论文部分内容阅读
自1973年我国第一批考古样品的碳十四测年数据公布以来,考古年代学研究在我国已取得长足的进展。这里主要的成果依然来自碳十四测年,其次是不平衡铀系和古地磁测年方法。已有约40个年龄小于30万年的我国旧石器考古与古人类遗址测定了铀系年龄,而古地磁法则测定了更早的,包括周口店第一地点下部、兰田和元谋等遗址的年代。裂变径迹法和热释光法也提供了个别遗址的年代数据。近年来新发展的电子自旋共振法将使旧石器考古年代学,加
Since the publication of the carbon 14 dating data of the first batch of archeological samples in China in 1973, the archeological chronological research has made great strides in our country. The main results here are still from the carbon 14 dating, followed by the unbalanced uranium and paleomagnetic dating methods. About 40 ancient Chinese archaeologists and palaeontology sites aged less than 300,000 years have determined the age of uranium, whereas the paleomagnetic laws have determined the older ones, including the lower part of the first place of Zhoukoudian, the sites of Lantian and Yuanmou . Fission track and thermoluminescence methods also provide chronological data for individual sites. In recent years, the newly developed electron spin resonance method will make Paleolithic archeology chronology, plus