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20世纪我国文学理论教材发展的四个时期
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作者 索松华 《中国大学教学》 CSSCI 2002年第6期41-44,共4页
如果从20年代算起的话,我国20世纪文学理论教材的发展已有80年历史,经历了一个从无到有,从少到多,内容不断充实,体系不断演变,质量不断提高的过程.对这一历史过程进行反思和明辨,将有助于我们进行当下的文学理论教材建设.本文拟将这一... 如果从20年代算起的话,我国20世纪文学理论教材的发展已有80年历史,经历了一个从无到有,从少到多,内容不断充实,体系不断演变,质量不断提高的过程.对这一历史过程进行反思和明辨,将有助于我们进行当下的文学理论教材建设.本文拟将这一过程划分为四个历史时期,分别加以阐释. 展开更多
关键词 20世纪 文学理论教材 中国 历史时 革新期 革创 高等教育
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Yunnan's Intent to Innovate
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作者 LIU HUANZHI 《China Today》 2007年第6期76-79,共4页
TOWARDS the end of last year, a Chinese magazine released a list of the country’s buzzwords of 2006. It was no surprise that "Innovation" ranked third. That year witnessed a nationwide campaign of sci-tech innova... TOWARDS the end of last year, a Chinese magazine released a list of the country’s buzzwords of 2006. It was no surprise that "Innovation" ranked third. That year witnessed a nationwide campaign of sci-tech innovation that reached unprecedented heat. And this time, the flames spread inland, to places like the frontier province of Yunnan. 展开更多
关键词 Yunnan Sci-tech Innovation nationwide campaign Long-term Development
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Transition of Quaternary glacial cyclicity in deep-sea records at Nansha,the South China Sea 被引量:37
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作者 汪品先 田军 成鑫荣 《Science China Earth Sciences》 SCIE EI CAS 2001年第10期926-933,共8页
High-resolution oxygen isotope records over the last 2249 ka (MIS 1-86) have been obtained from cores of the upper section (105.08 m) at ODP Site 1143 (water depth of 2772 m)drilled in the Nansha area, southern South ... High-resolution oxygen isotope records over the last 2249 ka (MIS 1-86) have been obtained from cores of the upper section (105.08 m) at ODP Site 1143 (water depth of 2772 m)drilled in the Nansha area, southern South China Sea. The sampling resolution is at about 2 ka intervals, resulting in one of the best oxygen isotope records over the global ocean. The oxygen isotope curves, displaying details in the Pleistocene glacial cycles, have revealed a nearly 300 ka long stage of transition from a predominant 40 ka to 100 ka periodicity. Therefore, the 'Mid-Pleistocene Revolution' should be considered as a process of transition rather than an abrupt change. Within the 100 ka glacial cycles, the changes in tropical sea surface water were found to lead those in high-latitude ice sheet. Our comparisons show that the ice sheet expansion and the glacial stage extension in the Northern Hemisphere with the 100 ka cycles must have been driven not by ice sheet itself, but by processes outside the high latitudes of the Northern Hemisphere. 展开更多
关键词 QUATERNARY glacial cycles Mid-Pleistocene Revolution oxygen isotope stages Nansha area
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