1) Chengdao area
埕岛海区
1.
Chengdao area, northeast of Huanghe subaqueous delta is typically characterized by the geologic hazards , which will threaten the safety of the offshore engineering such as drilling well and drilling oil platform, man-made island and oil transporting pipelines.
埕岛海区地处黄河三角洲东北角,是海底地质灾害频发地带。
2) Chengdao Shenghai area
埕岛-胜海地区
3) Chengdao sea area
埕岛海域
1.
The Shengli Chengdao sea area is located in the depositional system of the Yellow River delta, the original delta system has been eroded under the actions of wave and current, and the soft sediments are distributed on part of sea bottom.
胜利埕岛海域位于复杂的黄河三角洲沉积体系中。
2.
A method,named as Recursive Method,has been applied for the calculation of submarine pipeline settlement in the Chengdao sea area of Shengli Oil Field,and the results from this method were compared with those from the Japan Code Method and the Limit Method,which are the two commonly used methods at the present.
提出一种海底管道沉降计算方法——递推法,应用到胜利油田埕岛海域海底管道沉降计算中,并将计算结果与目前常用的日本规范法和极限法进行比较。
4) Chengdao Region
埕岛地区
1.
The paper applies seismic and well-log data to the study of the Mesozoic structural characteristics and tectonic evolution in Chengdao Region.
应用钻井资料、地震资料并结合区域资料,对渤海湾南部埕岛地区的中生代构造特征及演化进行了研究。
2.
Two groups of Mesozoic and Paleozoic fractures developed in Chengdao Region,one strike is northeast 30°,the other is nearly east west.
埕岛地区中、古生界发育两组裂缝 :一组走向为NE30° ,另一组为近EW走向。
5) Chengdao area
埕岛地区
1.
Characteristics of migration pathway system in Chengdao area;
埕岛地区输导体系发育特征
2.
Development characteristic of Mesozoic and Cenozoic faults and its control over deposition in Chengdao area;
埕岛地区中生代和新生代断层发育特征及其对沉积的控制作用
3.
Analysis of geochemical characteristics and oil sources in Chengdao area,Shengli petroliferous district.;
胜利油区埕岛地区原油地球化学特征与油源分析
6) Chengbei sea area
埕北海区
1.
Based on the multi -period water depth data of the Huanghe Delta Chengbei sea area, the amount and area of sediment erosion and accumulation are calculated and the corresponding contour diagrams and stereograms are plotted for different phases through computer - based method, and the regularity and characteristics of sediment erosion and accumulation are studied.
利用多期水深数据,对黄河三角洲埕北海区的泥沙冲淤量及冲淤面积进行分时段计算,绘制相应的冲淤等值线图和冲淤立体图。
补充资料：定海区
浙江省舟山市人民政府驻地、舟山群岛水陆交通枢纽。位于省境东北，由舟山岛中、 西部及金塘、 册子、长白等117座岛屿组成。陆域面积535平方公里，其中山地占43％。人口31万余。夏商为越东南境，周时属越周的句东,又称甬东。唐开元二十六年(738)置翁山县，北宋改称昌国县（当时船只靠山而泊，故别名舟山）。元升昌国州，明初复县。清康熙二十六年(1687)始称定海县。1987年撤县设区。岛上地势起伏,滨海平原狭小,农作以水稻、甘薯为主。附近海域盛产大、小黄鱼、带鱼和墨鱼。近年来大、小黄鱼产量大减。定海城关镇人口近5万。商业繁荣,工业有造船修船、水产品加工等部门。港口宽阔,有千吨级码头,班轮直达上海、宁波及舟山市的主要岛屿。杭州─沈家门公路上的海上汽车轮渡已建成。名胜古迹有晋"祖印寺"、明"同归域"、清"三忠祠"及舟山革命烈士陵园。
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