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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Africa
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Central Africa
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Burundi (1)
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Southern Africa
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Botswana (1)
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hardness
A pilot study investigating the rapid estimation of intact dry density of chalk using low impact energy hardness measurements taken with an Equotip Leeb hardness tester
Ferro-fluoro-edenite, a new amphibole endmember from Vulcano Island (Sicily, Italy)
A new method to rapidly and accurately assess the mechanical properties of geologically relevant materials
Controls on subglacial bedrock erosion and morphology near Drumnadrochit, Scotland
Hybrid nanocomposites of elastomeric polyurethane containing halloysite nanotubes and POSS nanoparticles: tensile, hardness, damping and abrasion performance
Geotechnical Engineering for Mass Mining
Wadi gravel – a new concrete aggregate in Qatar: Part 1 – investigation, processing and trials
Šlikite, Zn 2 Mg(CO 3 ) 2 (OH) 2 ·4H 2 O, a new Zn–Mg carbonate from Plavno, Jáchymov ore district, Czech Republic
Mine Planning and the Crucial Role of Geology
Garnet Compositions Track Longshore Migration of Beach Placers in Western New Zealand
Milanriederite, (Ca, REE ) 19 Fe 3+ Al 4 (Mg,Al,Fe 3+ ) 8 Si 18 O 68 (OH,O) 10 , a new vesuvianite-group mineral from the Kombat Mine, Namibia
Understanding Geologic Uncertainty in Mining Studies
Analysis of tempered bricks: from raw material and additives to fired bricks for use in construction and heritage conservation
Hard-rock aquifer response to pumping and sustainable yield of wells in some areas of Mediterranean Region
Abstract Pumping tests carried out in three highly tectonized Mediterranean areas, which share similar climate conditions, were used to characterize hard-rock aquifers and examine the issue of the sustainable yield of wells. On the basis of the identified drawdown trends and hydraulic parameters, pumping scenarios were simulated through different methods. The results show that the long-term trend in the drawdown and the initial thickness of the aquifer constrain the sustainable yield of a well. In the worst cases examined, namely those related to an aquifer with a barrier boundary and a delayed response of the aquifer, the sustainable well yield is 1–2 L s −1 . These well discharge values are significant when compared with those found in other regions of the world, and may be related to the dense network of the discontinuities which characterizes the sites.
Abstract This research aims to quantify the geophysical signature of the laminated layer, one of the main layers constituting the weathering profile of hard rocks. This laminated layer acts as a marker for locating the underlying groundwater productive stratiform fractured layer (SFL). The study is based at two sites on the interpretation of 50 km of electrical resistivity tomography (ERT) profiles, compared with outcrops and boreholes by geophysical modelling. For the first time, the geophysical signature of the laminated layer, located at the base of the saprolite, is characterized within granite formations. Where the stratiform weathered layer is detected by pole-dipole ERT profiles, the laminated layer is identified as a resistant layer on 90% of the SFL length using an appropriate inversion method. In addition, this layer is also revealed for the first time in certain types of metamorphic formations; here it is revealed in micaschists (62% of the SFL length). The location of the laminated layer in the weathering profile is important (1) for water well siting by determining if an underlying SFL exists in the weathering profile and (2) for assessing the residual thickness of the saprolite, and then evaluating water storage and the protection of the SFL aquifer. Supplementary material: A table presenting the ERT profiles used in this study, with the type of array and inversion method, the inversion parameters (RMSE and number of iterations), and the length of the inverted profiles where the laminated layer (LL) and the stratiform fractured layer (SFL) are identified is available https://doi.org/10.6084/m9.figshare.c.4088768