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Structures of the Bohai Petroliferous Area, Bohai Bay Basin
Acta Geologica Sinica, 2000Abstract This paper, for the first time, deals with a more systematic study of the structures in the Bohai petroliferous area that covers nearly one third of the Bohai Bay basin. The study mainly involves the effects of preexisting basement faults on the basin formation, the characteristics of basin geometry and kinetics, the modelling of the tectonic‐
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Cenozoic tectonic migration in the Bohai Bay Basin, East China
Geological Journal, 2016AbstractTectonic migration is a common geological process during basin formation and development. However, there are many disputes about the tectonic migration and its dynamic mechanism in the Bohai Bay Basin. By analysis of Cenozoic tectonic, sedimentation and magmatism migration processes in the Bohai Bay Basin, combined with previous studies, the ...
Suhua Jiang, Sanzhong Li
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A detailed receiver function image of the sedimentary structure in the Bohai Bay Basin
Physics of the Earth and Planetary Interiors, 2005Abstract If the site at which receiver functions are constructed is filled by sediments, then the waveforms from these receiver functions are dominantly controlled by the sedimentary structures within the first few seconds after the direct P arrival. Based on this observation, waveform data collected at 44 temporary seismic stations have been used to
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Characteristics and Genetic Mechanisms of Overpressure in the Depressions of Bohai Bay Basin, China
Acta Geologica Sinica, 2016AbstractThe distribution and genetic mechanisms of abnormal pressures in the Bohai Bay Basin were systematically analyzed. Abnormal pressures are widely developed in the Bohai Bay Basin, primarily in the Paleogene E2s4, E2s3, Es1, and Ed formations. From the onshore area of the Bohai Bay Basin to the center of the Bozhong area, the top depth of the ...
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Nanpu sag of the Bohai Bay basin: A transtensional fault-termination basin
Journal of Earth Science, 2011The Nanpu (南堡) sag has previously been modeled as (1) a pull-apart basin, (2) a rift basin, without significant strike-slip deformation, and (3) a transtensional basin. We present a new model for the Nanpu sag in which the basin is a transtensional fault-termination basin.
Xiaofeng Liu, Cuimei Zhang
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