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SHEN An jiang, ZHU Guo hua, SHOU Jian feng, XU Yang. A Research on E3l Nl N2l Clastic Rock Reservoir in Yuejin Area,Oaidam Basin,Northwest China[J]. Acta Sedimentologica Sinica, 2001, 19(1): 71-78.
Citation: SHEN An jiang, ZHU Guo hua, SHOU Jian feng, XU Yang. A Research on E3l Nl N2l Clastic Rock Reservoir in Yuejin Area,Oaidam Basin,Northwest China[J]. Acta Sedimentologica Sinica, 2001, 19(1): 71-78.

A Research on E3l Nl N2l Clastic Rock Reservoir in Yuejin Area,Oaidam Basin,Northwest China

  • Received Date: 2000-01-11
  • Rev Recd Date: 2000-02-18
  • More attention has been paid to the report of hvdrocarhon from E31、N1、N21 clastic rock reservoir in Yucjin area Qaidam hasin, northcrnwcst China. Based on research of approximate one hundred cast thin sections and mcrcurv intrusion curve from 15 wells, some results on E31、N1、N21 elastic rock reservoir in Yuejin area have been obtained.as follows:①The elastic rock reservoir was composed of fcldspathic sandstone } lithic arkosc and fcldspathic litharcnitc which is characterized by lower composition and texture maturity②The elastic rock reservoir has undergone compaction, pressure dissolution, authigcnc(fcrroan calcite, dolomite, anhydrite, cuthalitc, fcrroan dolomite pyrite ) ccmcntation and dissolution, which results in the forming of overwhelming relic primary intcrgranular pore.Corrclatahlc beds from eastern Yucjin and western Yucjin have different diagcnctic-porosity evolution because of their different burial depths which results in a more favourable reservoir in western Yucjin than in eastern Yuejin,③E31、N1、N21 elastic rock reservoir developed under distrihutarv channel sand flat and braided channel microfacics.Reservoir quality was controlled by composition and texture maturity, matrix material and diagcnctic environment}depth especially),④E3, elastic rock reservoir from western Yucjin characterized by very large, large and medium pore,Ⅱ-grade( high porosity and medium permeability ) in reservoir quality and a combination of large porefine throat while E3 elastic rock reservoir from eastern Yucjin did large and medium pore,Ⅴ-graded (very low porosity(very low permeability) in reservoir quality and a combination of medium pore-very fine throat. N1 elastic rock reservoir in Yucjin area characterized by very large large and medium pore,Ⅳ-andⅤ-grade( low porosity and very low permeability) in reservoir quality and a combination of large pore-very fine throat.
  • [1] 1 青藏油气区石油地质志编写组. 中国石油地质志(青藏油气区). 第 十四卷[M]. 北京:,石油工业出版社,1987

    2 张景廉,张平中. 黄铁矿对有机质成烃的催化作用讨论[J]. 地球科学进展,1996,11(3):282 ~ 287

    3 Carlos H,Bruhn. L. Reservoir Architecture of Deep-Lacustrine Sandstones from the Early Cretaceous Reconcavo Rift Basin,BraziI[J]. AAPG Bull,1999,83(9):1502 ~ 1525
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  • Received:  2000-01-11
  • Revised:  2000-02-18

A Research on E3l Nl N2l Clastic Rock Reservoir in Yuejin Area,Oaidam Basin,Northwest China

Abstract: More attention has been paid to the report of hvdrocarhon from E31、N1、N21 clastic rock reservoir in Yucjin area Qaidam hasin, northcrnwcst China. Based on research of approximate one hundred cast thin sections and mcrcurv intrusion curve from 15 wells, some results on E31、N1、N21 elastic rock reservoir in Yuejin area have been obtained.as follows:①The elastic rock reservoir was composed of fcldspathic sandstone } lithic arkosc and fcldspathic litharcnitc which is characterized by lower composition and texture maturity②The elastic rock reservoir has undergone compaction, pressure dissolution, authigcnc(fcrroan calcite, dolomite, anhydrite, cuthalitc, fcrroan dolomite pyrite ) ccmcntation and dissolution, which results in the forming of overwhelming relic primary intcrgranular pore.Corrclatahlc beds from eastern Yucjin and western Yucjin have different diagcnctic-porosity evolution because of their different burial depths which results in a more favourable reservoir in western Yucjin than in eastern Yuejin,③E31、N1、N21 elastic rock reservoir developed under distrihutarv channel sand flat and braided channel microfacics.Reservoir quality was controlled by composition and texture maturity, matrix material and diagcnctic environment}depth especially),④E3, elastic rock reservoir from western Yucjin characterized by very large, large and medium pore,Ⅱ-grade( high porosity and medium permeability ) in reservoir quality and a combination of large porefine throat while E3 elastic rock reservoir from eastern Yucjin did large and medium pore,Ⅴ-graded (very low porosity(very low permeability) in reservoir quality and a combination of medium pore-very fine throat. N1 elastic rock reservoir in Yucjin area characterized by very large large and medium pore,Ⅳ-andⅤ-grade( low porosity and very low permeability) in reservoir quality and a combination of large pore-very fine throat.

SHEN An jiang, ZHU Guo hua, SHOU Jian feng, XU Yang. A Research on E3l Nl N2l Clastic Rock Reservoir in Yuejin Area,Oaidam Basin,Northwest China[J]. Acta Sedimentologica Sinica, 2001, 19(1): 71-78.
Citation: SHEN An jiang, ZHU Guo hua, SHOU Jian feng, XU Yang. A Research on E3l Nl N2l Clastic Rock Reservoir in Yuejin Area,Oaidam Basin,Northwest China[J]. Acta Sedimentologica Sinica, 2001, 19(1): 71-78.
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