the tan-lu fault 郯庐断裂
the tan lu fault zone 郯庐断裂带
the tan-lu fault zone 郯庐断裂带
the paleo-tan-lu fault 古郯庐断裂
Paleogeotherm indicates high thermal flow of the upper mantle below the Tan Lu fault zone.
古地温线特征表明，断裂带之下的上地幔具有高的大地热流值。
Three stages of Meso Cenozoic evolution in the Tan Lu fault zone were all associated with volcanic activities.
在郯庐断裂带中生代以来的三期演化中，都伴生了火山活动。
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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