The genetic mechanism of mud-coated intraclasts within deep-water massive sandstone in Yanchang Formation of Ordos Basin was studied combining the test method of element geochemistry, XRD and rock thin section analysis. The find-ings of this study include the following:the Fe/Mn is low, the content of MnO2 is high, Th/U is high, theδU is less than 1, and the Sr/Ba is low in the argillaceous cladding layer, reflecting the geochemistry characteristics of shallow water environ-ment are nearshore, oxidation and low salinity. There is a large difference in depositional environment with the associated layered mudstone of the semi-deep lake. The main components of the core of the mud-coated intraclasts are sandy, muddy or dolomitic lump, which were formed in shore-shallow lake or delta front environment. The formation process of mud-coated in-traclasts was long, in which the soft sandy or muddy sediments within the delta front were transported into deep lakes in clumps from Chang7 to Chang63 period through four stages:lump formation of shallow lake facies, initial formation of struc-ture, mixed transfer of lithology and eventually deposition setting.%通过元素地球化学分析、X-衍射全岩分析、岩石薄片分析等试验方法对鄂尔多斯盆地延长组块状砂岩中"泥包砾"结构成因机制进行研究.结果表明:该结构中泥质包壳层Fe/Mn值较低、MnO2含量较高,Th/U值较高、δU小于1,Sr/Ba值较低,反映近岸、偏氧化及低古盐度的浅水地球化学特征,和与其伴生的半深湖层状泥岩的沉积介质环境存在较大差异性;结构中内核的主要成分为砂质、泥质或白云石团块,形成于滨浅湖或三角洲前缘环境;"泥包砾"结构非瞬态形成,而是贯穿长7—长63期三角洲前缘砂泥岩软沉积物往深湖区块体搬运的全过程,经历浅湖相团块形成、结构初始形成、岩性混合转移、最终停积定型4个阶段.
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