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南海北部双峰南陆坡深水区早-中中新世沉积充填特征及其影响因素

钱星 张莉 易海 韦振权 帅庆伟

钱星, 张莉, 易海, 韦振权, 帅庆伟. 南海北部双峰南陆坡深水区早-中中新世沉积充填特征及其影响因素[J]. 石油实验地质, 2015, 37(6): 751-757. doi: 10.11781/sysydz201506751
引用本文: 钱星, 张莉, 易海, 韦振权, 帅庆伟. 南海北部双峰南陆坡深水区早-中中新世沉积充填特征及其影响因素[J]. 石油实验地质, 2015, 37(6): 751-757. doi: 10.11781/sysydz201506751
Qian Xing, Zhang Li, Yi Hai, Wei Zhenquan, Shuai Qingwei. Sedimentary filling characteristics and the main controlling factors during the Early-Middle Miocene in the deep-water area of Shuangfengnan Slope in the northern South China Sea[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2015, 37(6): 751-757. doi: 10.11781/sysydz201506751
Citation: Qian Xing, Zhang Li, Yi Hai, Wei Zhenquan, Shuai Qingwei. Sedimentary filling characteristics and the main controlling factors during the Early-Middle Miocene in the deep-water area of Shuangfengnan Slope in the northern South China Sea[J]. PETROLEUM GEOLOGY & EXPERIMENT, 2015, 37(6): 751-757. doi: 10.11781/sysydz201506751

南海北部双峰南陆坡深水区早-中中新世沉积充填特征及其影响因素

doi: 10.11781/sysydz201506751
基金项目: 国土资源部海底矿产资源重点实验室开放基金项目(KLMMR-2013-A-11)及"南海北部陆坡及台湾海峡盆地西部油气地质特征及赋存规律研究"项目([2013]GZH002-31)资助。
详细信息
    作者简介:

    钱星(1985—),男,工程师,从事海洋地质方面的生产及科研工作。E-mail:qian.xing@foxmail.com

  • 中图分类号: TE121.3

Sedimentary filling characteristics and the main controlling factors during the Early-Middle Miocene in the deep-water area of Shuangfengnan Slope in the northern South China Sea

  • 摘要: 深水陆坡沉积是近年来我国海域油气勘探关注的重点。利用二维多道地震剖面及周边钻井资料,以外部形态和内部结构相结合的方式对南海北部双峰南陆坡区早-中中新世地层进行地震相分析,识别出斜交型前积、丘状前积、席状杂乱、席状平行4种地震相类型。结合研究区古地理及其邻区同时期的构造-沉积演化分析,认为其主要发育了陆架边缘三角洲、斜坡扇及滑塌体3种典型的沉积体,它们的发育与演化是构造运动、相对海平面变化及物源三方因素相互作用的结果。以华南及古珠江供源的三角洲体系是影响陆坡区沉积体系发育的最重要因素,是沉积体系发育的物质基础,构造运动和相对海平面变化为陆坡区沉积体系的发育提供了可容纳空间。

     

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出版历程
  • 收稿日期:  2014-10-17
  • 修回日期:  2015-10-09
  • 刊出日期:  2015-11-28

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