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NARROW
GeoRef Subject
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all geography including DSDP/ODP Sites and Legs
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Asia
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sulfides
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Primary terms
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Africa
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East Africa
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Malawi (1)
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Asia
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Far East
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Borneo
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Middle East
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atmosphere (1)
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carbon
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Tertiary
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ceramic materials (1)
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chemical analysis (16)
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Chordata
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Vertebrata
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sedimentary structures
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South America
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X-ray analysis (7)
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sedimentary structures
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sedimentary structures
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planar bedding structures
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bedding (1)
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-
sediments
-
sediments
-
clastic sediments
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clay (5)
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kaolin (2)
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silt (2)
-
-
-
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soils
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soils (5)
-
thermogravimetric analysis
Evaluation of the Rietveld method for determining content and chemical composition of inorganic X-ray amorphous materials in soils
Characterization and potential toxicity of asbestiform erionite from Gawler Downs, New Zealand
The glass transition temperature of anhydrous amorphous calcium carbonate
Experimental study on the kinetics of magnesiohornblende dehydration and its implications
Thermal Decomposition Kinetics of Clinochlore at High Temperature and Its Implications
High-temperature behaviour of fedorite, Na 2.5 (Ca 4.5 Na 2.5 )[Si 16 O 38 ]F 2 ⋅2.8H 2 O, from the Murun Alkaline Complex, Russia
Sintering inhibition and oil-absorption properties of calcined coal-series kaolin
The crystal structure and chemistry of natural giniite and implications for Mars
The occurrence of monoclinic jarosite in natural environments
Evaluation of forensic soil traces from a crime scene: robbery of a safety deposit box in Brazil
Abstract Soil traces can be used as evidence in criminal investigations due their transferability, great variability and persistence. The soil samples originated from a crime scene that occurred in the Curitiba Metropolitan Region, Brazil. Physical, chemical and mineralogical analyses were carried out on the soil samples. All results were statistically analysed using multivariate analysis (PCA) to verify the relative positioning of soil traces which had been recovered from a stolen safety deposit box (SDB) from a vehicle suspected of being used in the SDB transportation, and from the site allegedly used in the opening of the SDB. The methods employed were effective in discriminating between the sampling sites. The soil from the site used in the opening of the SDB could be excluded as being the location where the soil transferred to the SDB had originated as it was different in many characteristics.