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励心逸 《少年文艺(南京)》2008,(Z1):60-61
清澈见底的小河、古老的石拱桥、五色花岗石铺成的小道、充满民族风韵的建筑物、高高挂着的一串串大红灯笼、来来往往的人群……啊!我们终于来到了美丽的丽江古城。早上,我们随着潺潺流动的小溪,漫步在古城的商业街,展现在眼前的好像是一幅古老、典雅、幽静的水墨画,却比画真实,触手可及。一座座石桥如彩虹般横跨在小溪上,清澈的流水中,不时有红色的小鱼在水草丛中 相似文献
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LI Zi-long CHEN Han-lin YANG Shu-feng TAINOSHO Yoshiaki SHIRAISHI Kazuyuki OWADA Masaaki 《浙江大学学报(A卷英文版)》2007,8(7):1004-1010
Fluids (fluorine, chlorine, and OH) in accessory minerals (apatite, titanite and allanite) of Pan-African granitoids(Group-Ⅰ granitoids, Group-Ⅱ granitoids and Mefjell Plutonic Complex) from the Sor Rondane Mountains, East Antarctica were precisely measured by an electronic microprobe analyzer in this study. Apatites in the granites have commonly high fluorine contents. However, fluorine contents from the Group-Ⅰ, Group-Ⅱ granitoids and Mefjell Plutonic Complex (MPC) are of important variation, which F contents (3.21~7.20 wt%) in apatite from the Group-Ⅱ granitoids are much higher than those from the Group-Ⅰ granitoids (1.22~3.60 wt%) and the MPC (3.21~4.11 wt%). Titanite in the MPC has a low fluorine content (0.23~0.50 wt%), being less than those in the Group-Ⅰ granitoids (2.28 wt%) and Group-Ⅱ granitoids (1.85~2.78 wt%). Fluorine in allanite in the Group-Ⅱ granitoids seems to have much lower contents than those from the Group-Ⅰ granitoids and the MPC. Higher fluorine contents in the titanite from the Group-Ⅱ granitoids may be mainly controlled by late-magmatic fluid-rock interaction processes associated with melt, but may not be indicative of original magma contents based on its petrographic feature. Due to very lower chlorine contents from all of accessory minerals, the authors suggest that titanite and apatite with higher fluorine contents in the Group-Ⅱ granitoids have much lower H2O (OH) contents compared with those in the Group-Ⅰ granitoids according to the partition among (F, Cl, OH).Fluorine contents in whole-rock samples show a variation from the higher in the Group-Ⅰ granitoids to the lower in the Group-Ⅱ granitoids and the MPC, which are consistent with the changes of those from the biotite and hornblende as well as fluorite occurred in the Group-Ⅰ granitoids reported previously. Based on the above study of fluorine in accessory minerals and combined with the previous fluorine contents from biotites and hornblendes, the authors suggest that apatites and titanites with higher F contents in the Group-Ⅱ granitoids and the MPC may not be an indicator of higher fluorine contents in whole-rock, which reflect fluorine contents in magma sources and/or late-thermal activity. Higher fluorine contents in apatite, titanite and allanite may be an additional evidence of A-type affinity. 相似文献
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关于科普类文章的教学,许多教师会走进这样两大误区:第一,在课堂中大讲特讲科学发展的知识,不走进课文,不进行语言训练,将语文课上成了科学课,这样的课堂就遮挡了语文教学的本来面目——是"读文",而不是"科普"。第二,有的老师认为科普类文章的教学,就得讲说明方法,否则就没有紧扣文本的特点,就没有完成教学目标。这样一来,文本叙述简洁的语言,就被直接得只剩下"举例子、列数字、作比较"等说明方法 相似文献
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