Search results for " basin"

showing 10 items of 838 documents

Xenoliths from the sub-volcanic lithosphere of Mt Taranaki, New Zealand

2010

Abstract Mount Taranaki is located 140 km west of the Taupo Volcanic Zone and represents the most westerly expression of subduction-related volcanism on the North Island of New Zealand. Taranaki is a predominantly high-K arc volcano but compositions range from basaltic andesite to andesite with minor dacite and basalt. The sub-volcanic basement under Taranaki is thought to comprise calc–alkaline plutonic and metamorphic rocks of the Median Batholith, overlain by a sequence of Cretaceous and Tertiary sediments. Taranaki lavas contain abundant xenoliths that represent samples of the upper to lower crust beneath the volcano. The xenolith suite has been initially organised into six groups based…

geographygeography.geographical_feature_categoryAndesiteGeochemistryTaranaki BasinVolcanic rockIgneous rockGeophysicsBasaltic andesiteGeochemistry and PetrologyBatholithUltramafic rockXenolithPetrologyGeologyJournal of Volcanology and Geothermal Research
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Palaeoproterozoic crustal accretion and collision in the southern Capricorn Orogen: the Glenburgh Orogeny

2004

Abstract The Capricorn Orogen in central Western Australia records the Palaeoproterozoic collision of the Archaean Pilbara and Yilgarn Cratons. Until recently only one orogenic event was thought to be the cause of this collision, the 1830–1780 Ma Capricorn Orogeny. However, recent work has uncovered an older event, the Glenburgh Orogeny that occurred between 2000 and 1960 Ma. The Glenburgh Orogeny reflects the collision of a late Archaean to Palaeoproterozoic microcontinent (the Glenburgh Terrane) with the Archaean Yilgarn Craton and is therefore tectonically distinct as well as significantly older than the widespread 1900–1800 Ma tectonothermal events recorded in northern Australia. The Gl…

geographygeography.geographical_feature_categoryArcheanGeochemistryMetamorphismGeologyOrogenyYilgarn CratonCratonGeochemistry and PetrologyShear zonePetrologyForeland basinGeologyTerrane
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A New Small Drifter for Shallow Water Basins: Application to the Study of Surface Currents in the Muggia Bay (Italy)

2016

A new small drifter prototype for measuring current immediately below the free surface in a water basin is proposed in this paper. The drifter dimensions make it useful for shallow water applications. The drifter transmits its GPS location via GSM phone network. The drifter was used to study the trajectory of the surface current in the Muggia bay, the latter containing the industrial harbor of the city of Trieste (Italy). The analysis has been carried out under a wide variety of wind conditions. As regards the behavior of the drifter, the analysis has shown that it is well suited to detect the water current since its motion is marginally affected by the wind. The study has allowed detecting…

geographygeography.geographical_feature_categoryArticle Subject010504 meteorology & atmospheric sciencesMeteorologyOcean currentSettore ICAR/02 - Costruzioni Idrauliche E Marittime E IdrologiaDrainage basin010502 geochemistry & geophysics01 natural sciencesCurrent (stream)DrifterWaves and shallow waterOceanographyControl and Systems EngineeringFree surfacelcsh:Technology (General)Trajectorylcsh:T1-995Electrical and Electronic EngineeringInstrumentationBayCoastal Drifter Muggia Bay GPS CommunicationGeology0105 earth and related environmental sciences
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Structurally controlled drainage basin development in the south of Menorca (Western Mediterranean, Spain)

2005

Abstract The south of Menorca consists of a gently folded Upper Miocene carbonate platform over which a drainage system has developed. Three areas with different drainage characteristics have been delimited: the central area, the eastern area and the western area. The central area is characterised by deep streams with steep slopes, whereas the western and eastern areas have slightly incised streams with gentle slopes. The drainage development has been controlled by the inversion of a normal fault in Pliocene times, resulting in a wide anticline with a NNE–SSW orientation. The deep streams of the central area follow the faults associated with this anticline. The amount of incision achieved b…

geographygeography.geographical_feature_categoryCarbonate platformInversion (geology)AnticlineGeochemistryDrainage basinSTREAMSStructural basinDrainage system (geomorphology)DrainageGeomorphologyGeologyEarth-Surface ProcessesGeomorphology
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A management and optimisation model for water supply planning in water deficit areas

2014

Summary The integrated water resources management approach has proven to be a suitable option for efficient, equitable and sustainable water management. In water-poor regions experiencing acute and/or chronic shortages, optimisation techniques are a useful tool for supporting the decision process of water allocation. In order to maximise the value of water use, an optimisation model was developed which involves multiple supply sources (conventional and non-conventional) and multiple users. Penalties, representing monetary losses in the event of an unfulfilled water demand, have been incorporated into the objective function. This model represents a novel approach which considers water distri…

geographygeography.geographical_feature_categoryComputer sciencebusiness.industryDrainage basinIntegrated water resources managementWater supplyDistribution (economics)Environmental economicsWater scarcityWater conservationEmpirical researchbusinessWater resource managementWater useWater Science and TechnologyJournal of Hydrology
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Tectonics and seismicity of the Tindari Fault System, southern Italy: Crustal deformations at the transition between ongoing contractional and extens…

2006

[1] The Tindari Fault System (southern Tyrrhenian Sea, Italy) is a regional zone of brittle deformation located at the transition between ongoing contractional and extensional crustal compartments and lying above the western edge of a narrow subducting slab. Onshore structural data, an offshore seismic reflection profile, and earthquake data are analyzed to constrain the present geometry of the Tindari Fault System and its tectonic evolution since Neogene, including the present seismicity. Results show that this zone of deformation consists of a broad NNW trending system of faults including sets of right-lateral, left-lateral, and extensional faults as well as early strike-slip faults rewor…

geographygeography.geographical_feature_categoryContext (language use)Structural basinInduced seismicityFault (geology)NeogeneTectonicsGeophysicsGeochemistry and PetrologySlabSubmarine pipelineSeismologyGeologyTectonics
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La reserva de semillas en una cuenca de "badlands" (Petrer, Alicante)

1992

In order to determine the influence of erosion in the absence of vegetation of badlands slopes, the seed content of the regolith and the seed removal by runoff in five storms were analyzed in an experimental catchment at Petrer (Alicante). Both, seed redistribution and seed loss were detected, but these seem to be insufficient to explain the lack of vegetation. It is hypothesized that besides the erosion process, factors such as pedoclimate, and chemical and physical properties of the regolith should be considered.

geographygeography.geographical_feature_categoryEcologySoil seed bankDrainage basinfood and beveragesForestrybadlandsVegetationalicante (spain)erosionRegolithlcsh:QH540-549.5ErosionSoil seed bank; badlands; erosion; Alicante (Spain)Environmental sciencelcsh:Ecologysoil seed bankSurface runoffAlicante (Spain)Ecology Evolution Behavior and SystematicsQH540-549.5
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Sabanejewia Aurata (De Filippi, 1863) Populations Management Decisions Support System for Rosci0132 (Olt River Basin)

2015

Abstract The ADONIS: CE was used to design a specific management model for the Sabanejewia aurata (De Filippi, 1863) populations. The proposed model is based on this species, in situ identified biological/ecological necessities in relation to the habitats, the conservation status indicators and appropriate management actions and the pressures and threats founded in the study area. Such on species, on habitats and on site based management system was done to complete this approach for ROSCI0132, the other fish species which are living there being treated already in this respect.

geographygeography.geographical_feature_categoryEcologybiologyEcologyEcology (disciplines)Drainage basingolden spined loachnatura 2000 siteSabanejewia auratabiology.organism_classificationFisherySupport systemromaniamanagementQH540-549.5Transylvanian Review of Systematical and Ecological Research
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Mitigation of urban flooding: A simplified approach for distributed stormwater management practices selection and planning

2005

The urbanization process and the hydraulic insufficiency of drainage systems are two of the most common causes of urban flooding. In some technical regulations, distributed stormwater management practices (DSMPs) are regarded as a solution for urban flooding problems. They can prevent the formation of runoff, dispose of it locally, or dampen its peak before it reaches the drainage system. Due to their diffuse localization and the wide number of available solutions, the evaluation of their efficiency in terms of flood reduction is very difficult. The methodology proposed in the present paper relies on the concept that the mitigation effects of DSMPs can be expressed as a function of the chan…

geographygeography.geographical_feature_categoryFlood mythGeography Planning and DevelopmentFlooding (psychology)Drainage basinEnvironmental engineeringDispose patternUrbanizationDrainage system (geomorphology)Environmental scienceDrainageWater resource managementSurface runoffWater Science and TechnologyUrban Water Journal
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Water resource assessment in karst and fractured aquifers of Termini Imerese-Trabia Mts. (Northern central Sicily, Italy).

2014

The carbonatic siliciclastic Mesozoic reliefs of Termini Imerese-Trabia Mts. (Northern central Sicily) were selected in order to investigate groundwater resources, as these fissured to karstic aquifers are used for potable water supply. These reliefs, part of the Sicilian Apennine Chain, consist of a tectonic units (deformed and emplaced during the Miocene-Pleistocene, and collapsed during the Plio-Pleistocene) mostly formed by clayey pelagic limestones (Sicilidi domain) overthrusting Meso-Cenozoic carbonate and silicoclastic rocks (Imerese Basin, Late Triassic-Early Oligocene) and terrigenous covers (Numidian Flysch, Late Oligocene-Early Miocene). The evolution of karstic network and subsu…

geographygeography.geographical_feature_categoryFlyschGroundwater flowTerrigenous sedimentSettore GEO/04 - Geografia Fisica E GeomorfologiaGeochemistryAquiferStructural basinKarstSiliciclasticGeomorphologyGroundwaterGeologyAquifers karst
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