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.

Dynamics of the evolution of the Tanlu fault zone:A multiforce-in-multiphase acting model;

An attempt to apply three geothermometers in the interpretation of low-temperature mylonites in the southern segment of the Tanlu fault zone;

Fault activities and hydrocarbon migration and accumulation during the Neotectonic period in the Bozhong-Bonan segment of the Tanlu fault zone

Deep structures of the Bohai part of the Tan-Lu fault zone and their dynamic implications;

Foreland sedimentation evidence of syn-orogenic motion of the Tan-Lu fault zone;

Tectonic characteristics and evolution of the Tan-Lu fault zone in the Xiwei area,Feidong County,Anhui Province;

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.

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.

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.

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.

Thermochronologic information from the Tan-Lu fault zone and its relationship with the exhumation of the Dabie Mountains;

The Tan-Lu fault zone, which played a key role in tectonic evoluiton of East China continent during Cenozoic, and controlled the formation and deformation of the large basins and their evaluation of petroleum resource, was one of the most important tectonic belts in eastern marginal areas of Asia.

Because extensional structures from late Cretaceous to Paleogene and compressional structures since Neogene are conserved well, most geologists agreed on that the Tan-Lu fault zone experienced extension and following compression since late Cretaceous.