Early Mesozoic southward subduction history of the Mongol–Okhotsk oceanic plate: Evidence from geochronology and geochemistry of Early Mesozoic intrusive rocks in the Erguna Massif, NE China

Author:

Tang Jie,Xu Wen-Liang,Wang Feng,Zhao Shuo,Wang Wei

Funder

National Key Basic Research Program of China

National Natural Science Foundation of China

Graduate Innovation Fund of Jilin University

Ministry of Land and Resources of the People's Republic of China

China University of Geosciences, Wuhan

Publisher

Elsevier BV

Subject

Geology

Reference132 articles.

1. Early–middle Archaean crustal evolution deduced from Lu–Hf and U–Pb isotopic studies of single zircon grains;Amelin;Geochimica et Cosmochimica Acta,2000

2. Correction of common lead in U–Pb analyses that do not report 204Pb;Anderson;Chemical Geology,2002

3. Rb–Sr whole rock isochron age of Daltyn-am Complex in Bayankhongor area, central Mongolia;Arakawa;Mongolian Geoscientist,1998

4. Genesis and evolution of mafic micro-granular enclaves through various types of interaction between coexisting felsic and mafic magmas;Barbarin;Transactions of the Royal Society of Edinburgh: Earth Sciences,1992

5. The Lu–Hf geochemistry of chondrites and the evolution of the mantle–crust system;Blichert-Toft;Earth Planetary Science Letters,1997

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