1) Gan-Hang uranium metallogenic belt
赣-杭铀成矿带
2) Gan-Hang Belt
赣杭带
1.
7) Ma and 105~98 Ma),each representing results of separate tectonic events,are recognized in the Gan-Hang Belt.
7)Ma)在赣杭带西端没有酸性岩出露,赣江断裂带附近的玄武岩浆来自亏损地幔,没有地壳物质混染,属于碱性玄武岩系列,属于板内拉张作用的产物。
3) Ganhang Tectonic Belt
赣杭构造带
1.
Prototype and Sedimentation of Red Basins along the Ganhang Tectonic Belt;
赣杭构造带红层盆地原型及其沉积作用
2.
This paper deals with the formation and the evolution of Mesozoic red sedimentary basins in the Ganhang Tectonic Belt,following the discussion on the formation and the evolution of Mesozoic volcanic basins in the same belt.
本文是在继讨论赣杭构造带中生代火山盆地的形成和演化之后，再对赣杭构造带中生代红色碎屑沉积盆地（简称赣杭带红盆）的形成和演化作一探讨。
4) Ganhang fault belt
赣杭断裂带
5) uranium metallogenetic areas(belts)
铀成矿区(带)
6) ganhang volcanic belt
赣杭火山岩带
补充资料：赣
| 赣 见江西省。 |
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