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Article Navigation >  Acta Sedimentologica Sinica  > 2007  >  25(2): 192-200

WANG Feng. Sedimentary Facies Model on Carbonate Rock in the Upper Shuaiba Member of Lower Cretaceous in Daleel Field, Oman[J]. Acta Sedimentologica Sinica, 2007, 25(2): 192-200.
Citation: WANG Feng. Sedimentary Facies Model on Carbonate Rock in the Upper Shuaiba Member of Lower Cretaceous in Daleel Field, Oman[J]. Acta Sedimentologica Sinica, 2007, 25(2): 192-200.
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Sedimentary Facies Model on Carbonate Rock in the Upper Shuaiba Member of Lower Cretaceous in Daleel Field, Oman

  • State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083

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  • Corresponding author: WANG Feng
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2007-04-10
  • The Upper Shuaiba Member(USH) is the main force pay bed in the Daleel oil field. Based on the data of geology, seicmic and paleobiology, the lithofacies assemblage and sedimentary environment in the USH were studied. Intershoal lows subfacies (where the water depth is 1050m) and shallow shoal subfacies( where the water depth is not more than 10m) were extinguished in the layer D, and storm deposit was found in the layer E1, in which intershoal lows subfacies also developed. The feature of the sedimentary subfacies and the sedimentary condition were summarized and studied, and the sedimentary model was set up in the paper that the intershoal lows on carbonate rocks were developed under the background of broad land in shallow sea, where storm events usually occurred in the lower Cretaceous in the area.
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Publishing history
  • Received:  1900-01-01
  • Revised:  1900-01-01
  • Published:  2007-04-10

Sedimentary Facies Model on Carbonate Rock in the Upper Shuaiba Member of Lower Cretaceous in Daleel Field, Oman

  • State Key Laboratory of Geological Processes and Mineral Resources, China University of Geosciences, Beijing 100083
    Corresponding author: WANG Feng
  • Received Date: 1900-01-01
  • Rev Recd Date: 1900-01-01
  • Publish Date: 2007-04-10

Abstract: The Upper Shuaiba Member(USH) is the main force pay bed in the Daleel oil field. Based on the data of geology, seicmic and paleobiology, the lithofacies assemblage and sedimentary environment in the USH were studied. Intershoal lows subfacies (where the water depth is 1050m) and shallow shoal subfacies( where the water depth is not more than 10m) were extinguished in the layer D, and storm deposit was found in the layer E1, in which intershoal lows subfacies also developed. The feature of the sedimentary subfacies and the sedimentary condition were summarized and studied, and the sedimentary model was set up in the paper that the intershoal lows on carbonate rocks were developed under the background of broad land in shallow sea, where storm events usually occurred in the lower Cretaceous in the area.

WANG Feng. Sedimentary Facies Model on Carbonate Rock in the Upper Shuaiba Member of Lower Cretaceous in Daleel Field, Oman[J]. Acta Sedimentologica Sinica, 2007, 25(2): 192-200.
Citation: WANG Feng. Sedimentary Facies Model on Carbonate Rock in the Upper Shuaiba Member of Lower Cretaceous in Daleel Field, Oman[J]. Acta Sedimentologica Sinica, 2007, 25(2): 192-200.
shu

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