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dì yuán shuō
以大地为球形的学说。相传为古希腊人亚诺芝曼德、毕达哥拉斯及挨拉托色尼所首创。至16世纪初,葡萄牙人麦哲伦绕地球一周,18世纪英国科学家牛顿以力学理论证明太阳系中各行星之形状,此学说遂为世人所公认。
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