We conduct zircon double dating (U-Pb and FT) for granitic gneiss bodies from the Chinmen area (central PDMB) and dioritic plutons in the ZIC (southern SCMB) in two sides of the Changle-Nanao fault. Results reveal a very fast cooling of the ZIC plutons after magmas emplaced at ~100 Ma which matches the field observations that they were very shallow intrusives. Relatively, the Chinmen area would be a geodynamically active terrain during Early Cretaceous in response to the deep emplacement of[…]

A thawt, an if a war alive, That zummet war tha matter.

You see that? The moths haven't got this, then. - You kept the old Sam Browne all these years? - Certainly. - And kept it polished. Might come in useful.

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