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Kamber, B. Tectonics , 15 6 , pp. View at publisher. The thermal peak of degrees C at 0. The coincidence of the temperature T maximum and compression is thought to be a response to lithospheric mantle thinning that resulted in granite emplacement and a consequent change in upper crustal theology. After initial exhumation and cooling, these high-temperature, low-pressure rocks resided at a comparatively shallow depth approximate to 10 km for Ma. Field, microstructural, and geochronological investigation of a low-temperature overprint establishes that reworking and final exhumation occurred at 1.

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The P—T—t path of high-grade metamorphic rocks is significant for understanding vertical motions and heating of the crust. In general, garnet is used to constrain P—T paths and metamorphic zircon is used to obtain t for different metamorphic stages. However, this approach may be complicated by polyphase tectonothermal events.

events in the Central Zone of the Limpopo Belt using Pb single phase dating of Dating of relic metamorphic assemblages can provide important information.

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Unraveling the record of successive high grade events in the Central Zone of the Limpopo Belt using Pb single phase dating of metamorphic minerals. Research.

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A Nature Research Journal. Precise dating of diamond growth is required to understand the interior workings of the early Earth and the deep carbon cycle. Here we report Sm-Nd isotope data from 26 individual garnet inclusions from 26 harzburgitic diamonds from Venetia, South Africa. Garnet inclusions and host diamonds comprise two compositional suites formed under markedly different conditions and define two isochrons, one Archaean 2.

The Archaean diamond suite formed from relatively cool fluid-dominated metasomatism during rifting of the southern shelf of the Zimbabwe Craton.

The MIS5 Pietersburg at ‘28’ Bushman Rock Shelter, Limpopo Province, South Africa

Skip to search form Skip to main content You are currently offline. Some features of the site may not work correctly. DOI: This age, combined with petrographic and field observations, suggests the metamorphism in the syenites occurred during Palaeoproterozoic event. View via Publisher. Save to Library.

() Unraveling the record of successive high grade events in the Central Zone of the Limpopo Belt using Pb single phase dating of metamorphic minerals.

Many Precambrian granulite-facies metamorphic complexes contain so-called straight gneisses, which are massive rocks with a clearly pronounced blastomylonitic texture, lineation, and gneissosity. These rocks occur exclusively in high-temperature ductile shear zones, which can develop either during the primary exhumation of rock complexes or during the overprinting by high-temperature dynamometamorphism.

The main criterion for distinguishing between these two types of straight gneisses is the configuration of their P-T trajectories, which are recorded in the mineral assemblages in these rocks and their host gneisses. Straight gneisses in Proterozoic polymetamorphic complexes commonly compose high-temperature ductile shear zones overprinted on Archean granulite complexes, and the P-T paths of these rocks are Z-shaped.

Such ductile shear zones commonly have a strike-slip morphology and can be easily seen in aerial photographs and discerned during structural geological surveying. These zones can overprint older gneisses without any notable thermal effect on the latter.

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In this multicentre, open-label, randomised trial, we recruited patients with uncomplicated P falciparum malaria at 18 hospitals and health clinics in eight countries. We excel on the partnerships we build with our donors, country and regional offices, various ministries of health and most importantly the lives we touch. This was attributed to the capacity of sFGL2 to inhibit HIV, tuberculosis, malaria,neglected tropical diseases and viral hepatitis affect billions of people around the world, and cause more than 4 million deaths each year.

The Northern Marginal Zone;; The Central Zone; and; The Southern Marginal Pilanesberg exhibits evidence of human civilisations dating back as far as the.

Ductile shear zones associated with the to Ma Limpopo Orogeny locally contained gold mineralization. Some of these shear zones were reactivated under brittle conditions and contain zones of hydrothermal alteration that are of potential economic significance. Within the approximately Ma Matok Complex, two examples of this shear zone controlled alteration are exposed, the Dwars River and Sand River alteration zones.

The granitic rocks of this Complex experienced early selective sericitization of plagioclase and the subsequent development of perthitic porphyroblasts. This early regional alteration was overprinted along brittle shear zones by pervasive propylitization and vein controlled quartz-albite alteration. The setting, composition, and the age of the Matok Complex make it a possible source for Archaean gold mineralization. The Dwars River and Sand River alteration zones are characterized by the absence of significant gold mineralization.

The pattern of wall-rock alteration indicates that the hydrothermal processes were different from typical Archaean lode gold deposits. P-T conditions during the shear-zone controlled alteration were less than degrees C and 1,9 – 2,8 kb. The shear zone hosted alteration could have taken place anytime between emplacement of the Matok Complex and about Ma ago.

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In the past few decades, a diverse array of research has emphasized the precocity of technically advanced and symbolic practices occurring during the southern African Middle Stone Age. However, uncertainties regarding the regional chrono-cultural framework constrain models and identification of the cultural and ecological mechanisms triggering the development of such early innovative behaviours.

Comparisons with other published lithic assemblages show technological differences between the Pietersburg from BRS and other southern African MIS5 traditions, especially those from the Western and Eastern Cape. We argue that, at least for part of MIS5, human populations in South Africa were regionally differentiated, a process that most likely impacted the way groups were territorially and socially organized.

ABSTRACT Sequential reaction textures in Archaean garnet-corundum-​sapphirine granulites from the Central Zone of the Limpopo Belt document a progression.

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Decompressional Heating of the Mahalapye Complex (Limpopo Belt, by in situ dating of monazite, xenotime and zircon grains from metasediments, and a.

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OPINION: Digit preference during Covid-19 yet to play out

By Opinion Aug 21, In the study of data on human populations, especially in less literate stings, digit preference for age or year of birth is driven by several factors. Dramatic events in life affect procreation and progression of cohorts of populations. Pestilence, famines and wars play a major role in driving cohorts.

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Fossil Hominid Sites of South Africa

There is a close, fundamental relationship between soils and the geology of the rocks that lie beneath them. Most soils are weathered and modified sediments from underlying bedrock , or have been transported to their present location by some form of mass transit. The lithology and geological structure of a region has a direct result on the storage, quality, availability and recharge potential of groundwater resources.

Moho poorly defined beneath the Limpopo–Shashe Belt central zone. (cf. Nguuri et ). Further, Re/Os dating of mantle nodules from the.

In the past few decades, a diverse array of research has emphasized the precocity of technically advanced and symbolic practices occurring during the southern African Middle Stone Age. However, uncertainties regarding the regional chrono-cultural framework constrain models and identification of the cultural and ecological mechanisms triggering the development of such early innovative behaviours.

Comparisons with other published lithic assemblages show technological differences between the Pietersburg from BRS and other southern African MIS5 traditions, especially those from the Western and Eastern Cape. We argue that, at least for part of MIS5, human populations in South Africa were regionally differentiated, a process that most likely impacted the way groups were territorially and socially organized.

Nonetheless, comparisons between MIS5 assemblages also indicate some typological similarities, suggesting some degree of connection between human groups, which shared similar innovations but manipulated them in different ways. We pay particular attention to the end-scrapers from BRS, which represent thus far the earliest documented wide adoption of such tool-type and provide further evidence for the innovative processes characterizing southern Africa from the MIS5 onwards. Editor: Michael D. This is an open access article distributed under the terms of the Creative Commons Attribution License , which permits unrestricted use, distribution, and reproduction in any medium, provided the original author and source are credited.

The funders had no role in study design, data collection and analysis, decision to publish, or preparation of the manuscript.

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