Basinal Texture Structure of Qikou Sag in Bohai Bay Basin and Its Evolution
Received date: 2011-02-09
Revised date: 2011-05-17
Online published: 2011-06-10
We use the new obtained super-large area 3D seismic data to deduce the structure feature,fault activities & tectonic evolution in the Qikou sag.The results show that a good connection between sub-sags would occur at early Paleogene Period (Es3).The separation between water and deposits was happened by the gradually uplift of the buried hill at the end of Es1-Ed tectonics.The superimposition of different phase tectonics was observed in the Qikou sag.With exception of boundary faults,the main faults in the Qikou sag were not active or moved weakly at the Es3 Period.We divide the tectonic activities into 4 epoches in the Qikou sag,including mid-Es3 Epoch,mid-Es1 Epoch,Ed Epoch end and Nm Epoch end.The unconformities exist between Es13,Ed and Ng,respectively.Two typical episodic stages in the Qikou sag could be divided,such as chasmic stage and thermal-depress stage.The two typical stages subdivide into four sub\|epoches like as chasmic Ⅰ(Es3-Es2)chasmic Ⅱ(Es1-Ed),stable thermal depress epoch (Ng-Nmx) and accelerrate thermal depress epoch(after Nmx).
Key words: Qikou sag; Basin structure; Fault activity; Basin evolution; Rifting; Thermal subsidence; Extension; Strike-slip.
ZHOU Li-Hong, LU Yi, XIAO Dui-Qing, ZHANG Zhi-Pan, CHEN Xian-Bao, WANG Hui, HU Shi-Ying . Basinal Texture Structure of Qikou Sag in Bohai Bay Basin and Its Evolution[J]. Natural Gas Geoscience, 2011 , 22(3) : 373 -382 . DOI: 10.11764/j.issn.1672-1926.2011.03.373
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