Zircon U-Pb geochronology, major, trace elemental, and Sr-Nd-Pb isotopic geochemistry: constraints on the age and magmatic origin of Mesozoic mafic dykes in the Guangxi Zhuang Autonomous Region, South China

Author:

Liu Shen1,Feng Caixia1,Hou Chenhui1,Coulson Ian M.2ORCID

Affiliation:

1. State Key Laboratory of Continental Dynamics and Department of Geology, Northwest University, Xi’an, China

2. Department of Earth Sciences, University of Regina, Regina, SK, Canada

Publisher

Informa UK Limited

Reference125 articles.

1. Correction of common lead in U–Pb analyses that do not report 204Pb

2. Barry, T.L., and Kent, R.W., 1998, Cenozoic magmatism in Mongolia and the origin of central and east Asian basalts, in Flower, M., Chung, S., Lo, C., and Lee, T., eds., Mantle dynamics and plate interactions in East Asia: Washington DC, American Geophysical Union, vol. 27, p. 347–364.

3. SHRIMP zircon U-Pb dating of the intrusive rocks in the Dachang Tin-Polymetallic Ore Field, Guangxi and their geological significance;Cai M.H.;Geologicasl Review,2006

4. Cao, J.J., 2006, Geochemistry and lithosphere evolution of Cenozoic basic veins in coastal areas of Guangdong and Hainan Island: Institute of Geochemistry, Chinese Academy of Sciences. (in Chinese with English abstract).

5. Geochemistry and genesis of mafic dikes from the coastal areas of Guangdong Province, China;Cao J.J.;Acta Petrologica Sinica,2009

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