Strontium and argon isotopic homogenization of pelitic sediments during low-grade regional metamorphism: The pan-African upper Damara sequence of Northern Namibia (South West Africa)-Reference-Cited by-同舟云学术

Strontium and argon isotopic homogenization of pelitic sediments during low-grade regional metamorphism: The pan-African upper Damara sequence of Northern Namibia (South West Africa)

Published:1979-01 Issue:1 Volume:43 Page:117-131
ISSN:0012-821X
Container-title:Earth and Planetary Science Letters
language:en
Short-container-title:Earth and Planetary Science Letters

Author:

Clauer N.,Kröner A.

Publisher

Elsevier BV

Subject

Space and Planetary Science,Earth and Planetary Sciences (miscellaneous),Geochemistry and Petrology,Geophysics

Reference36 articles.

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3. Pan African mobile belts as evidence for a transitional tectonic regime from intraplate orogeny to plate margin orogeny;Kröner,1978

4. The intracratonic branch of the Damara orogen in South West Africa;Martin;Precamb. Res.,1977

5. The Precambrian geology of South West Africa and Namaqualand;Martin,1965

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