Petrogenesis and tectonic implications of Devonian granitoids in the central Beishan orogen, NW China: geochemical and Sr-Nd-Hf isotopic constraints

Author:

Li Runwu12ORCID,Tong Ying1,Su Shangguo2

Affiliation:

1. Beijing SHRIMP Center, Institute of Geology, Chinese Academy of Geological Sciences, Beijing, China

2. School of Earth Sciences and Resources, China University of Geosciences, Beijing, China

Funder

the project of China Geological Survey

the National Key Research and Development Program of China

Publisher

Informa UK Limited

Subject

Geology

Reference147 articles.

1. Ao S.J. Xiao W.J. Han C.M. Li X.H. Qu J.F. Zhang J.E. Guo Q.Q. and Tian Z.H. 2012 Cambrian to early Silurian ophiolite and accretionary processes in the Beishan collage NW China: implications for the architecture of the Southern Altaids: Geological Magazine v. 149 no. 4 p. 606–625.

2. Genesis and tectonic setting of granite in the central region of the Beishan orogenic belt (Gansu section, China)

3. A review of the relationships between granitoid types;Barbarin B.;Their Origins and Their Geodynamic Environments: Lithos,1999

4. Zircon crystal morphology;Belousova E.A.;Trace Element Signatures and Hf Isotope Composition as a Tool for Petrogenetic Modelling: Examples from Eastern Australian Granitoids: Journal of Petrology,2005

5. A-type granites and related rocks: evolution of a concept;Bonin B.;Problems and Prospects: Lithos,2007

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