| 南海西北部新生代沉积基底构造演化 |
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| 引用本文： | 刘海龄,杨恬,朱淑芬,张伯友,丘学林,施小斌.南海西北部新生代沉积基底构造演化[J].海洋学报,2004,26(3):54-67. |
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| 作者姓名： | 刘海龄 杨恬 朱淑芬 张伯友 丘学林 施小斌 |
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| 作者单位： | [1]中国科学院南海海洋研究所和广州地球化学研究所边缘海地质重点实验室，广东广州510301 [2]中海石油研究中心勘探研究院，河北高碑店074010 |
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| 基金项目： | 国家重点基础研究发展规划资助项目(G2000046702)，中国科学院知识创新资助项目(KZCX2-SW-117,KZCX2-209,KZCX2-102)，国家自然科学基金资助项目(49873008)，中国科学院王宽诚博士后工作奖励基金，边缘海地质和古环境开放实验室基金资助项目(BYH02A01). |
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| 摘 要： | 在综合分析地质、地球物理、地球化学、古生物学等多方面资料的基础上,将南海西北部海域控制新生代主要沉积盆地的基底划分为5个区:北部湾古生界断堑基底区、莺歌海古生界走滑拉分基底区、琼东古生界断陷基底区、西沙北古生界裂谷基底区、西沙南古生界走滑伸展基底区.通过区域地质分析,初步重建了该海域的大地构造演化历史.该海域新生代沉积基底在前新生代时期与其北面陆上云开地区和其南面的南沙地区同处于特提斯构造域中,经历过古特提斯和中特提斯的发育历程,晚古生代以来可初步分为5个阶段:(1)D-P1,古特提斯东段多岛洋体系发育阶段;(2)P2,中特提斯(古南海)开始出现、古特提斯开始消减阶段;(3)T-K1,古特提斯东段多地块缝合阶段;(4)K2-N11,现代南海形成、中特提斯(古南海)消亡时期;(6)N12以来南海扩张停止、澳大利亚板块向北俯冲挤压阶段.
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| 关 键 词： | 特提斯 新生代沉积基底 南海西北部 |
| 文章编号： | 0253-4193(2004)03-0054-14 |
| 收稿时间： | 2002/10/11 0:00:00 |
| 修稿时间： | 2003/1/20 0:00:00 |
Tectonic evolution of Cenozoic sedimentary basements in the northwestern South China Sea |
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| LIU Hai-ling,YANG Tian,ZHU Shu-fen,ZHANG Bo-you,QIU Xue-lin and SHI Xiao-bin.Tectonic evolution of Cenozoic sedimentary basements in the northwestern South China Sea[J].Acta Oceanologica Sinica (in Chinese),2004,26(3):54-67. |
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| Authors: | LIU Hai-ling YANG Tian ZHU Shu-fen ZHANG Bo-you QIU Xue-lin and SHI Xiao-bin |
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| Institution: | LIU Hai-ling~ |
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| Abstract: | On the basis of synthetical analyses of geology, geophysics, geochemistry, paleontology and paleomagnetism, the basements which control the major Cenozoic sedimentary basins in the northwestern South China Sea are divided into five districts: Beibu Gulf Paleozoic Erathem faulted basement district, Yinggehai Paleozoic Erathem strike-slip pull-apart basement district, Qiongdong Paleozoic Erathem rift-faulted basement district, northern Xisha Paleozoic Erathem rifted basement district and southern Xisha Paleozoic Erathem extended basement district. The evolution history of the basements is divided into five stages: (1)D-P_1,the stage of development of eastern Tethyan archipelago ocean; (2)P_2,the stage in which Meso-Tethys (Paleo-South China Sea) began to open and the Paleo-Tethys to subduct; (3)T-K_1,the stage in which the eastern Paleo-Tethyan blocks sutured; (4)K_2-N~1_1,the stage of the formation of modern South China Sea and the consumption of the Paleo-Tethys; (5)since N~2_1,the South China Sea stopped spreading and the Australia plate subducted and compressed northward. |
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| Keywords: | Tethys Cenozoic sedimentary basements northwestern South China Sea |
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