1) the Qinling-Dabie tectonic line
秦岭-大别构造线
1.
Based on the results of leveling data processing and the character of mineral,rock,stratum,and structure,we think the Qinling-Dabie tectonic line and Tanlu fault zone are two of the most important structures which control the tectonic movement in eastern China.
并结合精密水准数据及研究区内的矿物、岩石、地层及地质构造特征,本文认为由于秦岭-大别构造线和郯庐断裂带是控制中国东部大陆地块运动的两条主要构造线,在郯庐断裂以东,秦岭-大别构造线经郯庐断裂转换后向北平移到青岛-五莲一带。
3) Qinling-Dabie orogen
秦岭-大别造山带
1.
A geochemical study, on major, trace and earth elements, of post-collisional intermediate and acid volcanic rocks from the Qinling-Dabie orogen was carried out.
秦岭-大别造山带中、新生代中酸性火山岩的地球化学研究表明，该区中酸性火山岩是由幔源基性岩浆与壳源物质的混合物经过多种过程（部分熔融、分离结晶等）综合作用形成的。
4) East Qinling-Dabie orogenic belt
东秦岭-大别造山带
1.
Characteristics of overthrust structures on northern edge of East Qinling-Dabie orogenic belt and hydrocarbon potentials;
东秦岭-大别造山带北缘逆冲推覆构造特征及油气前景
5) Qinling Dabie orogenic belt
秦岭大别山造山带
1.
metamorphosed ultramafic and mafic blocks) in the mylonite or blastomylonite zones, which are parallel or subparallel to the Qinling Dabie orogenic belt.
平行或近平行分布于秦岭大别山造山带的一个巨型构造混杂岩带，由变质表壳岩块、中深地壳变质块体、壳幔过渡带岩块和幔源岩块与糜棱岩和变晶糜棱岩基质共同组成。
6) northern edge of East Qinling-Dabie orogenic belt
东秦岭-大别造山带北侧
1.
The double factors method for blocks evaluation and its application in the blocks of the northern edge of East Qinling-Dabie orogenic belt,China
区块评价双因素法及其在东秦岭-大别造山带北侧区块的应用
补充资料：线状构造
见构造。
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