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Posted by / 16-Jul-2020 13:42

In the cassiterite–sulfide ore, Cst I has clear oscillatory zonation and is dull luminescing.In the cassiterite–iron oxide ± sulfide ore, Cst I core is dull luminescing (blue in OM−CL) and surrounded by a bright luminescing Cst I rim (yellow in OM−CL).

And the pace of Arctic sea ice loss experienced in the past few decades has not been seen in at least the past 1,450 years.Cst I is replaced by Cst II veinlets with bright luminescing (yellow in OM−CL).The SEM−CL luminescing intensity of cassiterite is mainly controlled by Ti content.As Walter Meier of NASA’s Goddard Space Flight Center has put it, “The climate system’s interconnected.So what happens in the Arctic doesn’t stay in the Arctic.” That’s true for a number of reasons, including this: Research suggests that Arctic warming is affecting day-to-day weather much farther south — not always pleasantly.

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Elevated W and Fe but low Nb, Ta, Zr and Hf concentrations of cassiterites from the Gaosong deposit, are distinctly different from those of cassiterites in VMS/SEDEX tin deposits, but similar to those from granite-related tin deposits.

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