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Titanium concentrations in stream sediments from the Atlantic Coastal Plain of the southeastern U.S. (1975-1999)

Dates

Publication Date
Start Date
1975
End Date
1999

Citation

Ellefsen, K.J., 2017, Titanium concentrations in stream sediments from the Atlantic Coastal Plain of the southeastern U.S. (1975-1999): U.S. Geological Survey data release, https://doi.org/10.5066/F7J38R16.

Summary

The titanium concentrations were obtained from a data set that is called the "National Geochemical Survey." This data set, as well as its documentation, are available in U.S. Geological Survey Open-File Report 2004-1001 (https://mrdata.usgs.gov/geochem/doc/home.htm). The titanium concentrations were measured in 3,457 samples of stream sediments from the coastal plain of the southeastern United States; this area includes parts of Virginia, North Carolina, South Carolina, Georgia, Florida, and Alabama. The samples were collected between 1975 and 1999 during several field surveys, and the concentrations were measured using inductively coupled plasma-atomic emission spectrometry.

Contacts

Point of Contact :
Karl J Ellefsen
Originator :
Karl J Ellefsen
Metadata Contact :
Karl J Ellefsen
Publisher :
U.S. Geological Survey
Distributor :
U.S. Geological Survey - ScienceBase
USGS Mission Area :
Energy and Minerals
SDC Data Owner :
Geology, Geophysics, and Geochemistry Science Center

Attached Files

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Conc.csv 174.88 KB text/csv
Shapefile: TitaniumConcentrations.zip
TitaniumConcentrations.cpg 5 Bytes
TitaniumConcentrations.dbf 165.55 KB
TitaniumConcentrations.prj 145 Bytes
TitaniumConcentrations.sbn 32.62 KB
TitaniumConcentrations.sbx 1.68 KB
TitaniumConcentrations.shp 94.62 KB
TitaniumConcentrations.shx 27.11 KB

Purpose

The titanium concentrations were obtained to help assess titanium mineral resources that are hosted in heavy-mineral sands within the coastal plain of the southeastern United States.

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/F7J38R16

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