1) the northern mid-Yangtze
中扬子北缘
1.
It shows that the upper Triassic of the northern mid-Yangtze basin can be divided into four third-order sequences(TS1,TS2,TS3 and TS4),and further grouped into one second-order tectonic sequence.
应用沉积学和层序地层学的基本原理和方法,对中扬子北缘上三叠统4条实测露头剖面和1条测井剖面进行了详细的沉积相分析和层序地层划分,同时阐述了沉积相迁移规律、层序界面类型、层序发育特征及其控制因素。
2) north edge of the middle and lower Yangtze area
中下扬子北缘
1.
Using evidence weight method,the authors selected tectonic activities,hydrocarbon abundance and thickness of source rocks,level of reservoir,complexity of reservoir,degree of mineralization of formation water as the evidence layers to evaluate the favorable zones of lower Palaeozoic pools at the north edge of the middle and lower Yangtze area.
利用地质异常研究中的证据权重法,选择构造活动、烃源岩有机质丰度、烃源岩厚度、储层级别、储层复杂程度、盖层发育程度、地层水矿化度作为证据层,对中下扬子北缘下古生界油气成藏有利区带进行了评价。
3) the northern part of lower Yangtze area
下扬子北缘
1.
The Yangtze platform starts to dive to the Qinling platform during the late Permian and the northern part of lower Yangtze area accomplishes the tectonic environment conversion from extension to extrusion.
下扬子北缘主要受扬子板块、华北板块和秦岭微板块相互作用控制,自晚二叠世开始,扬子板块向北俯冲于秦岭微板块之下,构造环境由拉伸向挤压转换,于中三叠世形成下扬子北缘前陆盆地。
4) northern margin of Yangtze landmass
扬子陆块北缘
1.
Geological and geochemical characteristics of Mayuan Pb-Zn ore deposit on northern margin of Yangtze landmass;
扬子陆块北缘马元铅锌矿床地质和地球化学特征
5) northern margin of Yangtze platform
扬子地台北缘
1.
The foreland thrust belt in the northern margin of Yangtze platform is a united deformationunit.
扬子地台北缘前陆逆冲带由北向南逆冲，根带最前沿为城口～房县，襄樊～广济和嘉山～响水断裂。
6) northern margin of Yangtze craton
扬子克拉通北缘
1.
The systematic study of Rb Sr,Sm Nd and single zircon Pb evaporating dating methods, provides a set of Proterozoic date of chronology on the Beiba and Xixiang districts along the northern margin of Yangtze Craton.
报道和总结了近期陕西汉中碑坝和西乡地区重要地质体系统同位素年代研究成果，在重新厘定的年代学基础上，就扬子克拉通北缘同位素特征及其地质意义进行剖析，依据该区岩浆作用的上地幔源区性质及演化规律，提出了中、新元古代扬子克拉通北缘存在与现代板块运动类似的洋壳俯冲和壳幔再循环作用的同位素地球化学证
补充资料：北扬
北杨，汉语拼音（beiyang），为山东省潍坊市寒亭区开元街道办事处下辖的村。该村位于开元街道办事处西部，白浪河东岸。有277户，1160口人，1869亩耕地（2003年04月资料）。聚落呈长方形，面积约0.21平方公里。
据考，此村建于明代，明洪武初年，李姓由直隶枣强县迁居潍县城北老瓜村。后北迁一公里，在白流河岸向阳处定居。取村名为北阳。清代，李姓中有九世祖，名李君杨迁至潍东王伯村。为纪念东迁的世祖君杨，遂渐改村名为北杨。
此村以李姓居民居多。
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