Termination time of peak decratonization in North China: Geochemical evidence from mafic igneous rocks-Reference-Cited by-同舟云学术

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Termination time of peak decratonization in North China: Geochemical evidence from mafic igneous rocks

Published:2016-01 Issue: Volume:240-243 Page:327-336
ISSN:0024-4937
Container-title:Lithos
language:en
Short-container-title:Lithos

Author:

Dai Li-Qun,Zheng Yong-Fei,Zhao Zi-Fu

Funder

Chinese Ministry of Science and Technology

National Natural Science Foundation of China

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference62 articles.

1. Evolution of the lithospheric mantle beneath the southeastern North China Craton: constraints from mafic dikes in the Jiaobei terrain;Cai;Gondwana Research,2013

2. Physical, chemical and chronological characteristics of continental mantle;Carlson;Reviews of Geophysics,2005

3. Sources of Anfengshan basalts: subducted lower crust in the Sulu UHP belt, China;Chen;Earth and Planetary Science Letters,2009

4. Trace element and isotope characteristics of Cenozoic basalts around the Tanlu Fault with implications for the east plate boundary between North and South China;Chung;Journal of Geology,1999

5. Zircon Hf–O isotope evidence for crust-mantle interaction during continental deep subduction;Dai;Earth and Planetary Science Letters,2011

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