搜索结果: 1-15 共查到“地球科学总论 the West”相关记录25条 . 查询时间(0.06 秒)
Structural Organization and Tectono-Metamorphic Evolution of the Pan-African Suture Zone: Case of the Kabye and Kpaza Massifs in the Dahomeyide Orogen in Northern Togo (West Africa)
Togo Pan-African Dahomeyide Suture Zone Microstructures
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2013/3/11
The Kabye and Kpaza Massifs correspond to two main granulitic suites in the suture zone of the Pan-African Dahomeyide orogenic belt, in northern Togo. The Kabye Massif is composed of an important west...
Mineralogic Characterization and Petroleum Potential of Clays (Shales) of the N’Kappa Formation (Paléocene-Eocene) in the Douala Sedimentary Sub-basin (South-West Cameroon)
Mineralogy Organic Matter Petroleum Potential
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2013/3/11
The aim of this research work was to report a facies analysis of the N’Kappa formation, identified the clay minerals present in those facies and evaluate their oil potential. For that to be done, Lith...
Estimation of Basal Area in West Oak Forests of Iran Using Remote Sensing Imagery
Northern Zagros Forests Basal Area SPOT-5 Data
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2013/3/7
The objective of this study is to evaluate the capability of satellite imagery for the estimation of basal area in Northern Zagros Forests. The data of the high resolution geometric (HRG) sensor of SP...
Geomechanical Characterization of Sandstones Cliffs of Segou (Senegal, West Africa) in the Madina Kouta Basin
Unconfined Compression Test-Uniaxial Compression Strength (UCT, Rc)
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2013/3/7
This work presents the behavior of Segou sandstones in the laboratory and in the field conditions. Four types of sandstone are collected in the northern part of the Madina Kouta basin (eastern Senegal...
Structural Evolution of a Precambrian Segment: Example of the Paleoproterozoic Formations of the Mako Belt (Eastern Senegal, West Africa)
Kedougou Kenieba Inlier Paleoproterozoic Transpression
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2013/3/7
The western part of the Kedougou Kenieba Inlier is located in the West African Craton. It consists of paleoproterozoic NE-trending elongate belts (subprovinces) of metavolcanic and granitic rocks that...
Gravity Interpretation of the Cameroon Mountain (West Central Africa) Based on the New and Existing Data
Mount Cameroon CVL Gravity Anomalies Bouguer Anomalies
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2013/3/7
A new gravity survey of the Mount Cameroon area has enabled the definition of four major gravimetric do- mains, which coincide with the recognized structural units. In order to determine the nature of...
Deep-Sea Benthic Foraminiferal Distribution in South West Indian Ocean: Implications to Paleoecology
Paleoecology Benthicforaminifera Holocene Indian Ocean
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2013/3/6
Five grab samples from the southwestern part of the Indian ocean were collected by ORV Sagar Kanya during the third expedition to the southern Indian ocean in June 2009. The sediment samples have been...
The TAMORA algorithm: satellite rainfall estimates over West Africa using multi-spectral SEVIRI data
The TAMORA algorithm satellite rainfall estimates West Africa multi-spectral SEVIRI data
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2010/9/10
A multi-spectral rainfall estimation algorithm has been developed for the Sahel region of West Africa with the purpose of producing accumulated rainfall estimates for drought monitoring and food secu...
The Volta Basin Water Allocation System: assessing the impact of small-scale reservoir development on the water resources of the Volta basin, West Africa
Volta Basin Water Allocation System Volta
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2010/2/3
In the Volta Basin, infrastructure watershed development with respect to the impact of climate conditions is hotly debated due to the lack of adequate tools to model the consequences of such developme...
Optical Characterization of an Eddy-induced Diatom Bloom West of the Island of Hawaii
Optical Characterization an Eddy-induced Diatom Bloom West the Island of Hawaii
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2010/1/21
Optical properties were collected along a transect across cyclonic eddy Opal in the lee of Hawaii during the E-Flux III field experiment (10–27 March 2005). The eddy was characterized by an intense do...
Simultaneous measurements of CO2 and water exchanges over three agroecosystems in South-West France
Simultaneous measurements CO2 and water exchanges three agroecosystems South-West France
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2010/1/21
During the last few decades, many studies have been performed to determine water and carbon budgets of broadleaf and deciduous forests, crops and grasslands. However, since most measurements have been...
Modern techniques and Old Red problems–determining the age of continental sedimentary deposits with 40Ar/39Ar provenance analysis in west-central Norway
Modern techniques Old Red problems continental sedimentary deposits 40Ar/39Ar provenance analysis
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2009/12/3
Ages of continental 'Old Red Sandstone' (ORS) deposits in Norway have been notoriously difficult to obtain due to the paucity of fossil-bearing horizons. In general, 40Ar/39Ar ages from detrital mica ...
Temporal and spatial variations in Late Quaternary slope sedimentation along the undersupplied margins of the Rockall Trough,offshore west Ireland
Temporal and spatial variations Late Quaternary slope sedimentation undersupplied margins
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2009/12/3
A total of 63 gravity cores, together with high-resolution bathymetry data and sidescan sonar imagery, were studied along both eastern and western margins of the Rockall Trough, offshore west Ireland....
Elevated erosion surfaces in central West Greenland and southern Norway:their significance in integrated studies of passive margin development
Elevated erosion surfaces southern Norway integrated studies passive margin development
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2009/12/2
Elevated erosion surfaces were used as an independent data set in an integrated study of the landscape development in central West Greenland.The study resulted in a time-constrained model describing m...
The Molo Formation,deposited by coastal progradation on the inner Mid-Norwegian continental shelf,coeval with the Kai Formation to the west and the Utsira Formation in the North Sea
Molo Formation coastal progradation inner Mid-Norwegian continental shelf Kai Formation
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2009/12/2
The Molo Formation represents a characteristic depositional unit on the inner Mid-Norwegian continental shelf and extends along the coast for about 500 km from Møre to Lofoten. It was deposited...