1) Sino-Mongolian border
中蒙边界
1.
Mylonitic potassic granitoids from the Yagan metamorphic core complex on Sino-Mongolian border: a mark of transition from contractile to extensional tectonic regime;
中蒙边界亚干变质核杂岩糜棱状钾质花岗岩——早中生代收缩与伸展构造体制的转换标志
2) China-Mongolia border region
中蒙边界地区
1.
Structure,evolution and origin of Late Mesozoic extensional basins in the China-Mongolia border region;
中蒙边界地区晚中生代伸展盆地的结构、演化和成因
4) China-Mongolia border region
中蒙边境
1.
The China-Mongolia border region and its neighboring areas are located at the convergence zone of Siberian platform, Tarim plate and North China craton, and serve as one of the most important copper metallogenic provinces in the world.
依据金属矿床围岩岩性组合和成矿作用特征 ,将中蒙边境及邻区分布的斑岩铜矿床 (点 )划分为 3种类型 :①加里东期经典型斑岩铜矿床 (点 ) ;②海西期经典型和火山岩型斑岩铜矿床 ;③燕山期深成岩型和火山岩型斑岩铜矿床。
2.
According to the study on the porphyry copper deposits in China-Mongolia border region,the authors try to summarize and study the typical porphyry copper deposits in the Paleoasian metallogenic domain through geochemistry method.
依据前人对中蒙边境各典型斑岩型铜矿床的研究成果,对中蒙边境古亚洲洋成矿域内典型斑岩型铜矿床的含矿岩体进行了地球化学探讨,结果表明:1)区内岩石属于钙碱性-高钾钙碱性系列、低铝质岩石;2)岩石均呈现出轻稀土富集的右倾型模式,重稀土分布平坦,岩石矿化蚀变后出现明显的负Eu异常,同位素结果表明均来自地幔的部分熔融;3)区内矿床均形成于岛弧环境,矿床的形成具有多期、多源、多构造变化特征,是特定时期地壳演化阶段构造-岩浆-热液活动的产物。
5) Monte-Carlo boundary method
蒙特卡罗边界法
6) JinInner Mongolia area
晋蒙边界地区
补充资料：中蒙
1.中途昏暗。比喻中道衰微。
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