Formation mechanism of the global Dupal isotope anomaly. (21st January 2016)

• Record Type: Journal Article
• Authors: Zhang, Zhen; Li, Sanzhong; Suo, Yanhui; Somerville, I. D.; Li, Xiyao
• Other Names: Li S. guestEditor.; Li G. guestEditor.; Liu X. guestEditor.; Somerville I. D. guestEditor.
• Is Part Of: Geological journal. Volume 51(2016)Supplement 1
• Page Start: 644
• Page End: 651
• Publication Date: 2016-01-21
• Subjects: Dupal anomaly -- mantle reservoir -- superplume -- hotspots; Geology -- Periodicals; 551
• DOI: 10.1002/gj.2751
• Languages: English
• ISSNs: 0072-1050

Abstract

Abstract: The Dupal anomaly has been a frequently discussed feature since it was first proposed three decades ago. We here limit the distribution of the Dupal anomaly based on more than 10 000 Sr–Nd–Pb isotopic composition analyses and classify the anomaly into three types, located in three different oceans and with different mechanisms of formation. The Dupal anomaly in the East Asian Continental Margin subduction zone is related to enriched mantle II, which may originate from the recycling of the subducting plate or continental mantle. The high μ and enriched mantle I are the reason for the Dupal anomaly in the Pacific Ocean, which is related to the superplume. However, the source of the Dupal anomaly in the Indian Ocean and the Southern Atlantic Ocean is a mixture of enriched mantle I and enriched mantle II, and they come from the African superplume and the recycling of subcontinental mantle or continental crust of Gondwana. In consideration of all the above factors, we suggest that the superplume from the core–mantle boundary, the recycling subducting plate and continental mantle are the main characteristics of the global Dupal anomaly. Copyright © 2016 John Wiley & Sons, Ltd.