论文部分内容阅读
驻马店市地处黄淮平原西南部,系北亚热带向暖温带的过渡地区,地形以冲积平原为主,伏牛山余脉由西北向东南延伸,成为汉江与淮河水系的分水岭。境内古文化遗址众多,但由于以往未曾对早期遗址进行过正式发掘,长期以来,学术界对这一地界中原地
Zhumadian City is located in the southwest of the Huanghuai Plain, the transitional zone from the northern subtropics to the warm temperate zone. The terrain is dominated by alluvial plains. The foot of the Funiu Mountains extends from northwest to southeast and becomes the watershed between Han River and Huaihe River. The territory of many ancient cultural sites, but in the past have not been formally unearthed early ruins, for a long time, the academic community in this place of origin