Geological and geophysical methods were used to investigate the Karoo area extending from longitudes 25.50 E to 27.50 E and latitudes 300 S to 330 S in South Africa, particularly Fort Beaufort, Aliwal North, Venterstad and Smithfield.
Ndlovu, Nkosilathi
core
Neotectonics of the Sea of Galilee (northeast Israel): implication for geodynamics and seismicity along the Dead Sea Fault system. [PDF]
Gasperini L +9 more
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Coseismic river avulsion on surface rupturing faults: Assessing earthquake-induced flood hazard. [PDF]
McEwan E +4 more
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Dolomite luminescence thermochronometry reconstructs the low-temperature exhumation history of carbonate rocks in the central Apennines, Italy. [PDF]
Zhang J +8 more
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Are scattered microsatellites weak chromosomal markers? Guided mapping reveals new insights into Trachelyopterus (Siluriformes: Auchenipteridae) diversity. [PDF]
Haerter CAG +5 more
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Removal of dissolved organic carbon in the West Pacific hadal zones. [PDF]
Chu M +18 more
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Complex Fault Systems and Basin Evolution of the Bonan Area, Eastern China: Effects on the Sedimentation and Distribution of Source Rocks. [PDF]
Wang F +8 more
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Geochemistry and provenance of Mesozoic sandstones in Khon Kaen Geopark: Implication for tectonics of the western Khorat Plateau of Thailand. [PDF]
Singtuen V +5 more
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Direct evidence of active tectonics along the offshore sector of the Dinaric Fault System. [PDF]
Korbar T +4 more
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Utilizing multi-temporal thermal data to assess environmental land degradation impacts: example from Suez Canal region, Egypt. [PDF]
Arnous MO, Mansour BMH.
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