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    珠江口盆地珠江组混积岩中有孔虫的矿化特征与机制

    刘娜 吴克强 刘立 于雷 徐思萌 彭晓蕾

    刘娜, 吴克强, 刘立, 于雷, 徐思萌, 彭晓蕾, 2020. 珠江口盆地珠江组混积岩中有孔虫的矿化特征与机制. 地球科学, 45(10): 3746-3758. doi: 10.3799/dqkx.2020.079
    引用本文: 刘娜, 吴克强, 刘立, 于雷, 徐思萌, 彭晓蕾, 2020. 珠江口盆地珠江组混积岩中有孔虫的矿化特征与机制. 地球科学, 45(10): 3746-3758. doi: 10.3799/dqkx.2020.079
    Liu Na, Wu Keqiang, Liu Li, Yu Lei, Xu Simeng, Peng Xiaolei, 2020. Mineralization Characteristics and Mechanism of Foraminifera in Mixed Siliciclastic-Carbonate Sediments in Zhujiang Formation of Pearl River Mouth Basin. Earth Science, 45(10): 3746-3758. doi: 10.3799/dqkx.2020.079
    Citation: Liu Na, Wu Keqiang, Liu Li, Yu Lei, Xu Simeng, Peng Xiaolei, 2020. Mineralization Characteristics and Mechanism of Foraminifera in Mixed Siliciclastic-Carbonate Sediments in Zhujiang Formation of Pearl River Mouth Basin. Earth Science, 45(10): 3746-3758. doi: 10.3799/dqkx.2020.079

    珠江口盆地珠江组混积岩中有孔虫的矿化特征与机制

    doi: 10.3799/dqkx.2020.079
    基金项目: 

    中海油综合科研项目 CCL2015RCPS0150RCN

    国家自然科学基金 41202073

    国家自然科学基金 41572082

    详细信息
      作者简介:

      刘娜(1984-), 女, 博士, 讲师, 研究方向为储层成岩作用、流体-岩石相互作用.ORCID:0000-0002-2950-1285.E-mail:liuna_jlu@126.com

      通讯作者:

      刘立, E-mail:liuli0892@vip.sina.com

    • 中图分类号: P588.2

    Mineralization Characteristics and Mechanism of Foraminifera in Mixed Siliciclastic-Carbonate Sediments in Zhujiang Formation of Pearl River Mouth Basin

    • 摘要: 珠江口盆地白云凹陷是我国现今深水油气勘探的重要地区,在其南侧的荔湾X构造的珠江组在3 000~3 281 m以混积岩沉积为主.以荔湾X构造内含有孔虫混积岩为研究对象,通过开展岩石学和同位素地球化学研究,确定了有孔虫宿主岩石类型以及有孔虫矿化的岩相学特征,重点探讨了有孔虫的矿化机制,并最终建立了有孔虫的矿化模式.荔湾X构造珠江组混积岩的生物碎屑以有孔虫碎屑为主,有孔虫壳由刃状、等径状方解石或铁方解石组成.有孔虫的房室可分为未充填、半充填和全充填3种类型.根据有孔虫房室充填的主要自生矿物类型、产状及相互关系,可将有孔虫矿化按其形成的先后分为黄铁矿化、铁方解石化、片钠铝石化和铁白云石化4种类型,其中黄铁矿的形成可能与有孔虫软体组织的生物降解有关,铁方解石可能与有机质热脱羧作用有关,片钠铝石和铁白云石中的“碳”有深部来源的岩浆成因CO2的贡献.

       

    • 图  1  珠江口盆地荔湾X构造位置

      Fig.  1.  Research area in Liwan X of Pearl River Mouth basin

      图  2  珠江口盆地地层发育柱状图

      据李云(2012)和庞江(2018)

      Fig.  2.  Stratigraphic chart for the Pearl River Mouth basin

      图  3  混积岩三端元图及岩石类型投点

      底图据解习农等(2018)

      Fig.  3.  Composition diagram for mixed siliciclastic-carbonate sediment samples

      图  4  自生矿物典型镜下照片

      a.有孔虫体腔被黄铁矿部分充填,3 164.0 m,铸体薄片,单偏光;b.黄铁矿被放射状片钠铝石交代,二者共同填满有孔虫体腔,菱铁矿围绕有孔虫体腔外壁生长,染色后有孔虫体腔呈淡紫色,代表其主要成分为铁方解石,3 180.4 m,单偏光,染色薄片;c.有孔虫体腔内的铁方解石,3 226.3 m,染色薄片,单偏光;d.经染色后紫红色的铁方解石填满有孔虫体腔,3 101.0 m,染色薄片,单偏光;e.染色后呈淡紫色的铁方解石被不变色的菱形白云石交代,二者共同填满有孔虫体腔,另可见一有孔虫体腔被放射状的片钠铝石填满且完全交代,其原始体腔已消失不见,3 226.3 m;f.经染色后有孔虫体腔呈粉色,说明其成分为方解石,有孔虫体腔被铁白云石部分充填,3 164.0 m,染色薄片,单偏光;g.放射状的片钠铝石被自形的铁白云石交代,二者共同填满有孔虫体腔,注意有孔虫体腔已被片钠铝石完全交代,3 226.3 m,染色薄片,单偏光;h.同g,正交偏光.Pore.孔隙;Py.黄铁矿;Sd.菱铁矿;Fora.有孔虫;Daw.片钠铝石;FeC.铁方解石;Dol.白云石;Ank.铁白云石

      Fig.  4.  Micrographs of diagenetic minerals

      图  5  片钠铝石典型镜下照片

      a.放射状片钠铝石填满有孔虫体腔,经染色后体腔呈粉色,表示体腔成分为方解石,体腔壁由粒状方解石(蓝色箭头)和纤维状方解石(红色箭头)共同组成,3 213.8 m,染色薄片,单偏光;b.有孔虫体腔被放射状片钠铝石部分充填,3 180.0 m,染色薄片,单偏光;c.有孔虫体腔壁被放射状片钠铝石完全交代,3 226.3 m,正交偏光;d.有孔虫体腔被片钠铝石和铁白云石填满,二者分隔在相邻体腔内,3 164.0 m染色薄片,单偏光;e.多个有孔虫体腔被片钠铝石和铁白云石分别填满,注意被片钠铝石充填的有孔虫,其体腔壁已消失不见,3 226.3 m,染色薄片,单偏光;f.同g,正交偏光.Pore.孔隙;Fora.有孔虫;Daw.片钠铝石;Ank.铁白云石

      Fig.  5.  Micrographs of dawsonite in mixed siliciclastic-carbonate sediments

      图  6  荔湾X构造珠江组片钠铝石碳、氧同位素特征

      ①本次研究;②Baker et al.(1995), Uysal et al.(2011);③Golab et al.(2006);④Ferrini et al.(2003);⑤Zhao et al.(2018);⑥Liu et al.(2011);⑦Ming et al.(2017);⑧Gao et al.(2009);⑨董林森等(2011);⑩Zalba et al.(2011)

      Fig.  6.  Plot of δ13C versus δ18O values for dawsonite of Zhujiang Formation in Liwan X

      图  7  有孔虫壳的矿化模式

      Fig.  7.  Mineralization model of the foraminiferal

      表  1  荔湾X构造珠江组方解石、铁白云石、片钠铝石碳、氧同位素特征

      Table  1.   Carbon and oxygen isotopic compositions for calcite, ankerite and dawsonite of Zhujiang Formation in Liwan X

      埋深(m) 矿物 δ13C(‰, VPDB) δ18O(‰, VPDB) δ18O(‰, SMOW) 平衡的δ13CCO2(‰, VPDB)
      3 202 方解石 -3.8 -6.4 24.3 /
      3 277 方解石 -5.7 -8.6 22.1 /
      3 157 铁白云石 -1.1 -5.9 24.9 /
      3 202 铁白云石 -2.0 -4.9 25.9 /
      3 277 铁白云石 -4.6 -7.6 23.1 /
      3 424 铁白云石 -2.5 -8.1 22.6 /
      3 157 片钠铝石 -0.1 -4.9 25.8 -5.4
      3 277 片钠铝石 -4.7 -8.4 22.2 -9.1
      3 424 片钠铝石 -2.3 -8.4 22.2 -6.4
      注:与片钠铝石平衡的δ13CCO2 (‰,PDB)数据系根据实测值和方解石-CO2分馏方程(Ohmoto and Rye, 1979)及相关参数计算.
      下载: 导出CSV
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    • 收稿日期:  2019-12-30
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