晋宁运动

所以，晋宁运动是秦岭褶皱带漫长演化历史中的一个独立阶段。

Therefore , the Jinning movement is an independent stage in the long evolutionary history of the Qinling tectonic belt .

其全岩钐钕等时线年龄为828.6±27.9Ma，属晋宁运动产物。

It is the product of the Jinning movement with a whole rock Sm Nd isochron age of 828.6 ± 27.9 Ma .

中元古代末的神功运动表现强烈，青白口纪末的晋宁运动叠加褶皱明显。

The Shengong Movement in late Middle Proterozoic Era was strong and the superimposed fold of Junning Movement in late Qingbaikou Period was clear .

云南东部中上元古界的界线长期以来被置于晋宁运动所造成的不整合界面上。

The boundary between Middle and Upper Proterbzoic Erathem in East Yunnan was put on the unconformity interface led by the Jinning Movement for a long time .

北秦岭侵入岩带与同时代的蛇绿岩带有力地证明，北秦岭晋宁运动的构造体制是板块体制。

The intrusive rock belt and the ophiolite belt of the same time together demonstrate that the tectonic system of the North Qinling during the Jinning movement is plate tectonic system .

塔里木克拉通由塔北地块与塔南地块晋宁运动时拼合形成，基底构造线因地而异。

The Tarim Craton was created in the Jinningian orogeny by amalgamation of the North Tarim and South Tarim Blocks , with the basement structures being varied in its northern , middle and southern parts .