1) Tanlu strike-slip fault zone
郯庐走滑断裂带
1.
Tanlu strike-slip fault zone had experienced several phases of movement,exerting strong influence and control upon the hydrocarbon pooling within the 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。
2) Tan-Lu fault belt
郯-庐断裂带
1.
Using aeromagnetic data in combination with other geophysical information,the authors studied basic characteristics of the Tan-Lu fault belt in the Bohai Sea area,discussed detailed features of the tectonic line passing through the sea area,and investigated the control role of the fault belt over the Bohai Sea Basin as well as the relationship between this fault belt and the oil and gas fields.
利用航磁资料并结合其他地球物理资料,研究了渤海海域郯-庐断裂带的基本特征,讨论了构造线通过海域细节特征,探讨了该断裂对渤海湾盆地的控制作用,以及新生代期间与油气田的关系,指出渤海湾地区是寻找火山岩型油气藏的有利场所,并可期待在郯-庐断裂主断裂一线及旁侧具备生油的范围内寻找新近系油气田。
3) Tanlu fault zone
郯庐断裂带
1.
Dynamics of the evolution of the Tanlu fault zone:A multiforce-in-multiphase acting model;
郯庐断裂带演化动力学——多力源多时期分段作用模式
2.
An attempt to apply three geothermometers in the interpretation of low-temperature mylonites in the southern segment of the Tanlu fault zone;
地质温度计在郯庐断裂带南段低温糜棱岩中的尝试
3.
Fault activities and hydrocarbon migration and accumulation during the Neotectonic period in the Bozhong-Bonan segment of the Tanlu fault zone
郯庐断裂带渤中-渤南段新构造运动期断层活动与油气运聚
4) Tan-Lu fault zone
郯庐断裂带
1.
Deep structures of the Bohai part of the Tan-Lu fault zone and their dynamic implications;
郯庐断裂带渤海段的深部构造与动力学意义
2.
Foreland sedimentation evidence of syn-orogenic motion of the Tan-Lu fault zone;
郯庐断裂带同造山期活动的前陆沉积证据
3.
Tectonic characteristics and evolution of the Tan-Lu fault zone in the Xiwei area,Feidong County,Anhui Province;
安徽肥东西韦地区郯庐断裂带的构造特征与变形规律
5) Tancheng-Lujiang fault zone
郯庐断裂带
1.
The thermal gradient evolution histories of 120 wells during the Cenozoic time in six depressions,which located along the middle part of Tancheng-Lujiang Fault Zone,were modeled by using the vitrinite reflectance and apatite fission track data in this paper.
郯庐断裂带两侧分布众多的坳陷,其构造-热演化历史对于这些含油气坳陷的油气成藏起到重要的作用。
2.
Based on multi-period data of vertical deformation and geological tectonic background in Jiangsu-Shandong-Anhui area from 1953 to 1995,the features of recent crust movement in the area and the activity in Tancheng-Lujiang fault zone are studied.
根据苏鲁皖地区１９５３～１９９５年多期精密复测水准资料，以及地质地貌构造背景，研究了苏鲁皖地区的地壳垂直运动及郯庐断裂中南段现今的活动特征，获得如下结论：（１）横穿本区的郯庐断裂带的活动直接控制着本区的构造活动；（２）郯庐断裂的活动特征为张压交替；（３）约自１９５３年开始，苏鲁皖地区地壳运动的演化顺序为张→压→张→压；新的“压”性运动约始于１９９３年，目前正在加强；（４）郯庐断裂带近期运动性质为左旋走滑；（５）张、压运动并不处于同一方向上（彼此相差约４５°）。
6) the Tan Lu fault zone
郯庐断裂带
1.
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。
2.
With becoming young of the Cenozoic basalts from the middle southern segment of the Tan Lu fault zone, their alkali, the fractional degree of LREE/HREE and incompatible elements enrichment increase.
郯庐断裂带中南段新生代玄武岩随时代逐渐变新 ,碱性逐渐增强 ,轻、重稀土元素分离程度及不相容元素的富集程度也逐渐增强 ,Sr、Nd同位素组成越来越亏损。
补充资料：断裂带
亦称“断层带”。有主断层面及其两侧破碎岩块以及若干次级断层或破裂面组成的地带。在靠近主断层面附近发育有构造岩，以主断层面附近为轴线向两侧扩散，一般依次出现断层泥或糜棱岩、断层角砾岩、碎裂岩等，再向外即过渡为断层带以外的完整岩石。断层带的宽度以及带内岩石的破碎程度，决定于断层的规模、活动历史、活动方式和力学性质，从几米至几百米甚至上千米不等。一般压性活压扭性断层带比单纯剪切性质的断层带宽。在一些大型的断层带中，由于被后期不同方向的断层切错，和夹有一些未破碎的大型岩块，只是断层带的结构趋于复杂化，从而在近代的断层活动中容易形成运动的阻抗，是应力易于积累和发生地震的场所。
说明：补充资料仅用于学习参考，请勿用于其它任何用途。
参考词条