摘要
通过对独山江寨地区下泥盆统丹林组、舒家坪组的石英砂岩、含砾砂岩的粒度分析,并结合上述两个地层组岩性组合和沉积构造特征,对该时期沉积环境进行了详细分析,识别出该地区下泥盆统为无障壁滨岸相的砂(砾)质高能海岸型沉积环境,层序特征具海岸沙丘-后滨(海滩砂脊)-前滨-临滨亚相的三个退积沉积旋回序列。
By grading analyses of Shujiaping formation in Low Devonian in quartz sandstone and pebbly Jiangzhai area, according to the sandstone of Danlin formation and lithology association and sedimentary structural features in these area, the sedimentary environment in this period is analysed, it finds out Devonian in this area is sandy high energy coast sedimentary environment without barrier onshore facies, it has 3 retrogra- date sedimentary cycle sequences :coast dune-backshore-foreshore-shore sub-facies.
出处
《贵州地质》
2015年第1期21-26,共6页
Guizhou Geology
基金
中国地质调查局地质大调查项目--贵州1:5万梵净山
德旺
江口
凯德场幅区域地质调查(编号:1212011120622)
贵州1:5万独山
河寨
甲良
周覃幅区域地质调查项目(编号:12120114072801)资助
关键词
下泥盆统
粒度特征
沉积环境
独山江寨
Lower Devonian
Grading features
Sedimentary environment
Jiangzhai Dushan