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白垩纪西珊瑚海 (澳大利亚东北岸外 )分裂时 ,形成了现今由碳酸盐台地披覆的大陆块体。生长在这些大陆块体之一的马里恩海底高原碳酸盐台地是研究成因、范围以及大陆边缘沉积对海平面变化影响的天然实验室。海平面是控制自然和大陆边缘沉积作用几何学的主要因素之一 ,然而 ,关
During the Cretaceous Western Coral Sea (off the northeast coast of Australia), continental blocks now covered by carbonate platforms were formed. The Marian Seabed Plateau carbonate platform, one of these continental blocks, is a natural laboratory to investigate the genesis, extent and impact of continental margin deposition on sea level changes. Sea level is one of the main factors controlling the sedimentation geometry of nature and continental margin. However,