东吴运动
- 网络dongwu movement
东吴运动-
东吴运动性质的厘定及其时空演变规律
Nature of the Dongwu Movement and Its Temporal and Spatial Evolution
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东吴运动后开始的印支期，区域应力条件发生变化。
In the Indosinian period , the conditions of regional stresses were changed .
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古岩溶作用的发生与黔桂运动、紫云运动、东吴运动等所形成的层序界面和低位体系域密切。
The occurrence of the palaeokarstification is closely associated with the sequence boundaries and lowstand systems tract created by the guizhou-guangxi , Ziyun and Dongwu movements .
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扬子西缘东吴伸展运动
Extensional Dongwu Movement in Western Margin of Yangtze Region