长沙沟,Changshagou
1)Changshagou长沙沟
1.Discovery of layered maflc-ultramafic intrusion in Changshagou, Altyn Tagh, and its geological implication:A pilot study on its petrological and geochemical characteristics.阿尔金山南缘长沙沟镁铁-超镁铁质层状杂岩体的发现与地质意义——岩石学和地球化学初步研究
2)Shagou沙沟
1.Characteristics of sulfide and silver minerals in Shagou silver-lead-zinc deposit of Xiong'er Shan, Henan Province, and their significance;河南熊耳山沙沟银铅锌矿床中硫化物和银矿物的矿物学特征及其意义
2.Geology and Ore-forming Fluid of Silver-Lead-Zinc Lode Deposit of Shagou, Western Henan Province;豫西沙沟脉状Ag-Pb-Zn矿床地质特征和成矿流体研究
3.Study on the Geologic Characteristics, Mineral Associations and Enrichment Regularity of Silver in the Silver-Lead-Zinc Ore Deposit of Shagou, Xiong'er Shan District, Henan Province;河南省熊耳山沙沟银铅锌矿床地质特征、矿物组合及银的富集规律研究
英文短句/例句

1.Water quality analysis of Tiechanggou-Shagou mine area of Xinjiang新疆铁厂沟-沙沟矿区水资源质量分析
2.DISCOVERY AND SIGNIFICANCE OF THE SHAGOU LEAD-ZINC DEPOSIT IN JIYUAN, HENAN PROVINCE河南省济源沙沟铅锌矿的发现及意义
3.When the tide had ebbed away the shells of many sea creatures were left on the sand.退潮后沙沟上留下了许多海洋生物的贝壳。
4.Sand and gravel may form bars within the channel.沙和砾石可以在沟槽内形成沙洲。
5.Research on Gully Erosion and Seabuckthorn Dam Sediment Intercepting Effect in Coarse-Sediment Producing Area of Yellow River Basin;黄河粗沙区沟道侵蚀与沙棘坝拦沙效应研究
6.Research for Sediment Storage-Release of Small Watershed in Loess Hilly-Gully Area黄土丘陵沟壑区沟道小流域泥沙存贮—释放初探
7.The stream had washed a channel in the sand.小河在沙地上冲出了一条沟.
8.The stream had washed (out) a channel in the sand.小河在沙地上冲出了一条沟。
9.The rain has washed channels in the sand.雨水在沙土上冲出一条条沟。
10.Shape optimization test of Dabeigou spillway reservior desilting tunnel大北沟水库泄洪排沙洞体型优化试验
11.Function of Series of Silt Arrester Dams to Detain Silt in Velley of Middle Reaches of the Yellow River--Taking Wangmau Valley as an Example黄河中游沟道流域淤地坝坝系拦沙作用分析——以王茂沟流域为例
12.Experimental Study on Evolution Process of Sheet Erosion-Rill Erosion-Gully Erosion and Sediment Yield Process on Loess Hillslope;黄土坡面片蚀—细沟侵蚀—切沟侵蚀演变与侵蚀产沙过程研究
13.Influence of Channel Networks on the Sediment Yield Under Variant Temporal and Spatial Scales:A Case Study of Chabagou Watershed不同时空尺度下沟壑对流域侵蚀产沙的影响——以黄土丘陵沟壑区岔巴沟流域为例
14.Walls and drains have been built to keep out sand and water.修筑了土墙和排水沟来防止风沙和水涝。
15.Stability of Tidal Creek System of Tiaozini Sand Shoals in the North of Jiangsu Coast苏北岸外条子泥沙洲潮沟系统的稳定性研究
16.Study on the Characteristics of Soil Erosion, Sediment Yield in Small Watershed in Loess Plateau Hilly, Gully Area by Using Tracers;黄土丘陵沟壑区小流域侵蚀产沙特征示踪研究
17.A Laboratory Study on Sediment-storage Effect of Check-dam Systems in the Small Watershed of Loess Plateau, China;黄土高原沟道坝系拦沙效应模型试验研究
18.Prediction Model of both Sediment Yield and Runoff Generation on Rill Erosion Zone over Loess Slope;黄土坡面细沟侵蚀带产流产沙模型研究
相关短句/例句

Shagou沙沟
1.Characteristics of sulfide and silver minerals in Shagou silver-lead-zinc deposit of Xiong'er Shan, Henan Province, and their significance;河南熊耳山沙沟银铅锌矿床中硫化物和银矿物的矿物学特征及其意义
2.Geology and Ore-forming Fluid of Silver-Lead-Zinc Lode Deposit of Shagou, Western Henan Province;豫西沙沟脉状Ag-Pb-Zn矿床地质特征和成矿流体研究
3.Study on the Geologic Characteristics, Mineral Associations and Enrichment Regularity of Silver in the Silver-Lead-Zinc Ore Deposit of Shagou, Xiong'er Shan District, Henan Province;河南省熊耳山沙沟银铅锌矿床地质特征、矿物组合及银的富集规律研究
3)rill length沟长
4)Shahegou bridge沙河沟桥
1.Shahegou bridge is a double arch bridge in Shandong Liaocheng city that firstly use anchor spray cement concrete to reinforce.沙河沟桥是山东聊城首座采用锚喷混凝土加固的双曲拱桥。
5)Shagou Formation沙沟组
1.regarded the "Gantang Formation" as not corresponding to the Shagou Formation but overlapping the Shagou beds.元谋盆地南部的甘棠村西剖面和沙沟村西剖面的岩性岩相及其所含生物化石性质,应属同时同相的地质体,沙沟组已具“甘棠组”的内涵,后者应予废除。
6)sediment trasportation in gully沟道输沙
延伸阅读

长沙长沙Changsha  长 沙刘社爱摄ChangshQ长沙(C hangsha)中国湖南省会,历史文化名城,军事重镇。位于湖南省东部,湘江下游。辖东、西、南、北、郊5区和长沙、望城、宁乡3县。面积6 810平方千米,人口423.64万,其中市区面积367平方千米,人口138.71万(1993)。 春秋战国为楚城邑。秦为长沙郡。西汉为长沙国都。东汉复为长沙郡。三国吴分民沙郡为湘东、湘西两郡。晋永嘉元年(307)复设长沙郡,并置湘州。隋开皇九年(589)撤湘州,改长沙郡为潭州,大业三年(607)复称民沙郡。唐初复为潭州。五代为楚国都,改潭州为长沙府。元为潭州路,后改为天临路。明复称长沙府。清康熙三年(1664)置湖南布政使司,为湖南省治。1933年设长沙市。1949年为省辖市。 地处湘东丘陵盆地区,地势南高北低。西依雪峰山,东靠连云山、罗霄山。市区海拔44米,西部是岳麓山、凤凰山、天马山等低山丘陵,其中岳麓山海拔295.4米,为市区制高点。东部有阿弥岭、杨家岭等一系列低岗,南部透遁着大片红色岗地,有金盆岭、黄土岭、东瓜山、妙高山、回龙山为屏障。北部是开阔的冲积平原。湘江由南向北纵贯市区,注人洞庭湖,枯水期水深1一15米,其西岸的靳江、伪水与东岸的浏阳河、捞刀河均为其支流,洪水期4-7月。属北亚热带湿润季风气候。年平均气温172℃,1月平均气温4.7℃,7月平均气温29.4℃。年平均降水量1 412毫米。矿产有硅砂、石灰石、煤、磷矿石、铁矿石等。长沙为湖南省重要的工业基地。以机械、化工、食品、纺织等工业为主。湘绣是中国四大名绣之一。农副业产品以水稻、生猪、鲜鱼_为主,盛产茶叶、柑桔、油菜籽等。是全省交通枢纽。北京一广州铁路纵贯,石门一长沙铁路正在建设中。公路干线通江西、湖北、四川、贵州、广东等省。湘江长沙港有泊位102个,长沙以下常年可航300吨船舶,长沙一株洲段常年可航15一300吨船舶。其支流中下游均可通航10~20吨船舶。湘江上建有两座公路大桥。民航通北京、上海、广州、成都、武汉、西安等城市。