试论南中国海盆地新生代板块构造及盆地动力学
On the Cenozoic tectonics and basin dynamics of the South China Sea
查看参考文献50篇
|
文摘
|
南海地处欧亚、印度一澳大利亚和菲律宾海板块的交互带,是西太平洋地区面积最大的边缘海之一,其成因机制和演化过程对探讨特提斯构造域和太平洋构造域相互作用及油气勘探等问题具有重要意义,虽备受关注但仍存争议。综合目前该区及外围已有的大地构造等方面的资料,本文从探讨南海外围的构造格架及中.新生代演化过程人手,分析了南海及外围板块构造早第三纪、晚第三纪和第四纪期间的板块演化序列及相应的沉积过程,以期对南海盆地的成盆动力学过程提供约束和启示。此外,还进一步概括了南海北、西和南部大陆边缘性质及其相应的盆地变形特征。 |
|
其他语种文摘
|
The South China Sea is located at the conjunction of the Eurasia,India-Australia and Philippine plates,and is the largest marginal sea in the western Pacific area.The mechanism and tectonic evolution of the South China Sea,which will shed great insights into the interaction between the Tethyan and Pacific tectonic realms and the assessment of the oil and gas potential,are still open to intense debate.Based on the existing srtructural and tectonic information of the South China Sea and its adjacent areas,we tentatively dicussed the tectonic evolution of regions around the South China Sea during the Early and Late Tertiary through the Quaternary.The origin and evolution of the South China Sea were largely restrained by the India-Asian collision and the rotation of continental blocks along the Red River fault during the Cenozoic.South China Sea developed under the rift-strike tectonic background with the levorotaroty of Red River fault transfer to dextrorotation accompanying the convergency of India-Asian plate.Cenozoic subduction of the Pacific plate beneath to the Erasian continent result the disintegration of accumulated East Asian terranes during the Mesozoic.Continous continental subduction of South China Sea casused the underplate of basalt and uplifted the continental curst,and initite the broad magmatisms during the Mid-Miocene,and formed the miniature of modern South China Sea's deformation and tectonic framework.Generally,the South China Sea experienced initial marginal rifting in early and Middle of the Early Tertiary,strike-slipping pull-apart and oceanic extension during the later Early Tertiary to the early Late Tertiary,and Neotectonism from later Late Titary to Quaternary,respectively.Meanwhile,sedimentary sequences correspongding to the relevant tectonic setting.Cenozoic basins within the South China Sea have undergone different formation times,continental marginal deformation and basin characteristics because of the multiple plate tectonic dynamics around it.The northern South China Sea is a typical extensional continental margin result from the extension of oceanic crust,while its southeast is a compressional margin and its west is a transfer extensional continental margin. |
|
来源
|
地质科学
,2011,46(3):638-652 【核心库】
|
|
关键词
|
走滑一拉分作用
;
伸展盆地
;
构造体制
;
南海
|
|
地址
|
1.
中海油研究总院, 北京, 100027
2.
南京大学地球科学与工程学院, 南京, 210093
3.
南京大学, 海岸与海岛开发教育部重点实验室, 南京, 210093
|
|
语种
|
中文 |
|
文献类型
|
研究性论文 |
|
ISSN
|
0563-5020 |
|
学科
|
地质学 |
|
基金
|
国家973计划
;
国家重大科技专项
|
|
文献收藏号
|
CSCD:4276643
|
参考文献 共
50
共3页
|
|
1.
广西壮族自治区地质矿产局.
广西壮族自治区区域地质志,1985:1-853
|
被引
96
次
|
|
|
|
|
2.
郭令智. 西太平洋中／新生代活动大陆边缘和岛弧构造的形成及演化.
地质学报,1983,57(1):11-21
|
被引
156
次
|
|
|
|
|
3.
郭令智. 莺歌海盆地周边区域构造演化.
高校地质学报,2001,7(1):1-12
|
被引
73
次
|
|
|
|
|
4.
李平鲁. 珠江口盆地构造结构及演化.
中国海上油气(地质),1989,3(1):11-18
|
被引
15
次
|
|
|
|
|
5.
李思田. 关于南海及其边缘盆地形成的地球动力学背景的讨论.
南海北部大陆边缘盆地油气分析与油气聚集,1998:1-122
|
被引
1
次
|
|
|
|
|
6.
孙珍. 南海的发育机制研究:相似模拟证据.
中国科学(D辑),2006,36(9):797-810
|
被引
35
次
|
|
|
|
|
7.
Sun Zhen. Research on the dynamics of the South China Sea opening:Evidence from analogue modeling.
Science China(Series D),2006,49(10):1053-1069
|
被引
29
次
|
|
|
|
|
8.
吴世敏. 南海南北共轭边缘伸展模型探.
高校地质学报,2005,11(1):105-110
|
被引
13
次
|
|
|
|
|
9.
姚伯初. 南海北部陆缘的地壳结构及构造意义.
海洋地质与第四纪地质,1998,18(2):1-16
|
被引
44
次
|
|
|
|
|
10.
袁玉松. 南海北部深水区盆地特征及其动力学背景.
海洋科学,2008,32(12):102-110
|
被引
20
次
|
|
|
|
|
11.
张连生. 从红河剪切带走滑运动看东亚大陆新生代构造.
地质科学,1996,31(4):327-340
|
被引
67
次
|
|
|
|
|
12.
张功成. "源热共控论":来自南海海域油气田"外油内气"环带有序分布的新认识.
沉积学报,2010,28(5):987-1005
|
被引
59
次
|
|
|
|
|
13.
张功成. 南海北部陆坡深水区构造演化及其特征.
石油学报,2010,31(4):528-533
|
被引
89
次
|
|
|
|
|
14.
Allen C R. Red River and associated faults,Yunnan Province,China:Quaternary geology,slio rates,and seismic hazard.
Geological Society of America Bulletin,1984,95(6):686-700
|
被引
134
次
|
|
|
|
|
15.
Ben-Avraham Z. The evolution of the China Basin and the mesozoic paleogeography of Borneo.
Earth and Planetary Science Letters,1973,18(2):365-376
|
被引
49
次
|
|
|
|
|
16.
Briais A. Updated interpretation of magnetic anomalies and seafloor spreading stages in the South China Sea-Implications for the Tertiary tectonics of southeast-Asia.
Journal of Geophysical Research.B,1993,98(4):6299-6328
|
被引
487
次
|
|
|
|
|
17.
Cai J X. A new model for the Indochina and south China collision during the Late Permian to the Middle Triassic.
Tectonophysics,2009,469(1/4):35-43
|
被引
86
次
|
|
|
|
|
18.
Chen J F. Magmatism along the southeast margin of the Yangtze block:Precambrian collision of the Yangtze and Cathysia block of China.
Geology,1991,19(8):815-818
|
被引
110
次
|
|
|
|
|
19.
Chung S L. Intraplate extension prior to continental extrusion along the Ailao Shan Red River shear zone.
Geology,1997,25(4):311-314
|
被引
145
次
|
|
|
|
|
20.
Flower M F J. Mantle extrusion:A model for dispersed volcanism and DUPAL-like asthenosphere in east Asia and the western Pacifi.
Mantle Dynamics and Plate Interactions in East Asia,1998:67-88
|
被引
9
次
|
|
|
|
|
了解气象卫星更多信息，请访问