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IODP 359航次是为解决海平面、洋流和印度洋季风演化而设计的。7个建议的钻探站位位于马尔代夫,1个站位位于印度西部大陆边缘的Kerala-Konkan盆地(图1)。马尔代夫碳酸盐岩具有独特的和可以揭示新生代冰期印度洋的演变之谜。它为更好地了解印度-太平洋区域在全球演化中的作用提供了一个有着巨大潜力的关键地区。主要基于地震地层数据,为该碳酸盐浅滩演变模型已经研制成功,用来显示海平面变化和洋流格局的形成及结构。无论是海平面还是洋流驱动的碳酸盐沉积模式,印度季风被认为有着直接得
IODP 359 voyage is designed to address the evolution of sea level, ocean currents and the Indian Ocean monsoon. The seven proposed drilling stations are located in the Maldives with one station in the Kerala-Konkan basin on the western edge of India (Figure 1). The Maldivian Carbonates have unique and revealing mysteries about the evolution of the Indian Ocean in the Cenozoic ice age. It provides a key area of great potential for better understanding of the role of the Indian-Pacific region in global evolution. Based mainly on seismic formation data, a model for the evolution of this carbonate formate has been developed to show the formation and structure of sea level changes and ocean current patterns. Whether it is sea level or oceanic driven carbonate deposition patterns, the Indian monsoon is thought to have direct