Deciphering crustal growth in the southernmost Arabian Shield through zircon U-Pb geochronology, whole rock chemistry and Nd isotopes-Reference-Cited by-同舟云学术

Deciphering crustal growth in the southernmost Arabian Shield through zircon U-Pb geochronology, whole rock chemistry and Nd isotopes

Published:2021-10-12 Issue: Volume: Page:1-19
ISSN:0020-6814
Container-title:International Geology Review
language:en
Short-container-title:International Geology Review

Author:

Pease Victoria¹,Yeshanew Fitsum G.¹²,Whitehouse Martin J.²^ORCID

Affiliation:

1. Department of Geological Sciences, Stockholm University, Stockholm, Sweden

2. Department of Geosciences, Swedish Museum of Natural History, Stockholm, Sweden

Funder

Vetenskapsrådet

Publisher

Informa UK Limited

Subject

Geology

Link

https://www.tandfonline.com/doi/pdf/10.1080/00206814.2021.1983735

Reference72 articles.

1. Agar, R.A., Stacey, J.S., and Whitehouse, M.J., 1992. Archaean to Late Proterozoic evolution of the southern Afif terrane: A geochronologic study. Saudi Arabian Directorate General of Mines and Geology, Open File Report OF-03-12.

2. Late Neoproterozoic rise and fall of the northern Arabian–Nubian shield: The role of lithospheric mantle delamination and subsequent thermal subsidence

3. Barker, F., 1979, Trondhjemite: Definition, environment and hypotheses of origin. Developments in petrology, Vol. 6. Amsterdam: Elsevier, p. 1–12.

4. Nd–Sr–Hf–O isotope provinciality in the northernmost Arabian–Nubian Shield: implications for crustal evolution

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