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王利杰, 姚永坚, 孙珍, 李付成, 杨楚鹏, 徐子英. 2020. 南海东南部中生界识别及其构造属性[J]. 中国地质, 47(5): 1337-1354. doi: 10.12029/gc20200504
引用本文: 王利杰, 姚永坚, 孙珍, 李付成, 杨楚鹏, 徐子英. 2020. 南海东南部中生界识别及其构造属性[J]. 中国地质, 47(5): 1337-1354. doi: 10.12029/gc20200504
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WANG Lijie, YAO Yongjian, SUN Zhen, LI Fucheng, YANG Chupeng, XU Ziying. 2020. The discrimination of Mesozoic sequence and its tectonic attribute in the southeastern South China Sea[J]. Geology in China, 47(5): 1337-1354. doi: 10.12029/gc20200504
Citation: WANG Lijie, YAO Yongjian, SUN Zhen, LI Fucheng, YANG Chupeng, XU Ziying. 2020. The discrimination of Mesozoic sequence and its tectonic attribute in the southeastern South China Sea[J]. Geology in China, 47(5): 1337-1354. doi: 10.12029/gc20200504
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南海东南部中生界识别及其构造属性

  • 1.

    自然资源部海底矿产资源重点实验室, 中国地质调查局广州海洋地质调查局, 广东 广州 510760

  • 2.

    南方海洋科学与工程广东省实验室 (广州), 广东 广州 511458

  • 3.

    中国科学院南海海洋研究所边缘海与大洋地质重点实验室, 广东 广州 510301

  • 基金项目:
    中国地质调查局国家海洋专项项目（DD20160138, DD20201118）、南方海洋科学与工程广东省实验室（广州）人才团队引进重大专项（GML2019ZD0208）、广东省自然科学基金研究团队项目(2017A030312002)及国家自然科学基金项目（41606080）联合资助
详细信息
    作者简介: 王利杰, 男, 1982年生, 博士, 工程师, 主要从事海洋构造地质与地球物理研究; E-mail:ljwang@scsio.ac.cn
    通讯作者: 姚永坚, 女, 1964年生, 博士, 教授级高级工程师, 石油与天然气地质专业, 主要从事海洋油气地质和区域地质的综合研究; E-mail:yjyaomail@163.com

  • 中图分类号: P736.1;P714+.6

The discrimination of Mesozoic sequence and its tectonic attribute in the southeastern South China Sea

  • 1.

    MNR, Key Laboratory of Marine Mineral Resources, Guangzhou Marine Geological Survey, Guangzhou 510760, Guangdong China

  • 2.

    Southern Marine Science and Engineering Guangdong Laboratory(Guangzhou), Guangzhou 511458, Guangdong, China

  • 3.

    CAS, Key Laboratory of Ocean and Marginal Sea Geology, South China Sea Institute of Oceanology, Chinese Academy of Sciences, Guangzhou 510301, Guangdong, China

  • Fund Project: Supported jointly by Geological Survey Project (No. DD20160138,No. DD20201118), Key Special Project for Introduced Talents Team of Southern Marine Science and Engineering Guangdong Laboratory (Guangzhou) (No. GML2019ZD0208), Guangdong Natural Science Foundation Research Team Project (No. 2017A030312002), and National Natural Science Foundation of China (No. 41606080).
More Information
    Author Bio: WANG Lijie, male, born in 1982, engineer, mainly engages in the study of marine geology and geophysics; E-mail:ljwang@scsio.ac.cn .
    Corresponding author: YAO Yongjian, female, born in 1964, senior engineer, mainly engages in offshore petroleum geology and tectonic geology research; E-mail:yjyaomail@163.com

    摘要

  • 正确识别南海东南部中生界及其分布，对认识南海形成演化和油气资源潜力具有重要意义。受资料条件约束和地层系统划分差异的影响，南海东南部中生界分布和构造特征一直存在争议。本文在钻井、拖网约束下，通过井震对比、地震反射特征、层速度分析、岩浆岩体与地层接触关系和构造变形特征来综合识别中生界。结果表明，中生界呈平行、连续、低频的反射特征，层速度3400~4200 m/s，随着埋深或（和）变质程度增强，层速度增大（4500~5500 m/s），反射波组模糊，多数未见明显底界反射。研究区中生代地层发育局限，地震反射波组特征明显，但较难进行区域对比和解释。其中，西北、西南巴拉望盆地、礼乐滩和安渡北盆地中生界呈现低角度掀斜或近水平层状；礼乐滩西南部九章盆地中生界层速度3500~4500 m/s，高于上覆新生界，与钻井层速度吻合，地层呈高角度掀斜或挠曲变形，可能与岩浆活动侵位相关。结合中生代火山弧和识别的岩体分布，推测前者零散分布在弧前盆地靠火山弧一侧，构造活动相对弱，后者分布于岩浆活动强烈的弧间盆地。

    Discriminating the distribution of the Mesozoic strata on the southeastern South China Sea (SCS) continental margin is of great importance for understanding the SCS evolution as well as the oil and gas potential. Due to limited data constraints and varied stratigraphic system divisions, the distribution and tectonic features of the Mesozoic sequences in the southeastern SCS have remained controversial. Assisted by drilling and dredging data, the authors comprehensively identified the Mesozoic sequence using a combination of well-seismic comparison, seismic reflection characteristics, internal velocity analysis, contact relationship between igneous edifices and strata, and structural deformation characteristics. The results show that the Mesozoic sequence is characterized by parallel, continuous, and low-frequency reflections, with internal velocity of 3400-4200 m/s. As the burial depth or/and the degree of metamorphism increases, the internal velocity increases to 4500-5500 m/s. The seismic reflections of the Mesozoic strata in the depth is fuzzy, and most of them have no obvious bottom reflection. Despite the fact that the characteristics of seismic reflection are clear in a specific area, it is still difficult to make a comparative study and conduct a whole region seismic explanation because the range of the Mesozoic strata is limited. Among them, the Mesozoic strata in the Northwest, Southwest Palawan basin, Liyue and Andubei basin show low-angle tilting or nearly horizontal characteristics. By contrast, the Mesozoic strata in the northern part of Jiuzhang basin located in the southwest of Liyue have a velocity of 3500-4500 m/s, which is higher than the overlying Cenozoic velocity and coincides with the result constrained by drilling layer. In addition, the Mesozoic strata tilt or deflect at a high angle, which may be related to the emplacement of magmatic activity. Compared with the distribution of Mesozoic volcanic arc and identified igneous bodies, the authors infer that the first style Mesozoic strata are scattered in the forearc basin near volcanic arc and thus show a relatively weak tectonic activity, whereas the second style strata are distributed in the inter-arc basin and have a strong magmatic activity.

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  • 图 1  南海东南部地貌（Becker et al., 2009）、构造单元和地质背景分布图

    Figure 1. 

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    图 2  过西北巴拉望盆地和礼乐滩中生界地震反射特征（剖面位置见图 1a）

    Figure 2. 

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    图 3  西南巴拉盆地Pensacosa-1井和礼乐滩Sampaguita-1井地层速度(钻井位置见图 1a)

    Figure 3. 

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    图 4  不同时期岩浆岩体与围岩接触关系对比图(据Infante, 2018; Hansen and Cartwright, 2006修改)

    Figure 4. 

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    图 5  过九章盆地地震剖面及不同时期岩浆岩体与地层接触关系

    Figure 5. 

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    图 6  过西北、西南巴拉望盆地中、新生代地层组合及充填特征

    Figure 6. 

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    图 7  过礼乐滩西南部拖网站位SO27-21地震和层速度叠合剖面（a）及解释图（b）

    Figure 7. 

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    图 8  过九章和安渡北盆地构造地层解释剖面（a, b）、地质剖面图（c）和层速度剖面（d）

    Figure 8. 

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    图 9  南海东南部陆缘磁力化极、中生代火山弧、新生代裂后岩浆侵入体和中生界沉积盆地分布图（据Kudrass et al., 1986; Franke et al., 2008;2014 ；Chang et al., 2015；Dung et al., 2016; Li et al., 2018）

    Figure 9. 

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    图 10  主动型大陆边缘结构示意图（据李付成等，2012和Li et al., 2013修改）

    Figure 10. 

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    表 1  南海东南部陆缘盆地中生代地层钻井岩性及地质时代

    Table 1.  Drilling sites Mesozoic sediments and geological date in southeastern South China Sea basins

    下载: 导出CSV
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收稿日期:  2020-04-03
修回日期:  2020-07-08
刊出日期:  2020-10-25

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