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Article Navigation >  Acta Sedimentologica Sinica  > 2005  >  23(3): 389-396

MENG Yuan-lin, LIU De-Lai, HE Ru, WANG Zhi-guo, ZHANG Wen-cai, Yin Xiu-lan, LI Jun. Diagenetic Field Analysis and Porosity Prediction of the Shaer Member( Es2 ) in Overpressure Setting in the Qibei Depression[J]. Acta Sedimentologica Sinica, 2005, 23(3): 389-396.
Citation: MENG Yuan-lin, LIU De-Lai, HE Ru, WANG Zhi-guo, ZHANG Wen-cai, Yin Xiu-lan, LI Jun. Diagenetic Field Analysis and Porosity Prediction of the Shaer Member( Es2 ) in Overpressure Setting in the Qibei Depression[J]. Acta Sedimentologica Sinica, 2005, 23(3): 389-396.
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Diagenetic Field Analysis and Porosity Prediction of the Shaer Member( Es2 ) in Overpressure Setting in the Qibei Depression

  • 1.

    Daqing Petroleum Institute,Qinhuangdao Hebei 066004;

  • 2.

    China University of Geosciences, Beijing 100083;

  • 3.

    PetroChina Company Limited,Beijing 100112;

  • 4.

    Exploration & Exploitation Institute of Daqing Oil Field, Daqing, Heilongjiang 163712;

  • 5.

    China Institute of Geo-environmental Monitoring, Beijing 100081;

  • 6.

    Scientific and Technical Information Division, Dagang Oil Field, Tianjin 300280

  • Received Date: 2004-09-28
  • Rev Recd Date: 2004-12-28
  • Publish Date: 2005-09-10
  • The diagenetic field was defined as the whole of diagenetic intensity in the space at a certain moment according to the basic principle of field theory, which could be described by diagenetic intensity ID. A new multivariate non-leanermodel, porosity Φ= F ( Trask So, diagenetic intensity ID, pressure P), was set up on the basis of diagenetic field analysis, sedimentary parameters quantitative study, pressure and porosity correlation investigation. As the porosity prediction of beach bar sandstones of ShaerMember ( Es2 ) in the Qibei depression shows the predicted error of porosity for the sandstones with the cement of more than 10% is less than 2%, and the predicted porosity of sand bodies in the eastern Qibei depression is 15%-20%, which are the favorable reservoir area developed in the depression.
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  • Received:  2004-09-28
  • Revised:  2004-12-28
  • Published:  2005-09-10

Diagenetic Field Analysis and Porosity Prediction of the Shaer Member( Es2 ) in Overpressure Setting in the Qibei Depression

  • 1. Daqing Petroleum Institute,Qinhuangdao Hebei 066004;
  • 2. China University of Geosciences, Beijing 100083;
  • 3. PetroChina Company Limited,Beijing 100112;
  • 4. Exploration & Exploitation Institute of Daqing Oil Field, Daqing, Heilongjiang 163712;
  • 5. China Institute of Geo-environmental Monitoring, Beijing 100081;
  • 6. Scientific and Technical Information Division, Dagang Oil Field, Tianjin 300280
  • Received Date: 2004-09-28
  • Rev Recd Date: 2004-12-28
  • Publish Date: 2005-09-10

Abstract: The diagenetic field was defined as the whole of diagenetic intensity in the space at a certain moment according to the basic principle of field theory, which could be described by diagenetic intensity ID. A new multivariate non-leanermodel, porosity Φ= F ( Trask So, diagenetic intensity ID, pressure P), was set up on the basis of diagenetic field analysis, sedimentary parameters quantitative study, pressure and porosity correlation investigation. As the porosity prediction of beach bar sandstones of ShaerMember ( Es2 ) in the Qibei depression shows the predicted error of porosity for the sandstones with the cement of more than 10% is less than 2%, and the predicted porosity of sand bodies in the eastern Qibei depression is 15%-20%, which are the favorable reservoir area developed in the depression.

MENG Yuan-lin, LIU De-Lai, HE Ru, WANG Zhi-guo, ZHANG Wen-cai, Yin Xiu-lan, LI Jun. Diagenetic Field Analysis and Porosity Prediction of the Shaer Member( Es2 ) in Overpressure Setting in the Qibei Depression[J]. Acta Sedimentologica Sinica, 2005, 23(3): 389-396.
Citation: MENG Yuan-lin, LIU De-Lai, HE Ru, WANG Zhi-guo, ZHANG Wen-cai, Yin Xiu-lan, LI Jun. Diagenetic Field Analysis and Porosity Prediction of the Shaer Member( Es2 ) in Overpressure Setting in the Qibei Depression[J]. Acta Sedimentologica Sinica, 2005, 23(3): 389-396.
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