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1)  the Carboniferous period
礼县-麻沿河盆地
2)  Yanhe county
沿河县
1.
In recent years, in a view of the real situation of our country, Yanhe Tujia minority Autonomous County has made a scientific analysis to the present situation of industrial development present and the existence problems, proposed the development aims of Yanhe county industry an.
近年来,沿河土家族自治县立足县情,科学分析工业发展的现状及存在问题,提出了沿河县工业的发展目标,切实推进"兴工富县"发展战略。
2.
Take Yanhe county of Guizhou province as an example, Combined with the conversed factor and static structure factor analytical method, cultivated land production potential in Yanhe was 5688.
以贵州省典型山区农业县—沿河县作为研究对象,运用逆向因子修正法和静态因子分析法相结合的方法,计算出沿河县目前耕地的生产潜力为5688。
3)  Yanhe Autonomous County
沿河自治县
1.
Yanhe Autonomous County is one of the state-level Under-developed Counties.
作为一个典型的农业大县和国家级贫困县,沿河自治县必须加快农业产业化、山区工业化、城镇化和民营经济发展步伐,实现跨越式发展。
4)  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。
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)  Huangxian Basin
黄县盆地
1.
Maceral and geochemical characteristics of coal seam and oil shale in Huangxian Basin;
黄县盆地古近纪煤与油页岩的有机岩石学和地球化学特征及形成条件
补充资料:沿河
1.靠河地带。 2.顺着河道。
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