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2.09 Ga old eclogites in the Eburnian-Transamazonian orogen of southern Cameroon: Significance for Palaeoproterozoic plate tectonics

Denny Loose, +1 more
- 01 Jan 2018 - 
- Vol. 304, pp 1-11
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TLDR
The Nyong Complex of the Eburnian-Transamazonian orogen has been found to have a trace element pattern similar to those of mid-ocean ridge basalts, indicating that the precursor melts formed in a depleted mantle source as mentioned in this paper.
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This article is published in Precambrian Research.The article was published on 2018-01-01. It has received 92 citations till now. The article focuses on the topics: Craton & Eclogite.

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Toward an integrated model of geological evolution for NE Brazil-NW Africa: The Borborema Province and its connections to the Trans-Saharan (Benino-Nigerian and Tuareg shields) and Central African orogens

TL;DR: The Borborema Province of NE Brazil and the geological provinces of NW Africa (the Trans-Saharan Orogen consisted of the Tuareg and Benino-Nigerian shields and the Central African Orogen of Cameroon, Chad, and Central African Republic) are complex geological regions with superposition of distinct deformational, metamorphic and magmatic events and final structural configuration during the Brasiliano/Pan-African Orogeny.
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Eclogite facies metabasites from the Paleoproterozoic Nyong Group, SW Cameroon: Mineralogical evidence and implications for a high-pressure metamorphism related to a subduction zone at the NW margin of the Archean Congo craton

TL;DR: In this article, a clockwise P-T path with nearly isothermal decompression is deduced from mineral zoning and textural relationships characterized by mineral recrystallization and multi-layered coronitic overgrowths of plagioclase and clinopyroxene surrounding garnet porphyroblasts.
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The global tectonic context of the ca. 2.27-1.96 Ga Birimian Orogen – Insights from comparative studies, with implications for supercontinent cycles

TL;DR: In this article, the Birimian Orogen is considered to have formed in a plate tectonic setting similar to that which currently characterizes SE Asia, with the orogenic system forming in a wedge-shaped complex plate boundary zone, bordered to the north and south by continental blocks and opening up to face a major oceanic basin.
References
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Subcommission on geochronology: Convention on the use of decay constants in geo- and cosmochronology

TL;DR: The IUGS Subcommission on Geochronology (FOOTNOTE 4) as discussed by the authors recommended the adoption of a standard set of decay constants and isotopic abundances in isotope geology.
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Chemical differentiation of the Earth: the relationship between mantle, continental crust, and oceanic crust

TL;DR: In this paper, the average chemical compositions of the continental crust and the oceanic crust (represented by MORB), normalized to primitive mantle values and plotted as functions of the apparent bulk partition coefficient of each element, form surprisingly simple, complementary concentration patterns.
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