南海晚中新世&mdash;上新世红河沉积体系研究

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南海晚中新世—上新世红河沉积体系研究

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中图分类号: P512.2

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文章访问数: 2101
HTML全文浏览量: 1
PDF下载量: 777
被引次数: 0

Research on Red River Sedimentary System of late MioceneEarly Pliocene, South China Sea

摘要

摘要: 红河沉积体系为南海西北部近期新发现的大型远源沉积体系，其主要发育于南海莺歌海盆地和琼东南盆地。重点利用大量二维地震剖面资料，根据地震反射特征对晚中新世—上新世红河沉积体系的识别特征以及平面展布进行了研究，以此为基础划分了红河沉积体系在晚中新世—上新世演化阶段。研究结果表明：通过地震反射特征的分析，可以识别出三角洲、水下下切水道、海底峡谷、水道堤岸复合体以及海底扇朵体等沉积；依据红河沉积体系的平面组合和展布特征，可将晚中新世至上新世的红河沉积体系演化划分为3个阶段：10.5～5.5 Ma（SQ1、SQ2）为红河海底扇发育阶段，以发育大型“三角洲—水下下切水道—海底扇”为特征；5.5～3.6 Ma（SQ3、SQ4）为限制性海底扇—中央峡谷发育阶段，以先发育限制性海底扇，后发育大型海底峡谷为特征；3.6～1.8 Ma（SQ5、SQ6）为红河沉积体系衰弱阶段，在研究区内以红河沉积体系主体不发育，海南岛陆坡发育为特征。红河沉积体系是青藏高原隆升的产物，研究红河沉积体系除有利于制定油气勘探方向外，还有助于青藏高原隆升历史恢复、红河袭夺等问题的研究。
- /
- 晚中新世&mdash /
- 上新世 /
- /
- 红河沉积体系 /
- /
- 地震反射特征 /
- /
- 高原隆升
Abstract: In the northwest of South China Sea, a huge far source Sedimentary System which is called Red River Sedimentary System has been discovered recently. The Red River depositional system refers to "a genetically related combination of a series of deltas, submarine canyon infillings, submarine fans and finegrained suspension deposits deriving from the terrestrial clastics of the Red River in Neocene". The main body of this depositional system comprises the Red River delta, the Red River submarine fan and the Central Canyon. In order to understand the identify standard and distributing in the plan view, a great deal of 2D seismic profiles has been used. The paper mainly focuses on the system which is developed during late Miocene to Pliocene. Base on the distributing in the plan view, the development history of the Red River Sedimentary system can be understood. The results show that deltas, channels, submarine canyon, channellevee complex and lobes can be identified in the Red River Sedimentary system based on the seismic reflection characteristics. According to the combination and spatial distribution features of the Red River sedimentary system, the development history of the system can be subdivided into three stages: SQ1SQ2, the formation period of Red River submarine fan, which is characterized by huge submarine fan; SQ3SQ4, the development period of the confined submarine fanCentral Canyon, which is characterized by a confined submarine fan developed before the central Canyon; and SQ5SQ6,
the weakening period of the Red River depositional system, which is characterized by Red River Sedimentary System fading out in the research area, instead of Hainan slope's growing. Red River Sedimentary System derives from QinghaiTibetan Plateau uplift. The research is not only beneficial for ascertaining Oil and gas prospecting, but also helpful for rebuilding uplift history of QinghaiTibetan Plateau, and answering the question whether Red River capture occurred or not.
- late MiocenePliocene /
- Red River sedimentary system /
- characterize of seismic /
- QinghaiTibetan Plateau uplift /

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[1]	贺华瑞, 栾锡武, 龚梁轩, 叶传红, 闫恒. 南昆嵩凹陷中新世以来三角洲地震响应与沉积充填演化 . 沉积学报, 2023, 41(5): 1568-1582. doi: 10.14027/j.issn.1000-0550.2022.024
[2]	沈迪, 郭进京, 于美娜, 宫恩麟, 常西玲, 常璐璐. 西秦岭北缘上新统木梯寺砾岩成因 . 沉积学报, 2023, 41(2): 409-424. doi: 10.14027/j.issn.1000-0550.2021.089
[3]	吴劲宣, 夏国清, 陈云, 徐为鹏, 伊海生. 西藏伦坡拉盆地渐新世——中新世之交黏土矿物特征及其古气候意义 . 沉积学报, 2022, 40(5): 1265-1279. doi: 10.14027/j.issn.1000-0550.2021.032
[4]	. 塔里木盆地西北缘库孜贡苏剖面晚白垩世—早中新世沉积物岩石磁学研究 . 沉积学报, 2012, 30(5): 919-927.
[5]	. 南海北部白云凹陷早中新世东部沉积体系研究 . 沉积学报, 2012, 30(3): 461-468.
[6]	徐强. 南海白云凹陷深水区渐新世—中新世断阶陆架坡折沉积过程响应 . 沉积学报, 2010, 28(5): 906-916.
[7]	颜照坤. 龙门山前陆盆地晚三叠世沉积通量与造山带的隆升和剥蚀 . 沉积学报, 2010, 28(1): 91-101.
[8]	伊海生. 西藏高原沱沱河盆地渐新世—中新世湖相碳酸盐岩稀土元素地球化学特征与正铕异常成因初探 . 沉积学报, 2008, 26(1): 1-10.
[9]	解三平, 孙柏年, 阎德飞, 丛培允, 肖良, 韦利杰. 滇西新近纪植物气孔、碳同位素组成与古环境分析 . 沉积学报, 2006, (6): 883-888.
[10]	解三平孙柏年阎德飞丛培允肖良韦利杰. 滇西新近纪植物气孔、碳同位素组成与古环境分析 . 沉积学报, 2006, 24(06): 883-888.
[11]	朱迎堂, 方小敏, 高军平, 伊海生, 王世锋, 张伟林. 青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析 . 沉积学报, 2006, (6): 775-782.
[12]	朱迎堂方小敏高军平伊海生王世锋张伟林. 青藏高原南部乌郁盆地渐新世—上新世地层沉积相分析 . 沉积学报, 2006, 24(06): 775-782.
[13]	刘志飞, 王成善, 金玮, 伊海生, 郑洪波, 赵西西, 李亚林. 青藏高原沱沱河盆地渐新—中新世沉积环境分析 . 沉积学报, 2005, 23(2): 210-217.
[14]	李忠, 王清晨, 王道轩, 林伟. 晚新生代天山隆升与库车坳陷构造转换的沉积约束 . 沉积学报, 2003, 21(1): 38-45.
[15]	郑洪波, Kutherine Butcher, Chris Powell. 新疆叶城晚新生代山前盆地演化与青藏高原北缘的隆升——Ⅱ沉积相与沉积盆地演化 . 沉积学报, 2003, 21(1): 46-51.
[16]	宋春晖, 孙淑荣, 方小敏, 孙东. 酒西盆地晚新生代沉积物重矿物分析与高原北部隆升 . 沉积学报, 2002, 20(4): 552-559.
[17]	宋春晖, 方小敏, 高军平, 孙东, 范马洁. 青藏高原东北部贵德盆地新生代沉积演化与构造隆升 . 沉积学报, 2001, 19(4): 493-500.
[18]	苗晓东, 孙有斌, 鹿化煜. 黄土高原晚上新世红粘土粒度的空间变化 . 沉积学报, 2001, 19(2): 182-185.
[19]	王国芝, 王成善, 曾允孚, 赵锡奎. 滇西高原的隆升与莺歌海盆地的沉积响应 . 沉积学报, 2000, 18(2): 234-240.
[20]	邵龙义, 张鹏飞, 陈代钊, 罗忠. 滇东黔西晚二叠世早期辫状河三角洲沉积体系及其聚煤特征 . 沉积学报, 1994, 12(4): 132-139.

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文章访问数: 2101
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PDF下载量: 777
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南海晚中新世—上新世红河沉积体系研究

刊出日期: 2013-02-10

中图分类号: P512.2

关键词:

上新世 /

摘要: 红河沉积体系为南海西北部近期新发现的大型远源沉积体系，其主要发育于南海莺歌海盆地和琼东南盆地。重点利用大量二维地震剖面资料，根据地震反射特征对晚中新世—上新世红河沉积体系的识别特征以及平面展布进行了研究，以此为基础划分了红河沉积体系在晚中新世—上新世演化阶段。研究结果表明：通过地震反射特征的分析，可以识别出三角洲、水下下切水道、海底峡谷、水道堤岸复合体以及海底扇朵体等沉积；依据红河沉积体系的平面组合和展布特征，可将晚中新世至上新世的红河沉积体系演化划分为3个阶段：10.5～5.5 Ma（SQ1、SQ2）为红河海底扇发育阶段，以发育大型“三角洲—水下下切水道—海底扇”为特征；5.5～3.6 Ma（SQ3、SQ4）为限制性海底扇—中央峡谷发育阶段，以先发育限制性海底扇，后发育大型海底峡谷为特征；3.6～1.8 Ma（SQ5、SQ6）为红河沉积体系衰弱阶段，在研究区内以红河沉积体系主体不发育，海南岛陆坡发育为特征。红河沉积体系是青藏高原隆升的产物，研究红河沉积体系除有利于制定油气勘探方向外，还有助于青藏高原隆升历史恢复、红河袭夺等问题的研究。

Research on Red River Sedimentary System of late MioceneEarly Pliocene, South China Sea

Publish Date: 2013-02-10

Keywords:

Abstract: In the northwest of South China Sea, a huge far source Sedimentary System which is called Red River Sedimentary System has been discovered recently. The Red River depositional system refers to "a genetically related combination of a series of deltas, submarine canyon infillings, submarine fans and finegrained suspension deposits deriving from the terrestrial clastics of the Red River in Neocene". The main body of this depositional system comprises the Red River delta, the Red River submarine fan and the Central Canyon. In order to understand the identify standard and distributing in the plan view, a great deal of 2D seismic profiles has been used. The paper mainly focuses on the system which is developed during late Miocene to Pliocene. Base on the distributing in the plan view, the development history of the Red River Sedimentary system can be understood. The results show that deltas, channels, submarine canyon, channellevee complex and lobes can be identified in the Red River Sedimentary system based on the seismic reflection characteristics. According to the combination and spatial distribution features of the Red River sedimentary system, the development history of the system can be subdivided into three stages: SQ1SQ2, the formation period of Red River submarine fan, which is characterized by huge submarine fan; SQ3SQ4, the development period of the confined submarine fanCentral Canyon, which is characterized by a confined submarine fan developed before the central Canyon; and SQ5SQ6,
the weakening period of the Red River depositional system, which is characterized by Red River Sedimentary System fading out in the research area, instead of Hainan slope's growing. Red River Sedimentary System derives from QinghaiTibetan Plateau uplift. The research is not only beneficial for ascertaining Oil and gas prospecting, but also helpful for rebuilding uplift history of QinghaiTibetan Plateau, and answering the question whether Red River capture occurred or not.

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南海晚中新世—上新世红河沉积体系研究

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Research on Red River Sedimentary System of late MioceneEarly Pliocene, South China Sea

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南海晚中新世—上新世红河沉积体系研究

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Research on Red River Sedimentary System of late MioceneEarly Pliocene, South China Sea

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南海晚中新世—上新世红河沉积体系研究

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Research on Red River Sedimentary System of late MioceneEarly Pliocene, South China Sea

计量

出版历程

目录

南海晚中新世—上新世红河沉积体系研究

English Abstract

Research on Red River Sedimentary System of late MioceneEarly Pliocene, South China Sea

全文HTML

目录

友情链接

期刊在线

联系我们