Article ID Journal Published Year Pages File Type
8868685 Palaeogeography, Palaeoclimatology, Palaeoecology 2017 60 Pages PDF
Abstract
Our findings also demonstrate that carbonate evolution in the Xisha Islands was shaped by relative sea-level changes, implying that sea level fluctuations in the SCS were controlled by global eustatic factors in addition to regional tectonic subsidence.
Keywords
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Preview
Sea-level changes and carbonate platform evolution of the Xisha Islands (South China Sea) since the Early Miocene
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