The final collision of the CAOB: Constraint from the zircon U–Pb
Por um escritor misterioso
Descrição
The Linxi Formation occupies an extensive area in the eastern Inner Mongolia in the Central Asian Orogenic Belt (CAOB). The Linxi Formation is compose…
![The final collision of the CAOB: Constraint from the zircon U–Pb](https://media.springernature.com/lw685/springer-static/image/art%3A10.1007%2Fs12517-020-05658-3/MediaObjects/12517_2020_5658_Fig1_HTML.png)
Petrogenesis and tectonic setting of the Chaheilingashun pluton
![The final collision of the CAOB: Constraint from the zircon U–Pb](https://www.frontiersin.org/files/Articles/831677/feart-09-831677-HTML/image_m/feart-09-831677-g005.jpg)
Frontiers Early Permian Syn-Subduction Extension in the South
![The final collision of the CAOB: Constraint from the zircon U–Pb](https://media.springernature.com/m685/springer-static/image/art%3A10.1038%2Fsrep25751/MediaObjects/41598_2016_Article_BFsrep25751_Fig1_HTML.jpg)
Linking magmatism with collision in an accretionary orogen
![The final collision of the CAOB: Constraint from the zircon U–Pb](https://www.lyellcollection.org/cms/10.1144/jgs2017-079/asset/a1a91c87-3032-413e-a055-06b706070846/assets/images/large/jgs2017-079.01.jpg)
Geochemistry and zircon U–Pb–Hf isotopic data for Permo
![The final collision of the CAOB: Constraint from the zircon U–Pb](https://www.researchgate.net/publication/337582281/figure/fig6/AS:836924466008064@1576549750676/Distribution-of-zircon-TDM2-Hf-ages-blue-bars-and-U-Pb-ages-yellow-bars-from-the.png)
Distribution of zircon TDM2 (Hf) ages (blue bars) and U-Pb ages
![The final collision of the CAOB: Constraint from the zircon U–Pb](https://www.mdpi.com/minerals/minerals-13-00467/article_deploy/html/images/minerals-13-00467-g001.png)
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Sedimentary response to the non-synchronous closure of Paleo
![The final collision of the CAOB: Constraint from the zircon U–Pb](https://www.mindat.org/imagecache/05/9c/08345160016159070749474.jpg)
Zircon: Mineral information, data and localities.
![The final collision of the CAOB: Constraint from the zircon U–Pb](https://www.lyellcollection.org/cms/10.1144/SP516-2020-201/asset/91c74997-dab0-493e-8752-23148e1e49c5/assets/images/large/sp2020-201f08.jpg)
Thermochronological constraints on the exhumation history of the
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Zircon U–Pb and Hf isotopic study of Neoproterozoic granitic
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