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- W2742400259 abstract "The tectonic framework and crustal evolution of South China have been a longstanding hot debate in the geological community of China. A variety of tectonic models have been proposed, in which South China has been described geologically as the well-known cathaysia landmass, the Caledonia geosyncline, an arc-trench-basin system and the collision tectonics. However, none of the above tectonic models has been well acknowledged as a successful and dominant theory in delineating the geological evolution of South China. One of the major controversies in this field is related to the origin of granitoids in the region. This chapter presents a case study on a new insight into the origin of granitoids in South China. The neodymium (Nd) isotope approach, both initial ratio and model age, has been employed to constrain the source characteristics of both igneous and sedimentary systems in two case studies in South China, which would provide timing and source constraints on the granitoids in South China Block and the source province of sedimentary rocks in Yangtze Block, which is compatible and supplementary to the study of tectonic facies proposed by Ken Hsü in the same region." @default.
- W2742400259 created "2017-08-17" @default.
- W2742400259 creator A5052358933 @default.
- W2742400259 date "2001-01-01" @default.
- W2742400259 modified "2023-09-24" @default.
- W2742400259 title "Nd Isotopes vs. Ken Hsü's Tectonic Facies" @default.
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- W2742400259 doi "https://doi.org/10.1016/b978-044450560-6/50016-3" @default.
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