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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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East Africa
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Malawi (1)
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Asia
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Far East
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sulfur
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fossils
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Chordata
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Vertebrata
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Tetrapoda
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Aves
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Neornithes
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Charadriiformes (1)
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geochronology methods
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optical mineralogy (1)
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geologic age
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Cenozoic
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Quaternary
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Holocene
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upper Holocene
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Roman period (1)
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Tertiary
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Oligocene
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Paleozoic
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Permian (1)
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igneous rocks
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igneous rocks
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plutonic rocks
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granites (5)
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volcanic rocks
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pyroclastics
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phosphates
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framework silicates
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orthosilicates
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nesosilicates
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titanite (1)
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sorosilicates
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sheet silicates
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chlorite (3)
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clay minerals
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illite (3)
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sulfates
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melanterite (1)
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pickeringite (1)
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rozenite (1)
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sulfides
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helvite (1)
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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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-
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Asia
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Far East
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Borneo
-
Kalimantan Indonesia (1)
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China
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Chongqing China (1)
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Jiangsu China (1)
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Indonesia
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Kalimantan Indonesia (1)
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Japan
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Honshu
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Hiroshima Japan (1)
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Saitama Japan
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Tochigi Japan (1)
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Middle East
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Turkey (1)
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Atlantic Ocean
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atmosphere (1)
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Australia
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Canada
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Eastern Canada
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Ontario (1)
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Quebec (2)
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Western Canada
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Yukon Territory (1)
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carbon
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C-13/C-12 (1)
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Cenozoic
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Quaternary
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Holocene
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upper Holocene
-
Roman period (1)
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-
-
-
Tertiary
-
Paleogene
-
Eocene
-
upper Eocene (1)
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Oligocene
-
lower Oligocene (1)
-
-
-
-
-
ceramic materials (1)
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chemical analysis (14)
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Chordata
-
Vertebrata
-
Tetrapoda
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Aves
-
Neornithes
-
Neognathae
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Charadriiformes (1)
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-
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clay deposits (1)
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Poland (1)
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Sudeten Mountains
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Southern Europe
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United Kingdom
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England
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geochemistry (14)
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hydrogen (2)
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igneous rocks
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granites (5)
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volcanic rocks
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isotopes
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radioactive isotopes (1)
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C-13/C-12 (1)
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S-34/S-32 (1)
-
-
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magmas (1)
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Malay Archipelago
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Borneo
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Kalimantan Indonesia (1)
-
-
-
metal ores
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copper ores (1)
-
-
metals
-
actinides
-
uranium (1)
-
-
alkali metals
-
potassium (1)
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sodium (1)
-
-
alkaline earth metals
-
barium (1)
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magnesium (1)
-
-
aluminum (3)
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arsenic (1)
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cadmium (1)
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cobalt (2)
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-
iron
-
ferric iron (1)
-
-
lead (1)
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manganese (1)
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nickel (1)
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-
yttrium (1)
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-
metamorphic rocks
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metasomatism (2)
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minerals (20)
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Paleozoic
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Permian (1)
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phase equilibria (5)
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pollution (1)
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sedimentary petrology (2)
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sedimentary rocks
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chemically precipitated rocks
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clastic rocks
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oil shale (1)
-
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sedimentary structures
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planar bedding structures
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bedding (1)
-
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-
sediments
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clastic sediments
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clay (5)
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kaolin (1)
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silt (2)
-
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silicon (1)
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soils (4)
-
South America
-
Brazil
-
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-
-
Chile
-
Atacama Desert (2)
-
-
-
spectroscopy (18)
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springs (1)
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sulfur
-
S-34/S-32 (1)
-
-
thermal analysis (52)
-
United States
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Alaska (1)
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Arizona
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Jerome Arizona (1)
-
-
-
California
-
Santa Clara County California (1)
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Trinity County California (1)
-
-
Iowa
-
Keokuk County Iowa (1)
-
Webster County Iowa (1)
-
-
Michigan
-
Michigan Upper Peninsula
-
Keweenaw County Michigan (1)
-
-
-
-
weathering (4)
-
X-ray analysis (6)
-
-
sedimentary rocks
-
sedimentary rocks
-
carbonate rocks
-
limestone (2)
-
-
chemically precipitated rocks
-
weathering crust (1)
-
-
clastic rocks
-
black shale (1)
-
sandstone (1)
-
shale (1)
-
-
oil shale (1)
-
-
-
sedimentary structures
-
sedimentary structures
-
planar bedding structures
-
bedding (1)
-
-
-
-
sediments
-
sediments
-
clastic sediments
-
clay (5)
-
kaolin (1)
-
silt (2)
-
-
-
-
soils
-
soils (4)
-
thermogravimetric analysis
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.