摘要
我国地学研究思维形成一种单一的定势,即以归纳为主导的积累型研究方式为主流,并注重形象思维向抽象思维的连续过渡;但作为地学研究的基础——地质现象,却只是地史演化、变革过程中留下的残迹,这就大大限制了归纳思维内在力度的发挥。只有突破这种定势,强化以演绎为主导的研究方式,把握逻辑中断的契机,充分发挥非逻辑思维的作用,使研究思维由单维型向多维型,由传统型向开发型转化,方能增强我国地学研究思维的活力。
The research thinking in geology has been formeda single modIe in China, that is, the mode of accumulativetype is predominated by induction play an important partand the successive transformation is emphasised from theimages thinking to the abstract thinking. But the geologicalphenomenons which are the basis of all research reasoningare only the re1ic remains during the evolution of geologicalhistory, thus the ro1e which Is intrinsic strenth of the induc-tion thinking is restricted. The modle in research thinkingmust be breaked. the deduction thinking enhanced and theeffect of the non-Iogic thinking developed when logicbreakup befor the research thinking in geology can be pro-duced activity and transformed from single-dimension tomulti-dimension, trad itiona1 type to openi ng type.
出处
《编辑学报》
CSSCI
北大核心
1998年第2期65-67,共3页
Acta Editologica
关键词
地质学
研究思维
论文
评稿导向
Geology Research thinking Treatise Weigh-ing guide