摘要
Approximately from B. C. 5000 to 4000, the broadly-spoken Yiluo-Zhengzhou district around Xiongshan Mountains (from northwest Hubei to southeast Shanxi), Taihang eastfoot area, and the southern and northern and northern Qinling Mountains, respectively scattered Xiawansgang first-period culture, Xiapanwang culture and Beishouling culture. They originated from Zhongyuan neolithic middleperiod culture, and went on to Zhongyuan neolithic late period culture. They obviously showed the cultural transition. We think that these three cultures have the same technical systems. habitat mode and burial customs. They represented an important turning period in the development of Zhongyuan historical cultrual tradition. Their mutual blend and their interaction with Beixin culture and Zhaobaogou culture caused the cultural transition from Zhongyuan neolihic middle period culture to Zhongyuan neolithic late period culture.
Approximately from B. C. 5000 to 4000, the broadly-spoken Yiluo-Zhengzhou district around Xiongshan Mountains (from northwest Hubei to southeast Shanxi), Taihang eastfoot area, and the southern and northern and northern Qinling Mountains, respectively scattered Xiawansgang first-period culture, Xiapanwang culture and Beishouling culture. They originated from Zhongyuan neolithic middleperiod culture, and went on to Zhongyuan neolithic late period culture. They obviously showed the cultural transition. We think that these three cultures have the same technical systems. habitat mode and burial customs. They represented an important turning period in the development of Zhongyuan historical cultrual tradition. Their mutual blend and their interaction with Beixin culture and Zhaobaogou culture caused the cultural transition from Zhongyuan neolihic middle period culture to Zhongyuan neolithic late period culture.
出处
《华夏考古》
1997年第4期47-59,113,共14页
Huaxia Archaeology
