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    青藏高原东北缘循化盆地渐新世—上新世沉积相分析与沉积演化

    张楗钰 张克信 季军良 骆满生 陈奋宁 徐亚东 王岳明

    张楗钰, 张克信, 季军良, 骆满生, 陈奋宁, 徐亚东, 王岳明, 2010. 青藏高原东北缘循化盆地渐新世—上新世沉积相分析与沉积演化. 地球科学, 35(5): 774-788. doi: 10.3799/dqkx.2010.091
    引用本文: 张楗钰, 张克信, 季军良, 骆满生, 陈奋宁, 徐亚东, 王岳明, 2010. 青藏高原东北缘循化盆地渐新世—上新世沉积相分析与沉积演化. 地球科学, 35(5): 774-788. doi: 10.3799/dqkx.2010.091
    ZHANG Jian-yu, ZHANG Ke-xin, JI Jun-liang, LUO Man-sheng, CHEN Fen-ning, XU Ya-dong, WANG Yue-ming, 2010. Oligocene-Pliocene Sedimentary Facies Analysis and Sedimentary Evolution of Xunhua Basin in Northeastern Margin of Qinghai-Tibet Plateau. Earth Science, 35(5): 774-788. doi: 10.3799/dqkx.2010.091
    Citation: ZHANG Jian-yu, ZHANG Ke-xin, JI Jun-liang, LUO Man-sheng, CHEN Fen-ning, XU Ya-dong, WANG Yue-ming, 2010. Oligocene-Pliocene Sedimentary Facies Analysis and Sedimentary Evolution of Xunhua Basin in Northeastern Margin of Qinghai-Tibet Plateau. Earth Science, 35(5): 774-788. doi: 10.3799/dqkx.2010.091

    青藏高原东北缘循化盆地渐新世—上新世沉积相分析与沉积演化

    doi: 10.3799/dqkx.2010.091
    基金项目: 

    中国地质调查局项目 1212010610103

    国家自然科学基金项目 40921062

    国家自然科学基金项目 40830312

    详细信息
      作者简介:

      张楗钰(1986-), 男, 硕士研究生, 主要从事沉积学及微体古生物学研究.E-mail: zjyttd@163.com

      通讯作者:

      张克信, E-mail: kx_zhang@cug.edu.cn

    • 中图分类号: P542

    Oligocene-Pliocene Sedimentary Facies Analysis and Sedimentary Evolution of Xunhua Basin in Northeastern Margin of Qinghai-Tibet Plateau

    • 摘要: 位于循化盆地南缘的积石镇羊圈贡拜—西沟上庄剖面发育连续完整的晚渐新世—上新世地层, 从老至新依次出露渐新统—中新统他拉组、中新统咸水河组(中庄段、上庄段、东乡段)和中新统—上新统临夏组(柳树段和何王家段).沉积相分析认为, 他拉组以冲积扇相为主, 咸水河组以富含膏盐层的咸化湖相—三角洲前缘相为主, 临夏组以湖相—三角洲前缘相夹水下扇相为主.通过对沉积序列中古流向的系统测量和分析, 揭示他拉组、咸水河组沉积期的古水流方向多在SE-NW之间, 结合物源分析, 表明当时西秦岭北缘逆冲带和拉脊山逆冲带均已隆起并遭受剥蚀成为循化盆地沉积物的物源供应区; 而在临夏组沉积期, 古水流以NWW为主, 推测循化盆地东部的积石山隆起成为物源的主要供应区.剖面粒度概率累积曲线和C-M图分析结果印证了对剖面沉积相的划分, 并指示盆地沉积时期的三角洲前缘和水下扇发育区存在牵引流.

       

    • 图  1  研究区地质简图及剖面位置

      1.第四系;2.上新统积石组;3.中—上新统临夏组;4.中新统咸水河组;5.渐新统—中新统他拉组;6.下白垩统河口群;7.中—上三叠统古浪堤组;8.元古宇化隆岩群;9.角度不整合;10.断层;11.实测剖面

      Fig.  1.  Geological map of studied area and the location of the measured section

      图  2  青海省循化县积石镇羊圈贡拜渐新统—中新统实测剖面岩性岩相柱状图

      1.砾岩; 2.含砾砂岩; 3.石英砂岩; 4.砂岩; 5.粉砂岩; 6.泥质粉砂岩; 7.粉砂质泥岩; 8.泥岩; 9.灰岩; 10.石膏; 11.基性岩; 12.超基性岩; 13.变质岩; 14.其他; 15.平行层理; 16.水平层理; 17.板状交错层理; 18.楔状交错层理; 19.槽状交错层理; 20.不对称波痕; 21.叠瓦状构造; 22.爬升层理; 23.古流向; 24.钙质泥岩

      Fig.  2.  Lithological and lithofacies column for the measured section of Oligocene-Miocene in Yangjuangongbai, Jishi Town, Xunhua County, Qinghai Province

      图  3  青海省循化县积石镇羊圈贡拜—西沟上庄中新统实测剖面岩性岩相柱状图(图例参见图 2)

      Fig.  3.  Lithological and lithofacies column for the measured section of Miocene in Yangjuangongbai-Xigoushangzhuang, Jishi Town, Xunhua County, Qinghai Province

      图  4  青海省循化县积石镇西沟上庄中新统—上新统实测剖面岩性岩相柱状图(图例参见图 2)

      Fig.  4.  Lithological and lithofacies column for the measured section of Miocene-Pliocene in Xigoushangzhuang, Jishi Town, Xunhua County, Qinghai Province

      图  5  青海省循化县积石镇羊圈贡拜村渐新世—中新世地层沉积构造

      a.冲积扇相的扇根沉积,叠瓦状排列的砾石,剖面第5层底部;b.淡水湖相的滨湖沉积,具沙纹层理的钙质粉砂岩,第52层上部;c.上庄段和东乡段下部层序;d.半咸水湖相的浅湖沉积,为蓝灰、灰绿色膏泥岩夹白色薄层石膏,第81层;e.三角洲前缘的分支河道沉积,具底冲刷面和正粒序层理的含砾砂岩,第97层;f.淡水湖相的浅湖沉积,钙质泥岩中的水平层理,第99层和第100层

      Fig.  5.  Sedimentary structures of the Oligocene-Miocene strata in Yangjuangongbai Village, Jishi Town, Xunhua County, Qinghai Province

      图  6  青海省循化县积石镇羊圈贡拜—西沟上庄渐新统—上新统实测剖面各沉积相粒度概率累积频率

      样品的粒度测试在中国地质大学生物地质与环境地质教育部重点实验室LASER粒度仪室内完成.测量仪器为LS230激光粒度分析仪,测量范围为0.04~2 000 μm.样品层位:1.他拉组第7层;2.他拉组第9层;3.他拉组第12层;4.他拉组第18层;5.咸水河组中庄段第26层;6.咸水河组中庄段第54层;7.咸水河组中庄段第58层;8.咸水河组中庄段第34层;9.咸水河组中庄段第35层;10.咸水河组中庄段第38层;11.咸水河组中庄段第47层;12.咸水河组东乡段第119层;13.咸水河组中庄段第55层;14.临夏组柳树段第150层;15.临夏组柳树段第163层

      Fig.  6.  Grain size probability accumulative curves of the various sedimentary facies for the measured section of Oligocene-Pliocene in Yangjuangongbai-Xigoushangzhuang, Jishi Town, Xunhua County, Qinghai Province

      图  7  青海省循化县积石镇西沟上庄中新世—上新世地层沉积构造

      a.三角洲前缘泥岩—粉砂岩层中的水下分支河道充填的砂岩透镜体,第107层;b.东乡段中下部的三角洲前缘沙坝沉积和淡水浅湖相具水平和平行层理的泥岩—粉砂岩层;c.三角洲前缘的水下分支河道沉积,为具楔状交错层理的含砾砂岩,第112层底部;d.三角洲前缘的水下分支河道沉积,具板状交错层理的细砾岩,第114层;e.水下扇相沉积,为具叠瓦状构造与平行层理的砾岩及含砾砂岩,第159层底部;f.三角洲前缘沙坝沉积,具叠瓦状的的砾岩夹层,第163层

      Fig.  7.  Sedimentary structures of the Miocene-Pliocene strata in Xigoushangzhuang Village, Jishi Town, Xunhua County, Qinghai Province

      图  8  青海省循化县积石镇羊圈贡拜—西沟上庄渐新统—上新统实测剖面样品粒度C-M

      取样层位及其沉积环境:1.他拉组:1A.扇根相(第9层);1B.扇中相(第8层、10层、12层、14层);1C.扇端相(第17层、18层);1D.浅湖相(第20层);2.咸水河组中庄段:2A.浅湖相(第26层、30层、52层、54层、56层、58层);2B.滨湖相(第34层、35层、38层、44层、45层);2C.沙坝相(第50层、55层);2D.分支河道相(第47层);3.咸水河组上庄段浅湖相(第59层、60层、70层、78层);4.咸水河组东乡段:4A.浅湖相(第118层、121层、125层、149层);4B.滨湖相(第126层、143层);4C.分支河道相(第119层);5.临夏组柳树段:5A.浅湖相(第150层、158层、172层);5B.扇中相(第161层);5C.沙坝相(第150层、163层);5D.分支河道相(第166层);6.临夏组何王家段:6A.浅湖相(第188层、206层);6B.沙坝相(第191层、193层);6C.扇中相(第182层);6D.扇端相(第178层)

      Fig.  8.  C-M pattern of the samples for measured section of Oligocene-Pliocene in Yangjuangongbai-Xigoushangzhuang, Jishi Town, Xunhua County, Qinghai Province

      图  9  青海省循化县积石镇羊圈贡拜—西沟上庄渐新统—上新统实测剖面岩性岩相柱状图

      Fig.  9.  Lithological and lithofacies column for the measured section of Oligocene-Pliocene in Yangjuangongbai-Xigoushangzhuang, Jishi Town, Xunhua County, Qinghai Province

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    • 收稿日期:  2010-05-31
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