庐枞盆地及周缘地区黄马青组沉积微相及与含铜岩系的关系

庐枞盆地及其周缘地区黄马青组具有典型的河控三角洲沉积层序，为前三角洲亚相-三角洲前缘亚相沉积。上段主要由泥岩-砂岩组成，三角洲前缘亚相，发育远砂坝、河口砂坝、分流间湾、分支河道和天然堤等微相，总体构成向上变粗的海退三角洲序列。含铜岩系分布于黄马青组上段，由灰绿色、深灰等还原色调的粉砂质泥岩或泥质粉砂岩等细碎屑岩类组成，属于三角洲前缘亚相中的分流间湾微相环境，在庐枞盆地中南部最为发育。

Deposited Micro-facies of Huangmaqing Formation in and Around Luzong Basin and Its Relationships with Rocks Series Containing Cu

Through geological profile and trunk route survey, the characteristics of sedimentary facies of Huangmaqing Formation in Luzong basin and its peripheral regions has been studied. Through testing of samples, the contents characteristics of Cu, Pb, Zn, Au, Ag and some other metal elements at the upper Huangmaqing Formation has been analysed. Further more, the accumulation beds of Cu and its mechanism of concentration has been tentatively discussed. 
 Sedimentary sequence of Huangmaqing Formation in Luzong basin and its peripheral regions is typical river delta which includes front delta delta front subfacies. The Lower Huangmaqing Formation rich in marine fossil bivalve contains dark grey and purplish clay, silty clay, and a little micritic dolomite, calcareous clayey siltstone, whose sedimentary subfacies is front delta. The sedimentary subfacies of Upper Huangmaqing Formation containing mudstone and sandstone is delta front which developed mainly distal bar, river mouth bar, interdistributary bay, distributary channel, natural levee microfacies. On the whole, it is coarsening upward sequence of regression deltaic.
 The background content of Cu calculated by 84 samples from Upper Huangmaqing Formation is 79.39×10 6. However, content of Cu of various rocks is obviously different, with that of silty mudstone 8 times significantly higher than sandstone. Further analysis  manifests that the concentration of Cu in silty mudstone attributes to these grayish green dark gray silty mudstone and muddy siltstone  deposited in reducing environments, thus its content of Cu is 10 times higher than the background values of Huangmaqing formation. Thus, Cu  bearing stratiform of Huangmaqing Formation is silty mudstone and muddy siltstone covered with reduced colour of grayish green dark gray silty which deposited in interdistributary bay of delta front. The abundant organic matters and weak hydrodynamic forces of interdistributary bay is in favour of  sedimentataion of organic matters carried by running water of distributary channel. The organic matters can obsorb Cu2+, Fe2+. At the same time, H2S generated by bacterial degradation of the organic matters  to form  the reductive environments where Cu2+, Fe2+contained in the fluid and gel deposited. Thus reducing materials such as chalcocite, bornite, chalcopyrite, pyrite have been generated and the Cu is concentrated.
 The mudstone and silty mudstone of Upper Huangmaqing Formation developed in interdistributary bay, thus mudstone content can reflect its development. The litho facies paleogeography graph is plotted by ratio of rocks (contour map of mudstone/sandstone). By ratio of mudstone/sandstone of the section, the four areas of mudstone <10, 10~20, 20~30, >30 are determined through interpolation method which use contour value 10%, 20%, 30%. The four areas reflect the plane development of interdistributary bay microfacies and also the Cu bearing stratiform. The litho facies paleogeography graph manifests  the Cu bearing stratiform of Huangmaqing Formation is well developed to the east of Yijinqiao Shiji in south central basin.