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MA Yan ping, LIU Li. Sedimentary and Diagenetic Characteristics of Paleogene Lacustrine "Hunji" Rock in Beach District, Dagang[J]. Acta Sedimentologica Sinica, 2003, 21(4): 607-614.
Citation: MA Yan ping, LIU Li. Sedimentary and Diagenetic Characteristics of Paleogene Lacustrine "Hunji" Rock in Beach District, Dagang[J]. Acta Sedimentologica Sinica, 2003, 21(4): 607-614.

Sedimentary and Diagenetic Characteristics of Paleogene Lacustrine "Hunji" Rock in Beach District, Dagang

  • Received Date: 2002-08-21
  • Rev Recd Date: 2002-10-28
  • Publish Date: 2003-12-10
  • “Hunji” rocks of the lower part of number 1 of Shahejie Formation,Beach district,Dagang, are dominantly terrigenous clastithic-carbonate “Hunji” rock, subordinately carbonatic-terrigenous clastic “Hunji” rock and carbonate bearing-terrigenous clastic “Hunji” rock.“Hunji” rock of Baishuitou district lies in braided stream-fan delta front subfluvial branching river deposits,which mixed by gradual facies change.While Madong-Madong dong district is distributed in gravity flow deposit systems, mixed by turbidites.“Hunji” rocks of this area experienced compaction, cementation and dissolution /alteration process.Pore fluid experienced alkaline to acid and return to alkaline.The association of glauconite and micro-calcite cement, calcite precipi ation and a part of quartz dissolution is with alkaline pore fluid;The association of hydrocarbon emplacement, dissolution, quartz overgrowth and kaolinite precipitation is with acid pore fluid;And the association of illite, chlorite, albitization, pore-filling calcite and dolomite is with alkaline pore fluid.
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  • Received:  2002-08-21
  • Revised:  2002-10-28
  • Published:  2003-12-10

Sedimentary and Diagenetic Characteristics of Paleogene Lacustrine "Hunji" Rock in Beach District, Dagang

Abstract: “Hunji” rocks of the lower part of number 1 of Shahejie Formation,Beach district,Dagang, are dominantly terrigenous clastithic-carbonate “Hunji” rock, subordinately carbonatic-terrigenous clastic “Hunji” rock and carbonate bearing-terrigenous clastic “Hunji” rock.“Hunji” rock of Baishuitou district lies in braided stream-fan delta front subfluvial branching river deposits,which mixed by gradual facies change.While Madong-Madong dong district is distributed in gravity flow deposit systems, mixed by turbidites.“Hunji” rocks of this area experienced compaction, cementation and dissolution /alteration process.Pore fluid experienced alkaline to acid and return to alkaline.The association of glauconite and micro-calcite cement, calcite precipi ation and a part of quartz dissolution is with alkaline pore fluid;The association of hydrocarbon emplacement, dissolution, quartz overgrowth and kaolinite precipitation is with acid pore fluid;And the association of illite, chlorite, albitization, pore-filling calcite and dolomite is with alkaline pore fluid.

MA Yan ping, LIU Li. Sedimentary and Diagenetic Characteristics of Paleogene Lacustrine "Hunji" Rock in Beach District, Dagang[J]. Acta Sedimentologica Sinica, 2003, 21(4): 607-614.
Citation: MA Yan ping, LIU Li. Sedimentary and Diagenetic Characteristics of Paleogene Lacustrine "Hunji" Rock in Beach District, Dagang[J]. Acta Sedimentologica Sinica, 2003, 21(4): 607-614.
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