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Field, Geochemical, Geochronological, and Magnetic Data from a Pliocene basalt flow along the Deschutes River in north-central Oregon

Dates

Publication Date
Start Date
2014
End Date
2022

Citation

Pivarunas, A.F., O'Connor, J.E., Cannon, C.M., Sherrod, D.R., and Stelten, M.E., 2023, Field, Geochemical, Geochronological, and Magnetic Data from a Pliocene basalt flow along the Deschutes River in north-central Oregon, U.S. Geological Survey data release, https://doi.org/10.5066/P9R73C3D.

Summary

This dataset represents a variety of scientific measurements of basalt rock outcrops in central Oregon, United States. It consists of field observations, geochemical measurements, paleomagnetic directional measurements, magnetic susceptibility, and geochronology data (Ar-Ar methodology). This dataset was collected from 2014-2022 by the authors.

Contacts

Attached Files

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MagIC_Data Model_v3.0_July_7_2022.json 345.98 KB application/json
TB_Geochem_Data_1.csv 3.35 KB text/csv
TB_Geochem_Data_2.csv 1.32 KB text/csv
TB_Paleomag_Data_MagIC.txt 417.86 KB text/plain
T201-7.txt 20.21 KB text/plain
T202-10.txt 19.98 KB text/plain
T202-10B.txt 17.82 KB text/plain
T203-8.txt 19.52 KB text/plain
T204-2.txt 20.21 KB text/plain
T205-5.txt 19.29 KB text/plain
T206-8.txt 20.14 KB text/plain
T211-8.txt 19.75 KB text/plain
T212-3.txt 19.75 KB text/plain
T213-5.txt 19.9 KB text/plain
T214-6.txt 19.52 KB text/plain
TB_Ar_Data.csv 8.85 KB text/csv
TB_Field_Data.csv 9.46 KB text/csv
EMPTY1.txt 11.34 KB text/plain

Purpose

This dataset was collected in order to correlate a far-traveled basalt flow along the present and ancestral Deschutes River in central Oregon, United States. These data provide a foundation for asserting that widely-separated outcrops of basalt represent the same volcanic episode. They can be used for various purposes related to field geology, geochemistry/petrology, paleomagnetic analysis, and geochronology.

Additional Information

Identifiers

Type Scheme Key
DOI https://www.sciencebase.gov/vocab/category/item/identifier doi:10.5066/P9R73C3D

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