【摘 要】
：
基于薄片观察、粒度分析、环境扫描电镜和全岩矿物定量分析、荧光光谱元素分析等测试结果,对鄂尔多斯盆地旬邑、瑶曲地区三叠系延长组长7段中的砂质碎屑流和浊流的微观沉积特
【机 构】
：
中国石油勘探开发研究院 西北分院,兰州 730020;中国石油天然气集团公司 油藏描述重点实验室,兰州 730020;中国石油勘探开发研究院 西北分院,兰州 730020;中国石油 长庆油田分公司,西
论文部分内容阅读
基于薄片观察、粒度分析、环境扫描电镜和全岩矿物定量分析、荧光光谱元素分析等测试结果,对鄂尔多斯盆地旬邑、瑶曲地区三叠系延长组长7段中的砂质碎屑流和浊流的微观沉积特征进行了研究.结果表明:(1)砂质碎屑流沉积的碎屑颗粒呈杂乱无序排列,而浊流沉积(鲍马序列A段)则有较明显的定向排列特征,反映出前者为整体快速搬运特征,而后者具有部分牵引流特征,表明其密度偏低,而二者均具有黄铁矿;(2)砂质碎屑流砂岩概率曲线具明显的两段式,反映牵引流特征,结合镜下观察,其来源应为浅水或陆上河流,而浊流砂岩则为单段式,反映重力流特征;(3)瑶曲长7沉积期古环境为干冷气候,砂质碎屑流相对浊流而言,其古环境大部分时期淋滤作用较弱;(4)砂质碎屑流砂岩及伴生泥岩的Sr/Ba值均小于浊流,表明其对湖水的稀释作用更强,注入速度更快,瑶曲整体Sr/Cu值低于旬邑,相对降雨量更丰富,此外,砂质碎屑流砂岩中重矿物Zr含量整体要高于浊流,表明其具有更强的碎屑搬运能力;(5)砂质碎屑流沉积和浊流沉积的黏土组成及混层比无明显差异,但全岩矿物成分组成有差别,通过差异性较大的石英与黏土含量制订划分模板,可将砂质碎屑流沉积、浊流沉积及两者过渡段进行定量划分.
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