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    浅海背景下大型重力流沉积体能堆积与发育吗?

    王华 陈思 蒋恕

    王华, 陈思, 蒋恕, 2022. 浅海背景下大型重力流沉积体能堆积与发育吗?. 地球科学, 47(10): 3867-3868. doi: 10.3799/dqkx.2022.843
    引用本文: 王华, 陈思, 蒋恕, 2022. 浅海背景下大型重力流沉积体能堆积与发育吗?. 地球科学, 47(10): 3867-3868. doi: 10.3799/dqkx.2022.843
    Wang Hua, Chen Si, Jiang Shu, 2022. Can Large Gravity Flow Deposits Accumulate and Develop in Shallow Marine?. Earth Science, 47(10): 3867-3868. doi: 10.3799/dqkx.2022.843
    Citation: Wang Hua, Chen Si, Jiang Shu, 2022. Can Large Gravity Flow Deposits Accumulate and Develop in Shallow Marine?. Earth Science, 47(10): 3867-3868. doi: 10.3799/dqkx.2022.843

    浅海背景下大型重力流沉积体能堆积与发育吗?

    doi: 10.3799/dqkx.2022.843
    详细信息
      作者简介:

      王华(1964-),男,教授,博士生导师,主要从事沉积地质学、层序地层学研究.ORCID:0000-0003-2750-6258.E-mail:wanghua@cug.edu.cn

    Can Large Gravity Flow Deposits Accumulate and Develop in Shallow Marine?

    • [1] Huang, Y. T., Tan, X. F., Liu, E. T., et al., 2021. Sedimentary Processes of Shallow-Marine Turbidite Fans: an Example from the Huangliu Formation in the Yinggehai Basin, South China Sea. Marine and Petroleum Geology, 132: 105191. https://doi.org/10.1016/j.marpetgeo.2021.105191
      [2] Liu, E. T., Wang, H., Li, Y., et al., 2014. Sedimentary Characteristics and Tectonic Setting of Sublacustrine Fans in a Half-Graben Rift Depression, Beibuwan Basin, South China Sea. Marine and Petroleum Geology, 52: 9-21. https://doi.org/10.1016/j.marpetgeo.2014.01.008
      [3] McCaffrey, W., Kneller, B., 2001. Process Controls on the Development of Stratigraphic Trap Potential on the Margins of Confined Turbidite Systems and Aids to Reservoir Evaluation. AAPG Bulletin, 85: 971-988. https://doi.org/10.1306/8626ca41-173b-11d7-8645000102c1865d
      [4] Okay, S., Jupinet, B., Lericolais, G., et al., 2011. Morphological and Stratigraphic Investigation of a Holocene Subaqueous Shelf Fan, North of the İstanbul Strait in the Black Sea. Turkish Journal of Earth Sciences, 20: 287-305. https://doi.org/10.3906/yer-1001-16
      [5] Shao, L., Cao, L. C., Qiao, P. J., et al., 2017. Cretaceous-Eocene Provenance Connections between the Palawan Continental Terrane and the Northern South China Sea Margin. Earth and Planetary Science Letters, 477: 97-107. https://doi.org/10.1016/j.epsl.2017.08.019
      [6] Tokuhashi, S., 1996. Shallow-Marine Turbiditic Sandstones Juxtaposed with Deep-Marine Ones at the Eastern Margin of the Niigata Neogene Backarc Basin, Central Japan. Sedimentary Geology, 104(1-4): 99-116. https://doi.org/10.1016/0037-0738(95)00123-9
      [7] 操应长, 金杰华, 刘海宁, 等, 2021. 中国东部断陷湖盆深水重力流沉积及其油气地质意义. 石油勘探与开发, 48(2): 247-257. https://www.cnki.com.cn/Article/CJFDTOTAL-SKYK202102003.htm
      [8] 王策, 2016. 莺歌海盆地上中新统—更新统储层物源识别: 来自碎屑锆石U-Pb年代学和地球化学制约. 广州: 中国科学院研究生院(广州地球化学研究所).
      [9] 王亚辉, 张道军, 陈杨, 等, 2018. 琼东南盆地三亚组陆架边缘三角洲的发现及其油气勘探意义. 地质科技情报, 37(5): 30-36. https://www.cnki.com.cn/Article/CJFDTOTAL-DZKQ201805005.htm
      [10] 谢玉洪, 童传新, 裴健翔, 等, 2016. 莺歌海盆地黄流组二段碎屑锆石年龄与储层物源分析. 大地构造与成矿学, 40(3): 517-530.
      [11] 钟泽红, 张迎朝, 何小胡, 等, 2015. 莺歌海盆地东方区黄流组层序叠加样式与海底扇内部构型. 海洋地质与第四纪地质, 35(2): 91-99.
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    • 刊出日期:  2022-10-25

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