Incomplete mixing of isotopically variable melts in the lower oceanic crust and its implications on mantle heterogeneity: Evidence from oceanic cumulates from 14°45′N, Mid-Atlantic Ridge-Reference-Cited by-同舟云学术

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Incomplete mixing of isotopically variable melts in the lower oceanic crust and its implications on mantle heterogeneity: Evidence from oceanic cumulates from 14°45′N, Mid-Atlantic Ridge

Published:2024-03 Issue: Volume:648 Page:121940
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Wang Jixin,Li Bing,Zhang Fangyi,Liao Renqiang,Gu Xiaoyan,Li Congying,Sun Weidong

Funder

National Natural Science Foundation of China

Chinese Academy of Sciences

Tongji University

Natural Science Foundation of Shandong Province

State Key Laboratory of Marine Geology

Publisher

Elsevier BV

Reference84 articles.

1. Abundances of the elements: Meteoritic and solar;Anders;Geochim. Cosmochim. Acta,1989

2. The Logatchev Hydrothermal Field (MAR, 15°N): High-and Low- Temperature Alteration of Ultramafic Oceanic Crust-Geology, Geochemistry, Mineralogy;Augustin,2007

3. High-Mg and Low-Mg mantle eclogites from Koidu (West African Craton) linked by neoproterozoic ultramafic melt metasomatism of subducted Archaean Plateau-like oceanic crust;Aulbach;J. Petrol.,2019

4. Simultaneous determination of trace elements and lead isotopes in fused silicate rock powders using a boron nitride vessel and fsLA-(MC)-ICP-MS;Bao;J. Anal. At. Spectrom.,2016

5. Genesis of oceanic oxide gabbros and gabbronorites during reactive melt migration at transform walls (Doldrums Megatransform System; 7–8°N Mid-Atlantic Ridge);Basch;J. Petrol.,2022

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