A heavy mineral viewpoint on sediment provenance and environment in the Qiongdongnan Basin

LIU Xiaofeng ZHANG Daojun ZHAI Shikui LIU Xinyu CHEN Hongyan LUO Wei LI Na XIU Chun

刘晓锋, 张道军, 翟世奎, 刘新宇, 陈宏言, 罗威, 李娜, 修淳. 琼东南盆地物源和沉积环境变化的重矿物证据[J]. 海洋学报英文版, 2015, 34(4): 41-55. doi: 10.1007/s13131-015-0648-1
引用本文: 刘晓锋, 张道军, 翟世奎, 刘新宇, 陈宏言, 罗威, 李娜, 修淳. 琼东南盆地物源和沉积环境变化的重矿物证据[J]. 海洋学报英文版, 2015, 34(4): 41-55. doi: 10.1007/s13131-015-0648-1
LIU Xiaofeng, ZHANG Daojun, ZHAI Shikui, LIU Xinyu, CHEN Hongyan, LUO Wei, LI Na, XIU Chun. A heavy mineral viewpoint on sediment provenance and environment in the Qiongdongnan Basin[J]. Acta Oceanologica Sinica, 2015, 34(4): 41-55. doi: 10.1007/s13131-015-0648-1
Citation: LIU Xiaofeng, ZHANG Daojun, ZHAI Shikui, LIU Xinyu, CHEN Hongyan, LUO Wei, LI Na, XIU Chun. A heavy mineral viewpoint on sediment provenance and environment in the Qiongdongnan Basin[J]. Acta Oceanologica Sinica, 2015, 34(4): 41-55. doi: 10.1007/s13131-015-0648-1

琼东南盆地物源和沉积环境变化的重矿物证据

doi: 10.1007/s13131-015-0648-1

A heavy mineral viewpoint on sediment provenance and environment in the Qiongdongnan Basin

  • 摘要: 基于11口钻井岩心样品的重矿物数据,结合古生物学、元素地球化学和地震资料,对琼东南盆地的物源及沉积环境演变进行了分析.结果表明,盆地基底沉积以陆相沉积为主,自渐新世起,盆地逐渐接受海侵,大致经历了海陆过渡→滨浅海→浅海→半深海的沉积环境演变过程,水深总体呈逐渐增大的趋势且在同一时期南部区域水深整体上大于北部.随着沉积环境的变化,各地层(崖城组至莺歌海组)物源呈现出多源性特征,经历了原地→近源→远源的演变过程.在渐新世早期,物源以近源玄武质火山碎屑和邻区陆源碎屑为主,之后演变为远源的陆壳碎屑,物源区包括北部海南岛、南部永乐隆起、东北部神狐隆起、西部红河、西南部中南半岛乃至更广的区域.海南岛物源自早渐新世便开始发育,至中中新世成为盆地最主要的物源,并持续至现今;永乐隆起和神狐隆起物源在晚渐新世至早中新世期间最为发育,于中中新世逐渐消退;红河物源于晚中新世大规模加入,为中央峡谷的主要沉积物源,影响至上新世结束;中南半岛莺西物源自上新世发育,影响至更新世时期.此外,自生组分对盆地(尤其是南部区域)的沉积贡献也不容忽视.
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  • 收稿日期:  2014-06-23
  • 修回日期:  2014-12-02

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