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南海北部琼东南盆地中央峡谷成因新认识

王亚辉 张道军 赵鹏肖 陈扬 黄灿 苏榆丰

王亚辉, 张道军, 赵鹏肖, 陈扬, 黄灿, 苏榆丰. 南海北部琼东南盆地中央峡谷成因新认识[J]. 海洋学报, 2016, 38(11): 97-104. doi: 10.3969/j.issn.0253-4193.2016.11.009
引用本文: 王亚辉, 张道军, 赵鹏肖, 陈扬, 黄灿, 苏榆丰. 南海北部琼东南盆地中央峡谷成因新认识[J]. 海洋学报, 2016, 38(11): 97-104. doi: 10.3969/j.issn.0253-4193.2016.11.009
Wang Yahui, Zhang Daojun, Zhao Pengxiao, Chen Yang, Huang Can, Su Yufeng. A new consideration on the genetic mechanism of the central canyon in the Qiongdongnan Basin, the northern South China Sea[J]. Haiyang Xuebao, 2016, 38(11): 97-104. doi: 10.3969/j.issn.0253-4193.2016.11.009
Citation: Wang Yahui, Zhang Daojun, Zhao Pengxiao, Chen Yang, Huang Can, Su Yufeng. A new consideration on the genetic mechanism of the central canyon in the Qiongdongnan Basin, the northern South China Sea[J]. Haiyang Xuebao, 2016, 38(11): 97-104. doi: 10.3969/j.issn.0253-4193.2016.11.009

南海北部琼东南盆地中央峡谷成因新认识

doi: 10.3969/j.issn.0253-4193.2016.11.009
基金项目: 国家科技重大专项(2011ZX05025)。

A new consideration on the genetic mechanism of the central canyon in the Qiongdongnan Basin, the northern South China Sea

  • 摘要: 通过对区域构造断裂体系和逐渐连片的高分辨率三维地震资料的精细解析,认识到琼东南盆地中央峡谷的形成机制除了与晚中新世区域构造变动、大规模海平面下降、充足物源供给以及凹槽型古地形特征等因素相关之外,还存在另外一个非常重要因素:峡谷底部早期隐伏断裂带的存在。研究表明:琼东南盆地中央坳陷带发育平行于陆架坡折的大规模深水峡谷,峡谷底部发育大型走滑断层以及走滑断层派生出一系列次级断层形成的地层破碎带,认识到峡谷的形成、规模以及展布方向均受断裂带影响;相应地峡谷的充填及演化亦是受物源、海平面变化、重力流作用等多种因素共同作用和相互叠加的过程。从而为研究经历了裂陷期和坳陷期盆地演化过程形成的大型峡谷提供了科学依据。
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  • 收稿日期:  2016-04-20
  • 修回日期:  2016-07-15

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