庞军刚, 李文厚, 郭艳琴, 王起琮, 陈全红, 梁积伟. 陕北子洲地区二叠纪山西组沉积环境[J]. 煤田地质与勘探, 2006, 34(5): 5-8.
引用本文: 庞军刚, 李文厚, 郭艳琴, 王起琮, 陈全红, 梁积伟. 陕北子洲地区二叠纪山西组沉积环境[J]. 煤田地质与勘探, 2006, 34(5): 5-8.
PANG Jun-gang, LI Wen-hou, GUO Yan-qin, WANG Qi-cong, CHEN Quan-hong, LIANG Ji-wei. Sedimentary environment of Permian Shanxi Formation in Zizhou region,northern Shaanxi[J]. COAL GEOLOGY & EXPLORATION, 2006, 34(5): 5-8.
Citation: PANG Jun-gang, LI Wen-hou, GUO Yan-qin, WANG Qi-cong, CHEN Quan-hong, LIANG Ji-wei. Sedimentary environment of Permian Shanxi Formation in Zizhou region,northern Shaanxi[J]. COAL GEOLOGY & EXPLORATION, 2006, 34(5): 5-8.

陕北子洲地区二叠纪山西组沉积环境

Sedimentary environment of Permian Shanxi Formation in Zizhou region,northern Shaanxi

  • 摘要: 针对陕北子洲地区山西组是否受海水影响的争议,对该组岩石进行了微量元素测试。结果显示山西组的古环境以淡水为主,但间或受海水的影响。根据野外露头和岩心观测,依据沉积旋回、岩电特征、沉积构造等,识别出研究区山西组为曲流河三角洲,发育三角洲前缘,以水下分流河道广泛发育为特征,并构成研究区天然气的主要储集砂体,可进一步划分为水下分流河道、分流间湾、间湾沼泽等微相;论述了山23段沉积微相的平面展布。

     

    Abstract: Aimed at the discussion that the paleo-environment was or not influenced by seawater when Shanxi Formation was deposited,microelement testing is analyzed.And the result shows that the water in paleo-environment mainly was freshwater,but periodly influenced by seawater.Applied with field outcrop and core description,combining with sedimentary cycle,the character of lithology and electromotive curve,sedimentary structure etc,the front delta in meandering delta of Shanxi Formation are identified in study area,in which subaqueous distributary channels were developed widely and was the main sand body for gas accumulation.Furthermore,sub-aqueous distributary channel,inter-distributary bay,inter-distributary swamp etc are main micro-facies in front delta.The sedimentary microfacies of Shan23 in plane are discussed.

     

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