摘要
科学理论的发展具有累积式发展模式和否证式发展模式,人类认识史上两类模式的交替促进了科学理论循环往复向前推进。科学家总是在某个科学共同体中从事科学活动,总是从属于某个范式。具有不同范式的科学共同体以不同的方式理解和解释着自然界,这就是科学本质特征。把握科学范式的社会性特征,认识不同范式的科学共同体的存在和发展,是一个国家、一个民族、一门学科、一个新兴专业成熟的表现。延续百年的地学三大争论是二大范式的科学共同体此起彼伏的学术争鸣,它推动了地学学科不断向前发展。
The development of scientific theory has two development models of accumulative development and negative proof development. The exchange of the two kinds of models in the history of human' s cognition promotes the different ways. This is te nature characteristic of science It is the mature expression of a country, anation, a branch of learning and a new speciality to understand thoroughly social characteristic of scientific model and recognize the existence and development of scientific community of different models. A hundred years' three big arguments of the two models' scientific community. It promotes the development of geology continuously.
关键词
累积式
否证式
科学共同体
科学范式
地学三大争论
accumulative form
negative proofform
scientific community
scientific model
three big arguments about geology