The Anyuan-Xunwu area in Jiangxi, located in the mantle-uplifted area, is a hot doming extensional structure district, called Anyuan hot doming.
江西省安远-寻乌地区位于地幔隆起部位，为一热隆伸展构造区，称安远热隆。
The Tan Lu fault zone turned into a huge extensional structure during Late Cretaceous to Eogene, leading to a series of development of fault bounded basins.
晚白垩世早第三纪郯庐断裂带转变成巨型的伸展构造，普遍控制发育了断陷盆地。
The Tan Lu fault zone turned into a huge extensional structure during Late Cretaceous to Eogene, leading to a series of development of fault bounded basins.
晚白垩世早第三纪郯庐断裂带转变成巨型的伸展构造，普遍控制发育了断陷盆地。
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