Detrital Zircon Provenance of Upper Mingyuefeng Formation in West Slope of Lishui-Jiaojiang Sag, the East China Sea
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摘要: 沉积物源对油气储层发育具有重要影响.为研究丽水-椒江凹陷西斜坡明月峰组上段物源的岩性组成及其分布特征，选取4口钻井4个砂岩样品进行碎屑锆石U-Pb定年，并对陆上潜在物源区岩层(体)的岩性和年龄进行统计分析.结果显示：(1)样品中碎屑锆石以岩浆锆石为主，主要的年龄区间为125~90 Ma、145~125 Ma及170~145 Ma，还有少量变质锆石，其年龄区间为235~210 Ma及2 087~1 653 Ma；(2)陆上潜在物源区中以火山岩占绝对优势(173~94 Ma)，局部区域可能有较大规模白垩系永康群沉积岩，而变质岩(＞210 Ma)和侵入岩(107.0~87.8 Ma)仅零星出露.综合分析认为：研究区东北部明月峰组上段的物源以永康群火山-沉积岩和九里坪组火山岩为主，含有少量晚白垩世侵入岩；西南部以九里坪组、西山头组火山岩及元古代区域变质岩为主，侏罗纪火山岩为辅，这一区域可能更有利于优质储层的发育.
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关键词:
- 碎屑锆石U-Pb定年 /
- 明月峰组上段 /
- 物源 /
- 丽水-椒江凹陷 /
- 沉积物
Abstract: Sedimentary source has a significant impact on the development of oil and gas reservoir. To differentiate the provenance and analyze the lithological composition of the source area of the upper Mingyuefeng Formation in the west slope of Lishui-Jiaojiang sag, 4 detrital zircon samples from 4 drillings were selected for U-Pb isotopic dating, and then provenance analysis was conducted according to the dating results and the age and lithology of potential source. The results suggest that detrital zircons are mainly dominated by magmatic zircons falling into the age ranges of 125-90 Ma, 145-125 Ma and 170-145 Ma, and there are a small amount of metamorphic zircons aged 235-210 Ma and 2 087-1 653 Ma. In the potential source area, volcanic rocks in the age range of 168-94 Ma are in overwhelming majority, and metamorphic rocks older than 210 Ma and intrusive rocks formed in 107.0-87.8 Ma outcrop sporadically, while maybe there are sedimentary rocks of Yongkang Group concentrated locally. The comprehensive analysis shows that the provenance of the northeastern part of the study area was mainly volcanic-sedimentary rocks of Yongkang Group and volcanic of Jiuliping Formation and Late Cretaceous intrusions exposed locally. While in the southwestern part, the source rock was mainly Proterozoic metamorphic rocks and volcanic rocks from Xishantou Formation in addition to Jiuliping Formation, and a small amount of Jurassic volcanic rocks as well., which is more favorable to the development of high-quality reservoir in the southwestern part. -
图 1 丽水-椒江凹陷及潜在物源区地质
据浙江省地质矿产局(1989)和福建省地质矿产局(1985)修改；瓯江流域样品位置据Xu et al.(2007)；侵入岩体年龄据邱检生等(2008, 2011)、李艳军等(2009, 2010)和He and Xu(2012)
Fig. 1. Geology of Lishui-Jiaojiang sag and potential source area
图 2 丽水-椒江凹陷沉积地层综合柱状图(a)和浙东南地层区前新生代地层综合柱状图(b)
图a据田兵等(2012)修改；图b岩性据张国全等(2012)和浙江省地质矿产局(1989)
Fig. 2. Comprehensive stratigraphic column in Lishui-Jiaojiang sag (a) and comprehensive Pre-Cenozoic stratigraphic column of southeastern Zhejiang stratigraphic region (b)
图 4 丽水-椒江凹陷碎屑锆石典型CL图像特征
Fig. 4. Cathodoluminscence (CL) image of typical detrital zircons from Lishui-Jiaojiang sag
图 6 丽水凹陷明月峰组碎屑锆石年龄谱(n为测试锆石颗粒数)
Fig. 6. Detrital-zircon age-spectra from Mingyuefeng Formation in Lishui sag
图 7 浙闽沿海晚中生代火山岩锆石及瓯江流域碎屑锆石U-Pb年龄累积概率曲线
瓯江流域数据据文献Xu et al.(2007)；浙闽火山岩数据据文献余明刚等(2006)、邢光福等(2008)、Li et al.(2009)、崔玉荣等(2010)、Guo et al.(2012)、Liu et al.(2012)、Hu et al.(2012)和段政等(2013)
Fig. 7. Cumulative probability curve of zircon U-Pb age of Oujiang River and late Mesozoic volcanic rocks around Fujian and Zhejiang coastal
图 8 闽浙陆域前新生代不同岩层(体)锆石U-Pb年龄分布
数据据赵磊(2012)、Xu et al.(2007)、胡艳华等(2011)、向华等(2008)、陈多福等(1998)、Wan et al.(2007)、Li et al.(2014)、邱检生等(2008, 2011)、李艳军等(2009, 2010)、He and Xu(2012)和Guo et al.(2012)
Fig. 8. The distribution of zircon U-Pb ages in the different Pre-Cenozoic strata(intrusive mass) of Fujian and Zhejiang region
表 1 瓯江及飞云江-鳌江流域岩层(体)和岩性分布
Table 1. Rocks and its lithological distribution in Oujiang and Feiyunjiang-Aojiang River
瓯江流域(18 168.75 km2) 飞云江-鳌江流域(6 630.00 km2) 岩层(体) 面积(%) 沉积岩 面积(%) 沉积岩 剖面(%) 权重比例(%) 剖面(%) 权重比例(%) 永康群 方岩组 1.3 沉积岩为主 1.3 0 馆头组 3.4 31.0~88.3 1.1~3.0 10.8 沉积岩 10.8 朝川组 1.8 31.8~93.3 0.6~1.7 15.3 31.8~70.0 4.9~10.7 磨石山群 九里坪组 5.1 极少 0 5.8 极少 0 茶湾组 0.1 沉积岩为主 0.1 0.4 沉积岩为主 0.4 西山头组 30.8 0~3.6 0~1.1 28.1 0.7~19.0 0.02~5.30 高坞组 24.8 0~7.8 0~1.9 10.4 极少 0 大爽组 12.7 极少~39.5 0~5 0 0 变质岩 5.2 0 0 0 侵入岩 9.1 0 0 12.3 第四纪 4.5 28.3 其他 1.1 1.1 0.8 0.8 总计(第四纪除外) 火山岩+变质岩+侵入岩79.8%~91.7% 沉积岩+其他9.3%~20.2% 注：沉积岩权重比例(%)=流域内岩层面积比(%)×剖面中沉积岩厚度比例(%)，其他为长林组(沉积岩为主)和祝村组(无锆石U-Pb定年数据)，剖面沉积岩比例据浙江省地质矿产局(1989)和张国全等(2012). 
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