A peridotite source for strongly alkalic ultrabasic HIMU lavas of the Oslo Rift, Norway-Reference-Cited by-同舟云学术

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A peridotite source for strongly alkalic ultrabasic HIMU lavas of the Oslo Rift, Norway

Published:2023-04 Issue: Volume:622 Page:121377
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Hyung Eugenia,Sedaghatpour Fatemeh,Larsen Bjørn T.,Neumann Else-Ragnhild,Eriksen Zachary T.,Petaev Michail I.,Jacobsen Stein B.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference144 articles.

1. Trace element partitioning between mica-and amphibole-bearing garnet lherzolite and hydrous basanitic melt: 1. Experimental results and the investigation of controls on partitioning behaviour;Adam;Contrib. Mineral. Petrol.,2006

2. Isotopic and chemical effects produced in a continuously differentiating convecting Earth mantle;Allegre;Phil. Trans. R. Soc. Lond. A,1980

3. An unusual mantle source region for nephelinites from the Oslo Rift, Norway;Anthony;Geochim. Cosmochim. Acta,1989

4. The Pb isotopic evolution of the Earth: inferences from river water suspended loads;Asmerom;Earth Planet. Sci. Lett.,1993

5. A comparison of tomographic and geodynamic mantle models;Becker;Geochem. Geophys. Geosyst.,2002

Cited by 1 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. The survival of tracers of primordial mantle heterogeneity investigated through 142Nd/144Nd and 3He/4He isotope decoupling in the Gorgona Island lavas;Earth and Planetary Science Letters;2023-11

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