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《Acta Sedimentologica Sinica》 2003-04
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Sedimentary and Diagenetic Characteristics of Paleogene Lacustrine “Hunji” Rock in Beach District, Dagang

MA Yan ping LIU Li (College of Earth Sciences, Jinlin University ,Changchun 130061)  
“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 Madongdong 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 precipitation 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.
【Fund】: 中国石油大港油田分公司勘探开发技术研究中心资助
【CateGory Index】: P588.2
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