The Meso Cenozoic basin in Anhui Henan border area is located in the south of Hefei basin.
豫皖交界地段中新生代盆地位于合肥盆地的南缘。
More and more attention is being paid to the marine hydrocarbon exploration in the Hefei Basin.
合肥盆地海相油气的勘探逐渐受到重视。
Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu Tancheng?
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。
The geochemical field of the Hefei Basin belongs to that of low background values, low moisture and inhomogeneity.
合肥盆地地球化学空间场属低背景、低湿度和非均匀场范畴。
Sediments in the Hefei basin to the north of the Dabie orogen are important records of unroofing history for the orogen.
位于大别造山带北部的合肥盆地，其中的沉积是造山带剥露历史的重要记录。
Hefei basin is a Mz-Cz residual basin generated from common action by Dabie orogen and Tanlu (TanchengLujiang) 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。
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。
On the basis of line coding practice in Hefei Basin, the paper presented scientific and reasonable design principle for line coding system.
本文在合肥盆地测线编码实践基础上，提出了科学、合理的测线编码系统设计原则；
The distribution pattern of Bouguer gravity anomalies in Hefei basin has been described in detail, and the 1st order to the 4th order wavelet details were calculated.
在详细描述合肥盆地布格重力异常的分布特征的同时，给出了布格重力异常小波分析计算不同阶次细节的结果。
Afterwards, the subsidence-sedimentation process slowed down gradually in the south of the Hefei Basin in the Middle-Late Jurassic without any strengthening phenomenon.
随后中—晚侏罗世时盆地南部沉降—沉积强度显示出变弱的趋势，期间没有再出现沉降—沉积再加强的现象。
Since 1958, the exploration and study of oil and gas in the Hefei Basin was engaged by more than 10 units. The exploration history of the Hefei Basin is divided into 4 stages.
自1958年以来，先后有10余个单位参与过合肥盆地的油气勘探及研究工作，大致经历了三下四上的曲折历程。
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。
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。
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