中生界砂岩碎屑组分分析，表明其源区为大别造山带。
Detrital composition analysis of the Mesozoic sandstones indicates that their provenance is the Dabie orogen.
碎屑组分及其含量以及胶结物组分及其含量是影响储层物性的主要因素。
Content of detrital composition and Content of cement are major factors which influence on Reservoir Physical Property.
碎屑岩中的碎屑组分和地球化学特征直接反映物源区和沉积盆地的构造环境。
The detrital and chemical components can directly reflect the features of the provenance and its tectonic setting.
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