Sedimentary Facies of the First Member of Qingshankou-Formation in Late Cretaceous Songliao Basin of Daqing Oilfield China

Qian Zhang

doi:10.4028/www.scientific.net/AMR.898.428

Paper Titles

Axial Behavior of Concrete-Filled Double Skin Steel Tubular Stub Columns Filled with Demolished Concrete Lump
p.407

Theory and Practice on Non-Artificial Drainage of CBM High-Yielding Well
p.413

The Application of Improved Entropy Method in the Sustainable Utilization of Russia Oil Resources
p.420

Qingshankou-Formation Gravity-Flow Sedimentation in Early Cretaceous Songliao Basin of Northeast China: Evidences from Seismic Attributions Identification and Drilling Cores
p.424

Sedimentary Facies of the First Member of Qingshankou-Formation in Late Cretaceous Songliao Basin of Daqing Oilfield China
p.428

Conflict Resolution Strategy on Parameters Optimization in BTA Deep-Hole Processing
p.432

Investigation of Rare-Earth Salt Refiner on Purifying Effect of Impure Red Copper
p.436

Preparation of Ammonium Iron Blue from Copperas and Ammonium Sulfate Wasted Liquid
p.443

Influence of Fe Doping on Ce-Mn/TiO₂-ZrO₂ Catalysts for Low-Temperature Selective Catalytic Reduction of NO
p.447

HomeAdvanced Materials ResearchAdvanced Materials Research Vol. 898Sedimentary Facies of the First Member of...

Sedimentary Facies of the First Member of Qingshankou-Formation in Late Cretaceous Songliao Basin of Daqing Oilfield China

Abstract:

According to core, logging and seismic data, using tectonic-stratigraphic and sequence stratigraphic analysise theories in Qingshankou Formation of division and comparison, and the sequence boundary and sequence unit to be optimized, in order to carry out seismic deposition. By determining the levels of sequence interface on seismic, logging and faces reflecting characteristics of the study area to build sequence interface identifier. In the course of practical work, identified the continental basin of the more common of the one to three levels of sequence interface, system interface and the parasequence set interface. In Songliao Basin, second-order sequences often corresponding to the tectonic evolution of the basin episodic stage, and in each period of prototype basin internal episodic tectonic extension or episodic of tectonic inversion is consistent, in Qingshankou Formation in the development of one second-order sequence boundary SB11 (T11), three third-order sequence boundary, there are SB12 (T12), SB13 (T13) and SB2 (T2), seven forth-order sequence boundary. In the plane, using the data of 256 wells, analysis of the distribution characteristics of the sedimentary facies of the first member of Qingshankou-Formation.

You might also be interested in these eBooks

Applied Material Science and Related Technologies

View Preview

Info:

Periodical:

Advanced Materials Research (Volume 898)

Pages:

428-431

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.898.428

Citation:

Cite this paper

Online since:

February 2014

Authors:

Qian Zhang*

Keywords:

First Member of Qingshankou-Formation, Late Cretaceous, Sedimentary Facies, Songliao Basin

Export:

RIS, BibTeX

Price:

Permissions CCC:

Request Permissions

Permissions PLS:

Request Permissions

Сopyright:

Citation:

* - Corresponding Author

References

[1] Z. Q. Feng, C. Z. Jia and X. N. Xie: Tectonostratigraphic units and stratigraphic sequences of the nonmarine Songliao basin, Northeast China: Basin Research, Vol. 22 (2010), pp.79-95.

DOI: 10.1111/j.1365-2117.2009.00445.x

Google Scholar

[2] P.R. Vail, R. M. Mitchum and R. G. ToddJr: Seismic stratigraphy and globalchanges of sea level (Seismic Stratigraphy, AAPG Memoir, 1977) Vol. 26, pp.49-212.

Google Scholar

[3] H. L. Zeng, T. F. Hentz: High-frequency sequence stratigraphy from seismicsedimentology: Applied to Miocene, Vermilion Block 50, Tiger Shoal area, offshore Louisiana: AAPG Bulletin, Vol. 88 (2004) No. 2, pp.153-174.

DOI: 10.1306/10060303018

Google Scholar

[4] W. Z. Zhao, C. N. Zou and Y. L. Chi: Sequence stratigraphy, seismic sedimentology, and litho-stratigraphic plays: Upper Cretaceous, Sifangtuozi Area, Southwest Songliao Basin, China: AAPG Bulletin, (2011), p.35.

DOI: 10.1306/06301009125

Google Scholar