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WEI Wei, ZHANG Shun, ZHANG Chen-chen, WU Chao-dong. Seismic Sedimentology Characteristics of Lacustrine-Delta Facies of Quantou-Nenjiang Formations in North Songliao Basin[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1153-1161.
Citation: WEI Wei, ZHANG Shun, ZHANG Chen-chen, WU Chao-dong. Seismic Sedimentology Characteristics of Lacustrine-Delta Facies of Quantou-Nenjiang Formations in North Songliao Basin[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1153-1161.

Seismic Sedimentology Characteristics of Lacustrine-Delta Facies of Quantou-Nenjiang Formations in North Songliao Basin

  • Received Date: 2013-11-18
  • Rev Recd Date: 2014-02-26
  • Publish Date: 2014-12-10
  • The Quantou-Nenjiang Formations of Songliao Basin belong to the depression period, developed large fluvial facies in Quantou Formation, but developed large lacustrine-delta deposition in Qingshankou, Yaojia and Nenjiang Formations. The reservoir strata are mainly point bar sand body, progradational and retrogradational delta sand body and the gravity flow sand body of lacustrine facies. The traditional work of exploration just focused on 2D seismic data by point-line research method, so there may be some mistakes in understanding spatial form, the interior structure and the distribution of the sand bodies. By the enlargement of the cover area and the improvement of the acquisition accuracy in 3D seismic works, the Seismic Sedimentology is widespread used in North Songliao Basin. With fine depicting of the geologic bodies, we found that the progradational delta has the typical bird foot shape controlled by the high angle fluvial facies, narrow in the delta front, but wide in the delta plain, without underwater distributary channels developed. The retrogradational delta has the weeping willow shape controlled by the low angle laucustrine facies, wide in the delta front, but narrow in the delta plain, developed the underwater distributary channels. And we found large slump fan and turbidite fan in Qingshankou Formation and group 2-3 of Nenjiang Formation. Also, we found large turbidite channel in Yaojia Formation and group 1 of Nenjiang Formation. This study will cover the shortage of the traditional research techniques and refresh the new field of the exploration in North Songliao Basin.
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  • Received:  2013-11-18
  • Revised:  2014-02-26
  • Published:  2014-12-10

Seismic Sedimentology Characteristics of Lacustrine-Delta Facies of Quantou-Nenjiang Formations in North Songliao Basin

Abstract: The Quantou-Nenjiang Formations of Songliao Basin belong to the depression period, developed large fluvial facies in Quantou Formation, but developed large lacustrine-delta deposition in Qingshankou, Yaojia and Nenjiang Formations. The reservoir strata are mainly point bar sand body, progradational and retrogradational delta sand body and the gravity flow sand body of lacustrine facies. The traditional work of exploration just focused on 2D seismic data by point-line research method, so there may be some mistakes in understanding spatial form, the interior structure and the distribution of the sand bodies. By the enlargement of the cover area and the improvement of the acquisition accuracy in 3D seismic works, the Seismic Sedimentology is widespread used in North Songliao Basin. With fine depicting of the geologic bodies, we found that the progradational delta has the typical bird foot shape controlled by the high angle fluvial facies, narrow in the delta front, but wide in the delta plain, without underwater distributary channels developed. The retrogradational delta has the weeping willow shape controlled by the low angle laucustrine facies, wide in the delta front, but narrow in the delta plain, developed the underwater distributary channels. And we found large slump fan and turbidite fan in Qingshankou Formation and group 2-3 of Nenjiang Formation. Also, we found large turbidite channel in Yaojia Formation and group 1 of Nenjiang Formation. This study will cover the shortage of the traditional research techniques and refresh the new field of the exploration in North Songliao Basin.

WEI Wei, ZHANG Shun, ZHANG Chen-chen, WU Chao-dong. Seismic Sedimentology Characteristics of Lacustrine-Delta Facies of Quantou-Nenjiang Formations in North Songliao Basin[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1153-1161.
Citation: WEI Wei, ZHANG Shun, ZHANG Chen-chen, WU Chao-dong. Seismic Sedimentology Characteristics of Lacustrine-Delta Facies of Quantou-Nenjiang Formations in North Songliao Basin[J]. Acta Sedimentologica Sinica, 2014, 32(6): 1153-1161.
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