The Nama foreland basin: sedimentation, major unconformity bounded sequences and multisided active margin advance-Reference-Cited by-同舟云学术

The Nama foreland basin: sedimentation, major unconformity bounded sequences and multisided active margin advance

Published:1993-11 Issue:3-4 Volume:63 Page:247-272
ISSN:0301-9268
Container-title:Precambrian Research
language:en
Short-container-title:Precambrian Research

Author:

Gresse P.G.,Germs G.J.B.

Publisher

Elsevier BV

Subject

Geochemistry and Petrology,Geology

Reference44 articles.

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2. KAr age determinations of the northern Damara branch and their implications for the structural and metamorphic evolution of the Damara Orogen, South West Africa/Namibia;Ahrendt;Spec. Publ. Geol. Soc. S. Afr.,1983

3. RbSr and UPb geochronology of Late Precambrian-Early Palaeozoic igneous activity in the Richtersveld (South Africa) and South West Africa;Allsopp;Trans. Geol. Soc. S. Afr.,1979

4. Seismic/sequence stratigraphy: its role in petroleum exploration;Brown,1989

5. Trace fossils from the Nama Group (Precambrian-Cambrian) of Southwest Africa/Namibia;Crimes;J. Paleontol.,1982

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