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印度洋大地构造背景及其构造演化——印度洋底大地构造图研究进展

李江海 张华添 李洪林

李江海, 张华添, 李洪林. 印度洋大地构造背景及其构造演化——印度洋底大地构造图研究进展[J]. 海洋学报, 2015, 37(7): 1-14.
引用本文: 李江海, 张华添, 李洪林. 印度洋大地构造背景及其构造演化——印度洋底大地构造图研究进展[J]. 海洋学报, 2015, 37(7): 1-14.
Li Jianghai, Zhang Huatian, Li Honglin. The tectonic setting and evolution of Indian Ocean ——Research progress of tectonic map of Indian Ocean[J]. Haiyang Xuebao, 2015, 37(7): 1-14.
Citation: Li Jianghai, Zhang Huatian, Li Honglin. The tectonic setting and evolution of Indian Ocean ——Research progress of tectonic map of Indian Ocean[J]. Haiyang Xuebao, 2015, 37(7): 1-14.

印度洋大地构造背景及其构造演化——印度洋底大地构造图研究进展

基金项目: 印度洋脊多金属硫化物成矿潜力与资源环境评价(DY125-12-R-03);西南印度洋脊合同区多金属硫化物资源评价(DY125-11-R-01).

The tectonic setting and evolution of Indian Ocean ——Research progress of tectonic map of Indian Ocean

  • 摘要: 印度洋底大地构造图(1:1 500万)基于最新地球物理数据,结合中国大洋调查航次积累的地貌、地质、地球物理和矿产资源资料编制,综合反映印度洋底及周缘地质、地貌、地球物理和资源分布等特征,将为理解和推进印度洋盆构造演化和资源分布研究提供理论支撑.本文介绍了该图编制的思路和方法、数据来源、图面内容和大地构造单元划分,认为印度洋盆具有多微陆块、多期扩张、多洋底高原、无震海岭和"入"字形洋中脊等特征.在前人研究基础上,将印度洋盆地构造演化归纳为3个阶段:(1)冈瓦纳大陆裂解与洋盆初始张开 (侏罗纪-白垩纪中期);(2)洋盆持续张开与扩张中心跃迁(白垩纪中期-古近纪初期);(3)印度板块与欧亚板块俯冲碰撞及非洲板块裂解(新生代).在扩张中心跃迁式的发育形式下,现今印度洋盆多微陆块、多期扩张中心和"入"字形的洋中脊基本构造格局在古近纪早期便已形成.
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