An early Palaeozoic double-subduction model for the North Qilian oceanic plate: evidence from zircon SHRIMP dating of granites-Reference-Cited by-同舟云学术

An early Palaeozoic double-subduction model for the North Qilian oceanic plate: evidence from zircon SHRIMP dating of granites

Published:2009-06-15 Issue:2 Volume:53 Page:157-181
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Wu Cailai¹,Gao Yuanhong¹,Frost B. Ronald²,Robinson Paul T.³,Wooden Joseph L.⁴,Wu Suoping¹,Chen Qilong¹,Lei Min¹

Affiliation:

1. a Institute of Geology, Chinese Academy of Geological Sciences , Beijing, 100037, P.R. China

2. b University of Wyoming , Laramie, WY, 82071, USA

3. c Department of Earth Sciences , Dalhousie University , Halifax, Nova Scotia, B3H 3J5, Canada

4. d Stanford University , Stanford, CA, 94305, USA

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206810902965346

Reference85 articles.

1. Bureau of Geology and Mineral Resources of Ningxia Province. 1990.Regional geology of Ningxia province, geological memoirs of ministry of geology and mineral resources of People's Republic of China, 51–76. Beijing: Geological Publishing House. (in Chinese)

2. Geochemical and isotopic composition and inherited zircon ages as evidence for lower crustal origin of two Variscan S-type granites in the NW Bohemian massif

3. Pb diffusion in zircon

4. Rocks from the Mantle Transition Zone: Majorite-Bearing Xenoliths from Malaita, Southwest Pacific

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