Seismic Facies of Paleogene in Liaodong Bay,Bohai Basin
- Received Date: 1900-01-01
- Rev Recd Date: 1900-01-01
- Publish Date: 2007-08-10
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Key words:
- seismic sequence /
- seismic facies /
- Liaodong Bay /
- Paleogene
Abstract: Seismic facies of Paleogene in LiaoDong Bay are divided and named mainly based on the reliable internal reflection texture and external shape of the seismic sequence unit. Amplitude, continuity and other seismic parameters are also used in the description of seismic sequence units. In the study area, six seismic sequences are divided and more than seven seismic facies are identified, including parallelsubparallel matshaped, foreset, wedge shaped, filling, lenticular, moundy and hummocky seismic facies, which show differentiation in spatial distribution and hereditability in vertical evolution. The sedimentary facies in the lake environment, including semideepdeep lake subfacies, shallow lake and shore subfacies, fandelta, subaqueous alluvial fan, delta, turbidite, etc. The favorable areas are identified.
Citation: | DONG Yanlei. Seismic Facies of Paleogene in Liaodong Bay,Bohai Basin[J]. Acta Sedimentologica Sinica, 2007, 25(4): 554-563. |