪冲积粒状粘土、粉土等,第四系、第三系之下分布有侏罗系、二迭系、石炭系、奥陶系。因此菏泽市虽地处平原,却有着良好的地质开发情景。菏泽市地矿工作从无到有,已经逐步发展起来,但长期以来,地质工作程度有些偏低,很多具体工作没有真正开展起来,市区内的矿产资源并没有得到很好的开发利川。随着经济体制改革和对外开放的逐步深入,菏泽市经济正在迅速发展。就发展阶段而言,整个经济还处在工业化初始阶段。发达国家的经验表明,这一阶段是消耗能源即原材料最多的时期。因此,在今后相当长的时期内,菏泽市对矿产资源的需求将不断增 Southwest Plain, flat, Hurricane miles. Heze City is located in the central southwest of Shandong-Beijing-Kowloon Railway and the new stone railway interchange, is one of the important transport hub in North China. Heze City is located in the eastern section of the southern section of the fault zone and the western segment of the Heze fault zone. According to the regional crustal stability assessment results, it belongs to the unstable region and the sub-unstable region. The surface is Quaternary alluvial granular clay, silt and so on. The Quaternary and Tertiary are distributed with Jurassic, Permian, Carboniferous and Ordovician series. Therefore, Heze City, although located in the plains, but it has a good scene of geological development. Geological work in Heze City has been developed from scratch. However, for a long time, the degree of geological work has been somewhat low. Many concrete work has not really started. The mineral resources in urban areas have not been well developed. With the gradual deepening of economic reform and opening to the outside world, the economy of Heze City is rapidly developing. As far as the development stage is concerned, the economy as a whole is still in the initial stage of industrialization. The experience of developed countries shows that this stage is the period of consuming energy, that is, the largest amount of raw materials. Therefore, Heze City, the demand for mineral resources will continue to increase for a considerable period of time in the future