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    赵学钦, 杨海军, 马青, 周成刚, 孙崇浩, 蔡泉, 孙仕勇. 塔北西部一间房组碳酸盐岩礁滩体同生期暴露溶蚀作用模式[J]. 中国地质, 2015, 42(6): 1811-1811.
    引用本文: 赵学钦, 杨海军, 马青, 周成刚, 孙崇浩, 蔡泉, 孙仕勇. 塔北西部一间房组碳酸盐岩礁滩体同生期暴露溶蚀作用模式[J]. 中国地质, 2015, 42(6): 1811-1811.
    ZHAO Xue-qin, YANG Hai-jun, MA Qin, ZHOU Cheng-gang, SUN Chong-hao, CAI Quan, SUN Shi-yong. Syn sedimentary corrosion mode of carbonate reef banks in the middle Ordovician Yijianfang Formation within the western Tabei uplift of Tarim Basin[J]. GEOLOGY IN CHINA, 2015, 42(6): 1811-1811.
    Citation: ZHAO Xue-qin, YANG Hai-jun, MA Qin, ZHOU Cheng-gang, SUN Chong-hao, CAI Quan, SUN Shi-yong. Syn sedimentary corrosion mode of carbonate reef banks in the middle Ordovician Yijianfang Formation within the western Tabei uplift of Tarim Basin[J]. GEOLOGY IN CHINA, 2015, 42(6): 1811-1811.

    塔北西部一间房组碳酸盐岩礁滩体同生期暴露溶蚀作用模式

    Syn sedimentary corrosion mode of carbonate reef banks in the middle Ordovician Yijianfang Formation within the western Tabei uplift of Tarim Basin

    • 摘要: 提要: 在详细的钻井资料和岩心的宏观及微观特征研究的基础上, 通过对塔北隆起西部奥陶系中统一间房组礁滩体沉积相特征及展布规律的分析, 结合礁滩体储层同生期溶蚀作用特征研究, 按照古沉积地貌单元结合岩相的方法建立了一间房组礁滩体同生期溶蚀作用模式。研究认为一间房组开阔台地相包括台内滩、滩间海和台内点礁3个亚相, 沉积相平面分布稳定; 一间房组的同生期暴露溶蚀作用明显, 普遍反映出滩体的间歇性暴露的特征: 生物钻孔和溶蚀孔洞内充填礁滩体暴露形成的古土壤泥; 发育潮间带的化石碎片堆积和软体生物活动遗迹; 岩心观察和成像测井可以识别出渗流-潜流带溶蚀作用旋回。按照礁滩相沉积地貌结合岩相的模式, 将一间房组开阔台地的浅滩和点礁沉积划分出潮上长期暴露滩、潮间间歇暴露滩、潮下高能滩、瓶筐石障积礁、潮汐水道等地貌单元。

       

      Abstract: Abstract: On the basis of the detailed drilling data and the core characteristics at the macro and micro level, by means of analyses about characteristics and distribution rules of sedimentary facies, in combination with reef?banks syn?sedimentary corrosion reservoir characteristics,and according to the ancient sedimentary geomorphic units combined with lithofacies, the authors established the syn?sedimentary corrosion model of reef?banks in the Middle Ordovician Yijianfang Formation in the western Tabei uplift of Tarim Basin. According to the results obtained, first, the open platform facies of Yijianfang Formation contain platform?interbank, interbank sea and platform?inter patch reef, and the plane distribution of facies is stable; second, Yijianfang Formation exhibits obvious characteristics of the syn?sedimentary corrosion and widely reflects the characteristics of the intermittent exposure of bank: boring pores and corrosion pores are filled with ancient mud soil formed by the exposure of reef banks, the intertidal zone fossil fragment accumulation and traces of soft?bodied organisms activities are common, the corrosion cycle from seepage to undercurrent belt can be identified by core observation and Image Logging. According to the model, the banks and patch reefs of Yijianfang Formation are classified into five geomorphic units, i.e., supralittoral long?term exposure bank, intertidal intermittent exposure bank, subtidal high?energy bank, Calathium baffles tone and tideway.

       

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