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A kinematic and geochronological analysis of the 10-20-km-wide northeast-trending Dongxiang-Shexian ductile shear zone, that trends along a length of 250 km in the eastern part of the Jiangnan belt indicates a sinistral strike-slip ductile shear that was formed during the Neo-Proterozoic. The zone experienced polyphase deformation related to tectonic collision between the Huaiyu and the Jiuling terranes...
In southeastern China, the Wugongshan massif consists of metamorphic rocks and granites generally considered as basement rocks formed during an early Paleozoic orogeny. Our structural and radiometric reappraisal of this massif shows that it results from a Mesozoic doming. In the metamorphic rocks, the foliation defines an E-W elliptical shape and bears a N-S stretching lineation. The axial...
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