Open-system 182W142Nd isotope evolution of the Earth-Reference-Cited by-同舟云学术

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Open-system 182W142Nd isotope evolution of the Earth

Published:2022-11 Issue: Volume:611 Page:121104
ISSN:0009-2541
Container-title:Chemical Geology
language:en
Short-container-title:Chemical Geology

Author:

Kumari Seema,Stracke Andreas,Paul Debajyoti

Funder

Science and Engineering Research Board

Alexander von Humboldt-Stiftung

Deutscher Akademischer Austauschdienst

Deutsche Forschungsgemeinschaft

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference108 articles.

1. Chemical geodynamics;Allègre;Tectonophysics,1982

2. Chemical structure and evolution of the mantle and continents determined by inversion of Nd and Sr isotopic data, I. Theoretical methods; II. Numerical experiments and discussion;Allègre;Earth Planet. Sci. Lett.,1983

3. Lack of late-accreted material as the origin of 182W excesses in the Archean mantle: evidence from the Pilbara Craton, Western Australia;Archer;Earth Planet. Sci. Lett.,2019

4. Tungsten geochemistry and implications for understanding the Earth’s interior;Arevalo;Earth Planet. Sci. Lett.,2008

5. Simplified mantle architecture and distribution of radiogenic power. Geochemistry;Arevalo;Geophys. Geosystems,2013

Cited by 2 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 geochemical concept of a “Primitive Mantle”;Reference Module in Earth Systems and Environmental Sciences;2024

2. Hafnium-tungsten evolution with pebble accretion during Earth formation;Earth and Planetary Science Letters;2023-11

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