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《Acta Sedimentologica Sinica》 2006-02
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The Formation of Carbonate Breccia in Shulu Depression

QIU Long-wei~ 1,2 DU Rui~ 1 LIANG Hong-bin~ 3 MA Jun~ 3 (1.China University of Petroleum, Dongying, Shandong 257061; 2.Postdoctoral Scientific Research Center of Shengli Oilfield,Dongying, Shandong 257000; 3.Oil Exploration & Development Institute, CNPC Huabei Oilfield Company, Renqiu, Hebei 062552)  
Breccia in Shulu depression was found in the middle and low of the third segment of Shahejie Formation, itisabreccia with carbonate fragment as its main constituent, and distributes skirt-shapelyon slopes in the depression. Breccia and marlstonewith breccia are familiarbreccias in the area and the former is domestic. Grain and matrix in the breccia are mainly angular and subangular carbonate clastic particles, whose parent rock were carbonate stratum of Ordovician. Mainly grain support, massive structure, infrequent gradedbedding and others bedding, un-sorting of detrital grains and thicker breccia layer are important features of carbonate breccia in Shulu depression. Characteristics of component, fabric, structure and geologic background all reveal that the breccia in the study area is inviscous debris flow sediment of terrestrial formation.
【CateGory Index】: P588.245
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