Lead isotope evolution across the Neoproterozoic boundary between craton and juvenile crust, Bayuda Desert, Sudan-Reference-Cited by-同舟云学术

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Lead isotope evolution across the Neoproterozoic boundary between craton and juvenile crust, Bayuda Desert, Sudan

Published:2017-11 Issue: Volume:135 Page:72-81
ISSN:1464-343X
Container-title:Journal of African Earth Sciences
language:en
Short-container-title:Journal of African Earth Sciences

Author:

Evuk David,Lucassen Friedrich^ORCID,Franz Gerhard

Funder

DAAD

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference58 articles.

1. Geochemical and geotectonic controls of the metallogenic evolution of selected ophiolite complexes from the Sudan;Abdel-Rahman;Berl. Geowiss Abh A,1993

2. The saharan Metacraton;Abdelsalam;J. Afr. Earth Sci.,2002

3. Sutures and shear zones in the arabian-nubian shield;Abdelsalam;J. Afr. Earth Sci.,1996

4. The Neoproterozoic Keraf suture in NE Sudan: sinistral transpression along the eastern margin of west Gondwana;Abdelsalam;J. Geol.,1998

5. Neoproterozoic deformation in the northeastern part of the Saharan Metacraton, northern Sudan;Abdelsalam;Precam Res.,2003

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. Trace element and Pb and Sr isotope investigation of tooth enamel from archaeological remains at El-Kurru, Sudan: Evaluating the role of groundwater-related diagenetic alteration;Applied Geochemistry;2021-09

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