Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of east China: Partial melting of delaminated lower continental crust?
Chinese Academy of Sciences · Guangzhou Institute of Geochemistry · +3 more institutions
Abstract
Research Article| December 01, 2002 Origin of Mesozoic adakitic intrusive rocks in the Ningzhen area of east China: Partial melting of delaminated lower continental crust? Ji-Feng Xu; Ji-Feng Xu 1Guangzhou Institute of Geochemistry, Chinese Academy of Sciences, P.O. Box 1131, Guangzhou 510640, People's Republic of China Search for other works by this author on: GSW Google Scholar Ryuichi Shinjo; Ryuichi Shinjo 2Department of Physics and Earth Sciences, University of the Ryukyus, Nishihara, Okinawa 903-0213, Japan Search for other works by this author on: GSW Google Scholar Marc J. Defant; Marc J. Defant 3Department of Geology, University of South Florida, Tampa, Florida 33620, USA Search for other works by…
Citation impact
- FWCI
- 8.73
- Percentile
- 100%
- References
- 25
Authors
5Topics & keywords
- China
- Citation
- Icon
- Continental crust
- Partial melting
- Geology
- Crust
- Chinese academy of sciences