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1)  Tanlu
郯庐
1.
the NEE Jiaodong high-ultra high pressure metamorphic belt,the NNE Tanlu high-ultra high pressure metamorphic belt and the SEE Dabie high-ultra high pressure metamorphic belt.
依据榴辉岩的总体展布方向、岩石特征、高压-超高压变质作用及退变质作用的温压条件,可划分为NEE向胶东高压-超高压变质带、NNE向郯庐高压-超高压变质带和SEE向大别高压-超高压变质带。
2.
The geothermal fields in East China are of the areal and zonal properties,in which the Tanlu fault zone is an active zone of high geotherm,being closely related to its tectonic portion and to the tectonic events since Indosinian movement.
中国东部地热场具有地域性或分带性的特点 ,其中郯庐断裂带是一高地热活动带 ,这与其所处的大地构造部位和印支运动以来的构造事件密切相关。
2)  Tan-Lu fault zone
郯庐断裂
1.
Mesozoic tectonic evolution history of the Tan-Lu fault zone, China: Advances and new understanding;
郯庐断裂带中生代构造演化史: 进展与新认识
2.
The sedimentary features and tectonic evolution of Hefei basin were mainly controlled by Dabieshan orogenic belt and the Tan-Lu fault zone.
结果显示中生代以来,合肥盆地沉积地层最厚超过万米,中上侏罗统为主要沉积地层;三维埋藏史揭示合肥盆地的中新生代沉积演化历史受大别造山带和郯庐断裂带的共同控制,盆地沉积中心的迁移与大别造山带和郯庐断裂的活动密切相关。
3.
Tan-Lu fault zone is active giant fracture zone in the east of China.
郯庐断裂带是我国东部一条古老而现今仍在活动的巨型断裂带,它经历了长期而复杂的演化历史,它的存在与发展直接影响到其两侧区域的环境地质条件。
3)  Tanlu Fault
郯庐断裂
1.
Dominating action of Tanlu Fault on hydrocarbon accumulation in eastern Bohai Sea area;
郯庐断裂对渤海海域东部油气成藏的控制作用
2.
North China block,Jiao-Liao-Korea block and Tanlu fault;
华北块体、胶辽朝块体与郯庐断裂
3.
A number of Meso-Cenozoic medium and large petroliferous basins in the peri-Pacific region in the eastern part of continental China are distributed on both sides of or inside the Tanlu fault.
中国大陆东部滨太平洋地区一系列中新生代大中型含油气盆地分布于郯庐断裂两侧或位于郯庐断裂带内,显然,这些含油气盆地的形成演化和分布与郯庐断裂带的发展演化密切相关。
4)  Tanlu fault zone
郯庐断裂
1.
A discussion on the diversities of the source rock and hydrocarbon-generating evolution in the adjacent depressions of the Tanlu fault zone in China;
郯庐断裂带两侧坳陷、烃源岩及成烃演化的差异性
5)  Tan-Lu fault
郯庐断裂
1.
Inversion mechanism of Meso-Cenozoic basins of southern Tan-Lu fault and its adjacent areas;
郯庐断裂带南段及邻区中、新生代盆地的反转机制
2.
Qingdong sag was shaped in Paleogene companied by Tan-Lu fault activity.
青东凹陷是新生代伴随郯庐断裂活动而形成的凹陷。
3.
When the Tan-Lu fault fulfilled a rapid transformation from ductile to brittle deformation domain at the end o.
郯庐断裂带是中生代华北与扬子板块的碰撞造山带的陆内转换断层,大规模左行韧性剪切位移牵引胶北太古宙穹隆(栖霞复背斜)逆时针旋扭隆升,并且形成三山岛-仓上、焦家-黄县和招远-平度(破头青)等弧形右行剪切带和混合花岗岩。
6)  Tancheng-Lujiang fault
郯庐断裂
补充资料:题桐庐谢逸人(一作题庐峰谢山人)江居
【诗文】:
少小高眠无一事,五侯勋盛欲如何。湖边倚杖寒吟苦,
石上横琴夜醉多。鸟自树梢随果落,人从窗外卸帆过。
由来朝市为真隐,可要栖身向薜萝?



【注释】:



【出处】:
全唐诗:卷650-32
说明:补充资料仅用于学习参考,请勿用于其它任何用途。
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