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Qiuding Du
Researcher at Ministry of Land and Resources of the People's Republic of China
Publications - 7
Citations - 276
Qiuding Du is an academic researcher from Ministry of Land and Resources of the People's Republic of China. The author has contributed to research in topics: Zircon & Craton. The author has an hindex of 5, co-authored 5 publications receiving 227 citations.
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Paleoproterozoic I-type granites and their implications for the Yangtze block position in the Columbia supercontinent: Evidence from the Lengshui Complex, South China
TL;DR: In this paper, an integrated study of major and trace element data, SHRIMP and LA ICP-MS zircon U-Pb age data, and Hf isotopic data for the granites from the Lengshui Complex in the northern Yangtze Block is reported.
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The evolution of the Central Yangtze Block during early Neoarchean time: Evidence from geochronology and geochemistry
TL;DR: In this paper, the authors conducted a combined study of zircon U-Pb and whole-rock major and trace elements for seven quartz schist and two granite samples from the Yangpo Group in the Huji region, South China.
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Mature Archean continental crust in the Yangtze craton: Evidence from petrology, geochronology and geochemistry
TL;DR: In this paper, a petrological, geochronological and geochemical study of the Jinshan K-feldspar granite emplaced within the Yangpo Group, located in Huji Town, Zhongxiang City, Hubei Province, was conducted.
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2.85 Ga and 2.73 Ga A-type granites and 2.75 Ga trondhjemite from the Zhongxiang Terrain: Implications for early crustal evolution of the Yangtze Craton, South China
TL;DR: Zhang et al. as mentioned in this paper presented new zircon dating and detailed geochemical evidences to further reveal the magmatic events and their implication to related tectonic regimes.
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Geochronology and paleoenvironment of the pre-Sturtian glacial strata: Evidence from the Liantuo Formation in the Nanhua rift basin of the Yangtze Block, South China
TL;DR: In this paper, a detailed U-Pb zircon examination of geochronology and paleoenvironment of the Liantuo Formation in the Yangtze Block is presented.