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Two units of sedimentary carbonates in association with Neoproterozoic glaciations occur in the Lantian Formation of the Ediacaran system, equivalent to the Doushantuo Formation elsewhere in South China. Trace elements and strontium isotopes in the carbonates were analyzed by stepwise dissolutions with different strengths of acid. The results show that the carbonate component dissolved in 0.5 M acetic...
The geochemical and isotopic signature of Quaternary alluvial sediments filling a post-orogenic basin along the Tyrrhenian coasts of Italy (Cornia Plain, Tuscany) was investigated to unravel possible interactions with geothermal fluids from the Larderello geothermal field. Two cores located in the upper (UCP) and lower (LCP) sector of the plain were sampled to depths of up to 80 m. A third core in...
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