他咬上了牙，郯着水不管高低深浅的跑起来。
Gritting his teeth, he broke into a run in spite of the depth of the water.
郯庐断裂在两板块碰撞事件中起了主控作用。
The collision between the two plates is mainly controlled by Tancheng-Lujiang Fault Zone.
潍北盆地是发育于郯庐断裂带内的中、新生代盆地。
Weibei basin is a Mesozoic-Cenozoic basin developed in the Tanlu fault zone.
三叠纪，华南与华北克拉通碰撞，郯庐断裂带形成。
In the Triassic period, following the collision between North-China and South-China cratons, the Tanlu fault zone was formed.
辽河盆地是郯庐断裂系的组成部分，属大陆裂谷盆地。
Liaohe basin is a part of Tanlu rifting system, and it belongs to continental rift basin.
郯庐断裂带Q值分布表明，沂沭带介质强度的完整性较差。
Distribution of Q value of the Tanlu fracture zone shown that medium intensity of the Yinshu zone isn't complete.
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。
Three stages of Meso Cenozoic evolution in the Tan Lu fault zone were all associated with volcanic activities.
郯庐断裂东侧的现代构造应力场在区域上具有极大的稳定性。
The modern tectonic stress field on the eastern side of the Tanlu fault is regionally very stable.
济阳运动的成因，与郯庐断裂从左旋转向右旋的活动密切相关。
The origin of the Jiyang movement is closely related to the transformation of the Tanlu Fault Belt from sinistral to dextral movements.
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。
According to lots of field works, two phases of sinistral strike-slip ductile shear belts were found in the Tan-Lu fault zone.
笔者在郯庐断裂带中段及邻近地区新近测得了25个大地热流值。
In the paper, there are 25 new terrestrial heat flows of the mid-segment of the TanchengLujiang fault zone to be listed.
关于郯庐断裂的平移距离仍存在着较大的分歧与有待深入研究之处。
Divergent views exist as to the magnitude of displacement of the fault zone and more studies are needed.
郯庐韧—脆性剪切带是主要的导矿构造，其次级断裂是主要容矿场所。
The Tanlu ductile brittle shear zone is the major structure as passageway for ore fluid and its secondary faults are the main host.
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。
Depositional characteristics of the Hefei basin indicated a good coupling with evolution of the Tan-Lu fault zone to the east of the basin.
紧邻郯庐断裂带分布的山东昌乐新生代玄武岩含有丰富的辉石岩捕虏体。
Abundant pyroxenite xenoliths were found from the Cenozoic Changle basalts, an area distributing near the Tanlu fault zone.
合肥盆地是大别造山带和郯庐断裂带共同作用产生的中新生代残留盆地。
Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu Tancheng?
在此基础上，讨论了郯庐断裂带是否为巨大的左行平移断层或转换断层。
On that basis, the paper discusses whether the Tanlu fault is a gigantic sinistral strike-slip fault or a transform fault.
合肥盆地是大别造山带和郯庐断裂带共同作用产生的中新生代残留盆地。
Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu (TanchengLujiang) fault zone.
郯庐走滑断裂带经历了多期活动，影响和控制走滑断裂带内的油气成藏。
Tanlu strike-slip fault zone had experienced several phases of movement, exerting strong influence and control upon the hydrocarbon pooling within the zone.
孔子曾向郯子、苌弘、师襄、老聃学习。而郯子这些人，他们不如孔子贤能。
Confucius had ever learnt from Tanzi, Changhong, Shixiang, and Laodan, yet people like Yanzi were not sager than Confucius.
南华北盆地的形成演化主要受秦岭—大别造山带以及郯庐系断裂带活动的制约。
Formation and evolution of basins in the southern part of North China are mainly controlled by activities of the Qinling-Dabie orogenic belt and the Tanlu fracture belt.
东濮拗陷位于河北平原地震带东南部，南邻河淮地震带，东与郯庐地震带相望。
Dongpu depression is located at the southeast of Pingyuan, Hebei, seismic belt, which is adjacent to Hehuai seismic belt in south and opposite to Tanlu seismic belt in east.
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.
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 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.
苏北-南黄海盆地与渤海湾盆地之间以鲁苏隆起相隔，对称分布于郯庐断裂两侧。
Subei-south Huanghai Basin and Bohai Bay Basin are distributed symmetrically on the side of Tanlu fault, and are separated by Lusu uplift.
南华北中南部中新生代盆地的形成演化主要受郯庐断裂带、大别造山带构造运动的制约。
The formation and evolution of the Meso-Cenozoic basins in the middle and southern part of southern North China was mainly controlled by the Tanlu fault system and the Dabie orogenic belt.
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。
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。
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.
渤中34 - 1浅层复杂断块区处于郯庐走滑断裂带内，受其影响和控制该区断层较发育。
Bozhong 34-1 complex fault-blocks zone is located in Yanlu strike-slip fault zone. Affected and controlled by the strike-slip fault zone, faults are developed.
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。
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.
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