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In this case, the partial melting of rocks of the Shuangqiaoshan Group can produce S-, I- and transitional type granitoids.

After strong differentiation it formed tungsten-bearing granitoids characterized by enrichment of high alkali, silicon and volatile components.

The granitoid-related W ore systems in JNB resulted from the remelting of the Proterozoic crust.

The Lamo Zn–Cu deposit is a typical skarn deposit in the district and occurs at the contact zone between the Upper Devonian limestone and the granite.

Two granitoids are characterized by a negative slope with significant light REE/heavy REE fractionation [(La/Yb) Considering the two groups of parallel Late Mesozoic ore belts, namely the Jiangnan porphyry-skarn tungsten belt (JNB) in the south and the Middle-Lower Yangtze River porphyry-skarn Cu-Au-Mo-Fe ore belt (YRB) in the north, the Nanling granite-related W-Sn ore belt (NLB) in the south, the neighboring Qin-Hang porphyry-skarn Cu-Mo-hydrothermal Pb-Zn-Ag ore belt (QHB) in the north, as well as the Southeastern Coast porphyry-skarn Cu-Mo-Au ore belt (SCB) recognized in South China in this paper, we propose that the latest Jurassic to earliest Cretaceous granitoids and associated ores were formed during a tearing of the subducting Izanagi slab.

This tearing of the subduction slab caused the upwelling of asthenosphere and the resulting mantle-crust interaction.

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If this is equal to '*t' then this function will return a table, otherwise it will return a string. ', the returned data will use the UTC timezone rather than the local timezone. Not all flags are available on all operating systems and the result of using an invalid flag is undefined. Most or all flags are available on OS X and Linux but considerably fewer are available on Windows. Note that the # flags also crashes the game on Windows.

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