1) Shanghe Area
商河地区
1.
The igneous rock which is distributied in the first member of Shahejie Formition in Shanghe Area is pyroclastics formed by several stages of volcanic eruption.
商河地区沙一段火成岩由多期水下火山喷发作用形成,岩石类型主要有火山角砾岩、凝灰岩、沉积火山碎屑岩和火山碎屑沉积岩类。
2.
Many layers of carbonate rock deposition existed in the first member of Shahejie formation in Shanghe area of Huimin sag.
惠民凹陷商河地区沙一段发育多层碳酸盐岩沉积。
2) huimin shanghe area
惠民商河地区
1.
Apply the previous experience and outcome to huimin shanghe area of Jiyang depression.
总结了前人的经验和教训,并把前人的经验和研究成果应用到济阳坳陷惠民商河地区,从火成岩分布规律、油源条件、储集层条件、构造条件四个方面总结了该地区火成岩成藏规律,并建立了该地区的火成岩成藏模式。
4) Hetao land agent
河套地商
5) Hechi Region
河池地区
1.
Evaluation of agro-ecosystems in Karst Areas—A case study of Hechi Region of Guangxi Province;
西南喀斯特区域农业生态系统评价研究——以广西河池地区为例
6) Hehuang areas
河湟地区
1.
The Qing Dynasty was a period of the sustained development of agriculture in Hehuang areas,a vast amount of land in rivers and creeks had been cultivated in the Qianglong period of Qing Dynasty.
清代是河湟地区农业持续发展时期,土地垦殖的速度加快,到乾隆年间位于河川谷地的农田均已开垦出来,但随着人口增加,土地的开垦逐渐伸延及山坡地。
2.
This article probes mainly into the characteristics and cause for feudalization of Hehuang areas in Han Dyasty,and deems that carrying out the leap from the late period of primitive society to the feudal society in Hehuang areas in Han Dynasty depends on the special historical conditions and geographical circumstances at that time.
文章主要对汉代河湟地区封建化的原因和特点进行了分析 ,认为汉代河湟地区之所以实现了从原始社会晚期跨入封建社会的飞跃 ,主要取决于当时这一地区所处的特殊历史条件和地理环境。
补充资料：里下河地区
江苏省中部大体上以里运河、通扬运河、串场河和苏北灌溉总渠为四边的低洼地区。地势四周高，中部低，似锅状。河网密，湖泊多。原来洪涝严重。建国后兴修水利，已成为商品粮基地。
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