The Genesis of Layer-Bound Polygonal Faults in the Sanzhao Sag of Songliao Basin

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Through new 3-D seismic data and the technique of coherent slice, the development characteristic of layer-bound polygonal faults (PFs) is summarized in Zhaozhou oilfield in the south of Sanzhao sag, Songliao Basin. the layer-bound faults that show preferential alignment have lengths of 1503000 m, throws of 510 m, most strikes parallel to the slope direction and aligned faults are antithetic to the bedding dip. PFs activity coincided with a late K2qn to early K2y stage tilting event, gravity sliding model is proposed as a possible mechanism for the deformation.

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445-448

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August 2013

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© 2013 Trans Tech Publications Ltd. All Rights Reserved

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[1] J.A. Cartwright: Episodic basin-wide hydrofracturing of overpressured Early Cenozoic mudrock sequences in the North Sea Basin. Marine and Petroleum Geology. Vol. 11(1994), pp.587-607.

DOI: 10.1016/0264-8172(94)90070-1

Google Scholar

[2] J.A. Cartwright: Diagenetically induced shear failure of fine-grained sediments and the development of polygonal fault systems. Marine and Petroleum Geology. Vol. 28(2011), pp.1-18.

DOI: 10.1016/j.marpetgeo.2011.06.004

Google Scholar

[3] J.P. Henriet,M. de Batist,M. Verschuren: Early fracturing of Palaeogene clays, southernmost North Sea: relevance to mechanisms of primary hydrocarbon migration. Special Publication of European Association of Petroleum Geoscientists, Vol. 1(1991).

Google Scholar

[4] J. Watterson, J.J. Walsh, A. Nicol, P.A.R. Nell, P.G. Bretan: Geometry and origin of polygonal fault system. Journal of the Geological Society, Vol. 157(2000), pp.151-162.

DOI: 10.1144/jgs.157.1.151

Google Scholar

[5] W.G. Higgs, K.R. McClay: Analogue sandbox modelling of Miocene extensional faulting in the Outer Moray Firth. Geological Society Special Publication, Vol. 71(1993), pp.141-162.

DOI: 10.1144/gsl.sp.1993.071.01.07

Google Scholar

[6] D.N. Dewhurst, J.A. Cartwright, L. Lonergan: The development of polygonal fault systems by syneresis of colloidal sediments. Marine and Petroluem Goelogy, Vol. 16(1999), pp.793-810.

DOI: 10.1016/s0264-8172(99)00035-5

Google Scholar

[7] N.R. Goulty. Polygonal fault networks in fine-grained sediments – an alternative to the syneresis mechanism. First Break, Vol. 19(2001), pp.69-73.

DOI: 10.1046/j.1365-2397.2001.00137.x

Google Scholar

[8] R.J. Davies, M.T. Irelandn , J.A. Cartwright: Differential compaction due to the irregular topology of a diagenetic reaction boundary: a new mechanism for the formation of polygonal faults. Basin Research, Vol. 21(2009), pp.354-359.

DOI: 10.1111/j.1365-2117.2008.00389.x

Google Scholar

[9] A. Gay, C. Berndt: Cessation/reactivation of polygonal faulting and effects on fluid flow in the Vøring Basin, Norway Margin. Journal of the Geological Society, Vol. 164(2007), pp.129-141.

DOI: 10.1144/0016-76492005-178

Google Scholar

[10] S.A. Stewart J.D. Argent: Relationship between polarity of extensional fault arrays and presence of detachments. Journal of Structural Geology, Vol. 6(2000), pp.693-711.

DOI: 10.1016/s0191-8141(00)00004-3

Google Scholar

[11] Y. Song J.Y. Ren H.Z. Yang, D.J. Tong, C. Lei: Characteristics and dynamic background of bottom boundary in Yaojia Formation of the northern Songliao Basin. Acta Petrologica Sinica, Vol. 31(2010), pp.187-195(in chinese with English abstract).

Google Scholar