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    Volume 46 Issue 5
    May  2021
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    Article Navigation >  Earth Science  > 2021  >  46(5): 1783-1796
    Zhang Qingqing, Liu Keyu, Heng Liqun, Liu Taixun, Lu Yan, Sun Runping, Wang Jian, 2021. Characteristics and Genetic Distribution Model of Top Calcareous Cementation Layers within Zhujiang Formation in Panyu A Oilfield, Pearl River Mouth Basin. Earth Science, 46(5): 1783-1796. doi: 10.3799/dqkx.2020.139
    Citation: Zhang Qingqing, Liu Keyu, Heng Liqun, Liu Taixun, Lu Yan, Sun Runping, Wang Jian, 2021. Characteristics and Genetic Distribution Model of Top Calcareous Cementation Layers within Zhujiang Formation in Panyu A Oilfield, Pearl River Mouth Basin. Earth Science, 46(5): 1783-1796. doi: 10.3799/dqkx.2020.139
    shu

    Characteristics and Genetic Distribution Model of Top Calcareous Cementation Layers within Zhujiang Formation in Panyu A Oilfield, Pearl River Mouth Basin

    doi: 10.3799/dqkx.2020.139
    • 1.

      School of Geosciences, China University of Petroleum, Qingdao 266580, China

    • 2.

      Evaluation and Detection Technology Laboratory for Marine Mineral Resources, Qingdao National Laboratory for Marine Science and Technology, Qingdao 266071, China

    • 3.

      Research Institute of Petroleum Exploration & Development, Shenzhen Branch of China National Offshore Oil Corporation Limited, Shenzhen 518054, China

    • Received Date: 2020-06-21
    • Publish Date: 2021-05-15
      Abstract
    • Top calcareous cementation layers (TCCLs) are common type of carbonate cement that caps reservoir sandstone units. There is no consensus on the genetic mechanism of TCCLs at present and thus hindering our understanding of its distribution prediction and restricting the oilfield exploration and development. In this paper a suite of analytical techniques were employed to investigate the genesis and distribution of TCCLs within the Zhujiang Formation in the Panyu A oilfield, Pearl River Mouth basin, including core and log analysis, XRF scanning, casting thin section, scanning electron microscopy, cathodoluminescence, electron microprobe, stable carbon and oxygen isotopes. This enabled us to systematically study the log responses, petrologic characteristics, material source and genesis, distribution patterns, and genetic distribution model of TCCLs. TCCLs in the study area comprise mainly gravel-bearing sandstone and medium-coarse sandstone, and the carbonate cements consist mostly of ferrocalcite in basement-pore contacts accompanied by biological debris, and its precipitation temperature is between 55.9 and 72 ℃. The thickness of TCCLs is mainly in the range of 0.4-1.2 m, but there exist big differences between the thickness and development percentage of TCCLs among different oil-bearing reservoir beds. The analysis indicates that TCCLs were formed in the early diagenetic stage and their material sources are mainly composed of endogenous biological debris. The distribution of TCCLs is mainly controlled by sedimentary microfacies and high-frequency sequence stratigraphy surfaces. The estuary bars provide an important material source, and the superposition of each other contributes to the contiguous thickening of TCCLs, while the high-frequency marine-flooding surface can further promote the development of TCCLs by extending the retention time of sediments. The genesis and distribution of TCCLs in the study area are primarily controlled by the enrichment degree and distribution of bio-debris. Therefore, the spatial distribution of TCCLs can be predicted through the analysis of high-frequency sequence stratigraphy and detailed microfacies characterization.

       

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