15 results on '"Yao, Jinlong"'
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2. Tectono-metamorphic evolution of paragneiss in the Chengde metamorphic Complex, northern Paleoproterozoic Trans-North China Orogen
3. Late Neoarchean plume-induced crust-mantle interaction and crustal reworking: Evidence from the Jianping Complex, North China Craton
4. Paleogeographic affinity of the Alxa Block across the Archean–Proterozoic: Insights from metamorphosed Archean basement
5. Phase equilibria modelling and zircon U-Pb geochronology of Paleoproterozoic mafic granulites from the Chengde Complex, North China Craton
6. Phase equilibria modelling and zircon U-Pb ages of the Paleoproterozoic high-pressure mafic granulites in the Jianping Complex and tectonic implications
7. Zircons from the Tarim basement provide insights into its positions in Columbia and Rodinia supercontinents
8. Tectonic evolution of the eastern Jiangnan region, South China: New findings and implications on the assembly of the Rodinia supercontinent
9. Constraining timing and tectonic implications of Neoproterozoic metamorphic event in the Cathaysia Block, South China
10. Delineating and characterizing the boundary of the Cathaysia Block and the Jiangnan orogenic belt in South China
11. The Precambrian tectonic evolution of the western Jiangnan Orogen and western Cathaysia Block: Evidence from detrital zircon age spectra and geochemistry of clastic rocks
12. Neoproterozoic arc-related andesite and orogeny-related unconformity in the eastern Jiangnan orogenic belt: Constraints on the assembly of the Yangtze and Cathaysia blocks in South China
13. Neoproterozoic arc-trench system and breakup of the South China Craton: Constraints from N-MORB type and arc-related mafic rocks, and anorogenic granite in the Jiangnan orogenic belt
14. Neoproterozoic arc-related mafic–ultramafic rocks and syn-collision granite from the western segment of the Jiangnan Orogen, South China: Constraints on the Neoproterozoic assembly of the Yangtze and Cathaysia Blocks
15. Precambrian crustal evolution of the South China Block and its relation to supercontinent history: Constraints from U–Pb ages, Lu–Hf isotopes and REE geochemistry of zircons from sandstones and granodiorite
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