Sm-Nd and SHRIMP U-Pb zircon geochronology of high-pressure granulites in the Sanggan area, North China Craton: Timing of Paleoproterozoic continental collision

High-pressure (HP) mafic granulites are widely distributed as sheet-like and lenticular bodies within highly deformed tonalitic gneisses in the Sanggan area, North China Craton. They have clockwise isothermal decompression and isobaric cooling P-T paths implying continental collision tectonics. Whole-rock analyses of 15 samples define a Sm-Nd isochron yielding an age of 2547 ± 87 Ma with ε Nd(t)=2.7. Corresponding Nd depleted mantle model ages show a similar range and are interpreted as the age of the magmatic protolith to the high-pressure granulites. A combined Sm-Nd mineral+whole-rock isochron from one of these samples yields an age of 1813 ± 23 Ma, taken to represent the metamorphic age at an early stage on the cooling path. SHRIMP U-Pb zircon analyses of three HP mafic granulite samples give uniform weighted mean 207Pb/ 206Pb ages of 1817 ± 12, 1817 ± 12 and 1819 ± 16 Ma. These ages are interpreted to date metamorphism of the HP granulites and, with the Sm-Nd mineral + whole-rock result, strongly suggest that the time of continental collision was at ca.1.82 Ga. An additional sample records two age populations; one at 1803 ± 9 Ma and an older one at 1872 ± 16 Ma. The latter may indicate the timing of either an earlier metamorphic event or possibly the earliest stage of a single prolonged metamorphic episode that peaked at ∼1.82 Ga. These results confirm the Paleoproterozoic age for assembly of the North China Craton. © 2004 Elsevier Ltd. All rights reserved.link_to_subscribed_fulltex