According to lots of field works, two phases of sinistral strike-slip ductile shear belts were found in the Tan-Lu fault zone.
大量的野外工作发现，郯庐断裂带存在早、晚两期韧性剪切带。
Depositional characteristics of the Hefei basin indicated a good coupling with evolution of the Tan-Lu fault zone to the east of the basin.
合肥盆地的沉积作用与其东缘的郯庐断裂带演化有着良好的耦合关系。
As an important part of the Tan-Lu fault zone, it has good consistency with the Tan-Lu fault zone in the structural characteristics and evolution.
作为郯庐断裂系的重要组成部分，与郯庐断裂带的构造特征和演化方面有着良好的一致关系。
The Hanling-Pianling strike-slip fault zone is an important fault zone of the east of Liaoning, and a secondary fault at the east wall of the Tan-Lu fault zone in China.
寒岭—偏岭平移断裂带位于辽宁东部，是中国东部郯庐断裂东盘的一个次级断裂。
The Tan-Lu fault zone experienced intense extensional activities during the Late Cretaceous to the Early Paleogene. Thus, faulted basins were developed along the fault zone.
郯庐断裂带于晚白垩世至早第三纪经历了强烈的伸 展活动，普遍控制发育了断陷盆 地。
Compared with the volcanic activities inner NCC, the volcanic activities on the Tan-Lu fault zone began earlier and have a comparatively long history, the magma source became shallower.
与华北克拉通内部同期岩浆相比，郯庐断裂带内的岩浆活动具有较早的开始时间和长期的活动历史，岩浆源区较浅。
Hefei basin, closely near to the west of Tan-lu fault, is a Mes-Cenozoic compound superposition basin. Its generation and evolution have a close relationship with the activities of Tan-lu fault zone.
合肥盆地是紧邻郯庐断裂带苏皖段西侧发育的一典型的中新生代复合叠加盆地，合肥盆地的成生、演化与郯庐断裂带的活动有着密切的联系。
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。
Mesozoic volcanic activities of the Tan Lu fault zone mainly appeared in Early Cretaceous and resulted in a set of volcanic rocks characterized by shoshonite series.
郯庐断裂带中生代火山活动主要发生在早白垩世，形成了一套以橄榄安粗岩系为主的火山岩。
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。
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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