Article ID Journal Published Year Pages File Type
4700556 Chemical Geology 2009 10 Pages PDF
Abstract
The 87Srex flux forcing changes in seawater Sr isotopic composition is 1.13 × 106 mol a− 1 for the HTJR at Yibin, being far lower than those in the Ganges and Brahmaputra and merely accounting for 1.36% of the total carried by the global rivers. Therefore, impact of the HTJR on steady increase of seawater 87Sr/86Sr ratio since 40 Ma may be very small.
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Physical Sciences and Engineering Earth and Planetary Sciences Geochemistry and Petrology
Preview
Sr fluxes and isotopic compositions in the headwaters of the Yangtze River, Tongtian River and Jinsha River originating from the Qinghai-Tibet Plateau
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