Generation of I-type granitic rocks by melting of heterogeneous lower crust-Reference-Cited by-同舟云学术

Generation of I-type granitic rocks by melting of heterogeneous lower crust

Published:2018-09-11 Issue:10 Volume:46 Page:907-910
ISSN:0091-7613
Container-title:Geology
language:en
Short-container-title:

Author:

Hammerli Johannes¹,Kemp Anthony I.S.¹²,Shimura Toshiaki³,Vervoort Jeff D.⁴,Dunkley Daniel J.⁵⁶,

Affiliation:

1. Centre for Exploration Targeting, School of Earth Sciences, The University of Western Australia, Perth, Western Australia 6009, Australia

2. Geosciences, James Cook University, Townsville, Queensland 4811, Australia

3. Graduate School of Sciences and Technology for Innovation, Yamaguchi University, Yamaguchi 753-8512, Japan

4. School of the Environment, Washington State University, Pullman, Washington 99164, USA

5. Faculty of Earth Sciences, University of Silesia in Katowice, 41-200 Sosnowiec, Poland

6. National Institute of Polar Research, Tachikawa, Tokyo 190-0014, Japan

Publisher

Geological Society of America

Subject

Geology

Link

https://pubs.geoscienceworld.org/gsa/geology/article-pdf/46/10/907/4338704/907.pdf

Reference20 articles.

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2. Clarence River Supersuite: 250 Ma Cordilleran tonalitic I-type intrusions in eastern Australia;Bryant;Journal of Petrology,1997

3. Origin of infracrustal (I-type) granite magmas: Transactions of the Royal Society of Edinburgh;Chappell;Earth Sciences,1988

4. Lachlan Fold Belt granitoids: Products of three-component mixing: Transactions of The Royal Society of Edinburgh;Collins;Earth and Environmental Science,1996

5. The source of granitic gneisses and migmatites in the Antarctic Peninsula: A combined U-Pb SHRIMP and laser ablation Hf isotope study of complex zircons;Flowerdew;Contributions to Mineralogy and Petrology,2006

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