HelioWebStellenbosch University, South Africa
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I[Stellenbosch University, South Africa]
PI["Parent Institutions (0)"]
CI["Child Institutions (0)"]
AW["Affiliated Works (38)"]
CA["Linked Collaborating Authors (2)"]
I== skos:broader ==>PI
CI== skos:broader ==>I
AW== affil ==>I
AW== author ==>CA
click PI "#parent-institutions"
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Child Institutions [?]
Affiliated Works
sorted by decreasing year, and then by display-name
- A New Phase of Exploration and Understanding: Planning for The International Polar Year - 2007/2008
- Vestiges of a 3.2 Ga Subduction Zone, as Evidenced by High-Pressure, Low-Temperature Metamorphism in the Barberton Greenstone Belt
- A 3.2 Ga Magmatic arc Preserving 50 Ma of Crustal Convergence in the Barberton Terrain, South Africa
- The Araguainha impact crater at the Permo-Triassic boundary: implications for the carbon isotope excursion and the mass extinction.
- The Permo-Triassic Araguainha impact structure (central Brazil): impact products and collapse history in the central peak-ring
- The role and fate of peritectic garnet in S-type granite Petrogenesis: The example of the Cape Granite Suite (South Africa)
- Evolution of the North Central Peruvian Subduction Zone: Evidence From Late-Stage Adakite-Like Ignimbrites
- Thick fluidized cataclasites from subduction (Pasagshak Point Thrust, Alaska) and continental (Naukluft Thrust, Namibia) faults - textural evidence for transient weakening?
- Co-seismic thermal dissociation of carbonate fault rocks: Naukluft Thrust, central Namibia
- Paleoarchaean rhyolitic volcanism and the origin of the granitic continental crust
- Possible silica gel in the Olive Fault, Naukluft Nappe Complex, Namibia: A geologic record of dynamic weakening in faults during continental orogenesis
- U-Pb ages of zircons from sites in Spain and Italy provide more evidence linking the Chicxulub impact to the global K-P boundary layer
- Discontinuous melt segregation and granitic pluton construction exemplified from field observations in the Damara Belt, Namibia
- Growth of early continental crust by water-present eclogite melting in subduction zones
- The Mesoarchaean Tartoq Group suprasubduction zone ophiolite, SW Greenland
- The Early Life of a Stable Continental Craton: Mechanisms of Accretion as Consequences of a Late Neoproterozoic Ridge-Trench Interaction, Khomas Complex, Damara Belt, Namibia
- First demonstration of transcontinental SQUID magnetometry (Invited)
- Structural study and geochronology in the Hook Batholith, Central Zambia
- Subduction-related magmatism and crustal role in the early stage of the Damara Orogen, Namibia: new constraints from combined U-Pb and Lu-Hf isotopes from the Goas Magmatic Complex
- Composition of Crustal Melts at the Source Area: Information from Glassy Melt Inclusions in Anatectic Enclaves
- Kalahari Tectonic Landforms and Processes Beyond the Okavango Graben
- Metasomatic Diamond Formation revealed by X-Ray CT Scanning of Diamondiferous Eclogites from Southern Africa
- The Pliocene Sea Ice Cover in the Arctic Ocean
- The Tonalite-Trondhjemite-Granodiorite (TTG) to Calc-alkaline Granodiorite-Granite Transition: Evolution of the Archaean Basement of the Quadrilátero Ferrífero Province (Southeast Brazil)
- Assessing ecosystem response to multiple disturbances and climate change in South Africa using ground- and satellite-based measurements and model
- Climatic variability during the last deglaciation: A stalagmite-based multi-proxy record from Mawmluh cave, India
- Melting mud in Earth's mantle, evidence from sub-Moho S-type granites with extreme oxygen isotope signatures
- Enhancing the Extreme Climate Index (ECI) to monitor climate extremes for an index-based insurance scheme across Africa
- Modern Ocean Ground-truthing of Planktic Foraminifera-bound Nitrogen Isotopes
- Multi-Proxy Record of Indian Summer Monsoon Variability Since the Last Glacial Maximum
- Effects of an Explosive Polar Cyclone Crossing the Antarctic Marginal Ice Zone
- Forecasting future global biodiversity: Predicting current and future global plant distributions, community structure, and ecosystem function
- Magma flow and igneous differentiation at high crystallinity: Beginning to see the light
- Origin of sulfur in carbonatites revealed by isotopes : From a subduction influence to crustal imprint.
- The Variability of Indian Summer Monsoon Through Early to Mid-Holocene
- Use of Statistical Methods and Geospatial Techniques in Understanding Riverine Geochemistry
- Evaluating Climate-related Risks for Biosphere Reserves in South Africa
- Forest types outpace constituent tree species in range shifts under global change