Source nature and magma evolution of I-type granites from the North Qinling orogen, China, revealed by zircon morphology and grain-scale variations in Hf O isotope composition

Author:

Qin Zheng-wei,Wu Yuan-bao,Siebel Wolfgang,Wang Hao,Fu Jian-ming,Lu You-yue,Shan Liang,Yu Yu-shuai

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference75 articles.

1. A cryptic record of magma mixing in diorites revealed by high–precision SIMS oxygen isotope analysis of zircons;Appleby;Earth Planet. Sci. Lett.,2008

2. Aluminium saturation in I– and S–type granites and the characterization of fractionated haplogranites;Chappell;Lithos,1999

3. Two contrasting granite types;Chappell;Pac. Geol.,1974

4. Wyborn D. The importance of residual source material (restite) in granite petrogenesis;Chappell;J. Petrol.,1987

5. I– and S–type granites in the Lachlan Fold Belt;Chappell;Geol. Soc. Am. Spec. Pap.,1992

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