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Ductile shear structure of the Guanging-Bobai fault belt in the SW part of the Qin-Hang belt, South China, has been investigated and interpreted in terms of radiometric dating data. A series of ductile shear zones occurs within the fault belt with deformation and metamorphic features indicative of formation under medium temperature and pressure conditions. The foliation such formed is steeply dipping...
The North China–South China collision during early Mesozoic time formed the Dabie–Sulu ultrahigh pressure (UHP) metamorphic belt in eastern China, the largest UHP metamorphic belt on Earth. However, no consensus exists about the dynamics of this continental collision. In order to get insights into this process, a series of four analogue models was performed. The experiments used layers of silicone...
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