3) Liyue basin
礼乐盆地
1.
Liyue basin is a large-size Mesozoic-Cenozoic superposed basin,which is located in the east of Nansha sea areas and characterized by special geological setting and huge thick Mesozoic strata,showing great difference from other basins of Nansha sea areas.
位于南沙东部海域的礼乐盆地是一大型的中、新生代叠置盆地,其特有的地质背景及巨厚的中生代地层显示了其与南沙海域其他新生代沉积盆地的差异。
4) Dinoseb
地乐酚
1.
Experimental study on dinoseb degradation in soils;
土壤中地乐酚降解的实验研究
2.
Sorption is one of the most important mechanisms deciding Dinoseb transport in soils.
吸附是决定除草剂地乐酚在土壤中迁移的重要机制之一。
5) Lile Basin
礼乐盆地
1.
Analysis of static geological elements of petroleum-bearing combinations in the Lile basin, northeastern Nansha;
南沙东北部海域礼乐盆地含油气组合静态地质要素分析
2.
In order to evaluate systematically the hydrocarbon-generation potential in Lile Basin and to discuss the source rock features of the basin and its dynamic evolution processes,a comprehensive evaluation research on the hydrocarbon-generation system characteristics of the basin was carried out by use of BMPES (basin modeling and petroleum evaluating system).
为了系统地评价礼乐盆地的生烃潜力 ,探讨盆地的烃源岩特征及其动态演化过程 ,文章采用BMPES盆地模拟与油气评价系统对盆地的生烃系统特征进行了综合评价研究 ,认为盆地主要发育Mz、E11 -E22 、E31 3套烃源岩 ,古新统—中始新统和中生界是盆地的主力烃源岩 ,其有机碳丰度在 0 。
3.
The Lile basin, located in the north of the Nansha block, is a complicated superposition basin,which underwent four tectonic phases.
通过对地震剖面、钻井及拖网采样资料的分析,认为礼乐盆地发育有海相的中、新生代地层,存在晚白垩世与晚渐新世两个区域性不整合面,将沉积层分为三套构造层:下构造层较厚,为中生代地层,表现为翘倾断块和宽缓背斜两种构造样式;中构造层较薄甚至局部缺失,为古新世-早渐新世充填的张裂期沉积,表现为半地堑构造样式;上构造层为晚渐新统至第四系沉积,充填区域沉降期海相地层,地层较为平稳。
6) lercanidipine
乐卡地平
1.
Effects of Lercanidipine on Vascular Endothelial Function in Spontaneously Hypertensive Rats with Atherosclerosis;
乐卡地平对原发性高血压大鼠动脉粥样硬化血管内皮功能的影响
2.
Progress in the synthesis of lercanidipine;
乐卡地平合成的研究进展
3.
Long-term effect and tolerability of lercanidipine in Chinese patienls with mild to moderate essential hypertension;
乐卡地平治疗轻中度高血压患者的长期降压疗效和耐受性
补充资料：乐地
1.快乐的境地。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条