Mantle Melting and Intraplate Volcanism Due to Self‐Buoyant Hydrous Upwellings From the Stagnant Slab That Are Conveyed by Small‐Scale Convection-Reference-Cited by-同舟云学术

Mantle Melting and Intraplate Volcanism Due to Self‐Buoyant Hydrous Upwellings From the Stagnant Slab That Are Conveyed by Small‐Scale Convection

Author:

Long Xiaogang¹²^ORCID,Ballmer Maxim D.²³^ORCID,Córdoba Antonio M.‐C.²,Li Chun‐Feng⁴⁵^ORCID

Affiliation:

1. School of Ocean and Earth SciencesTongji University Shanghai China

2. Institute of GeophysicsETH Zurich Zurich Switzerland

3. Department of Earth SciencesUniversity College London London UK

4. Department of Marine SciencesZhejiang University Zhoushan China

5. Laboratory for Marine Mineral ResourcesQingdao National Laboratory for Marine Science and Technology Qingdao China

Funder

Schweizerischer Nationalfonds zur Förderung der Wissenschaftlichen Forschung

National Natural Science Foundation of China

China Scholarship Council

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Link

Reference230 articles.

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