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Geochemical correlations and implications for the magmatic evolutionof basalt flow groups at the Idaho National Engineering andEnvironmental Laboratory

Hughes, Scott S; McCurry, Michael; Geist, Dennis J (2002) Geochemical correlations and implications for the magmatic evolutionof basalt flow groups at the Idaho National Engineering andEnvironmental Laboratory. Special Paper - Geological Society of America, vol.353, pp.151-173,2002

AuthorsHughes, Scott S; McCurry, Michael; Geist, Dennis J
Year2002
TitleGeochemical correlations and implications for the magmatic evolutionof basalt flow groups at the Idaho National Engineering andEnvironmental Laboratory
SourceSpecial Paper - Geological Society of America, vol.353, pp.151-173,2002
Book editorsLink, Paul Karl; Mink, L L
ISBN813723531
ISSN0072-1077
GeoRef2002-042833
Keywordsalkaline earth metals; basalts; Bingham County Idaho; Butte CountyIdaho; chemical composition; Clark County Idaho; Columbia Plateau;correlation; geochemical logging; Idaho; igneous rocks; INEEL; isotoperatios; isotopes; Jefferson County Idaho; lava flows; magmatism;metals; Nd-144/Nd-143; neodymium; rare earths; Snake River plain;Sr-87/Sr-86; stable isotopes; strontium; United States; volcanicrocks; volcanism; well-logging; whole rock

Abstract

Whole-rock major element, trace element, and Sr-Nd isotopic analysesof samples taken from Idaho National Engineering and EnvironmentalLaboratory INEEL core holes are used to correlate subsurfacetholeiitic basalt lava flow groups in the Test Area North TANregion, and to evaluate time-space variations in their geochemicalsignatures. New super 40 Ar/ super 39 Ar ages are included tosupplement existing dates in order to confirm major eruptive episodes.Incompatible trace elements range by factors of approximately 7-10;major oxides, especially MgO, range by factors of approximately 2-3;initial super 87 Sr/ super 86 Sr ratios range from approximately0.706 to 0.708; and super 143 Nd/ super 144 Nd ratios range fromapproximately 0.706 to 0.708; and super 143 Nd/ super 144 Ndratios range from approximately 0.5122 to 0.5125. These data suggestthat each flow group represents a single shield-building monogeneticeruption derived from a separate magma batch. The geochemical patternsof flow groups older than ca. 0.8 Ma at TAN are compared to youngerca. 0.2-0.6 Ma flow groups located in the southern INEEL approximately 30 km distance to assess regional variations. No flowgroups are known to correlate between these two regions although someTAN flow groups are found in core hole 2-2A located approximately 10km south. Only the deepest flow group at TAN, with three measuredradiometric ages ranging from 2.38 to 2.46 Ma, is correlated to corehole USGS 126-A located on Lava Ridge approximately 9 km northwest ofTAN as well as core hole 2-2A. Recurrence of fairly primitiveMgO-rich, La-poor flow groups in the northern and southern INEELsuggests that similar processes of magma genesis and shield growth areoperative on eastern Snake River Plain volcanic rift zones regardlessof age.

276 samples from this reference

SampleRock nameMajorTraceIsotope
ICP121-125Basalt yesyesyes
2A-54Basalt yesyesyes
2A-298Basalt yesyesyes
2A-393Basalt yesyesyes
2A-422Basalt yesyesyes
2A-482Basalt yesyesyes
2A-586Basalt yesyesyes
2A-717Basalt yesyesyes
2A-821Basalt yesyesyes
2A-909Basalt yesyesyes
2A-1269Basalt yesyesyes
2A-1927Basalt yesyesyes
2A-2023Basalt yesyesyes
2A-2327Basalt yesyesyes
2A-2349Basalt yesyesyes
GIN5-30Basalt yesyesyes
GIN5-119Basalt yesyesyes
GIN5-241Basalt yesyesyes
GIN5-327Basalt yesyesyes
GIN5-403Basalt yesyesyes
GIN6-88Basalt yesyesyes
GIN6-133Basalt yesyesyes
GIN6-190Basalt yesyesyes
JC-C-1Basalt yesyesyes
JC-C-2Basalt yesyesyes
T34-215Basalt yesyesyes
T34-283Basalt yesyesyes
T34-334Basalt yesyesyes
T34-416Basalt yesyesyes
TCH1-61Basalt yesyesyes
TCH1-124Basalt yesyesyes
TCH1-216Basalt yesyesyes
TCH1-250Basalt yesyesyes
TCH1-370Basalt yesyesyes
TCH1-596Basalt yesyesyes
TCH2-58Basalt yesyesyes
TCH2-58Basalt yesyesyes
TCH2-99Basalt yesyesyes
TCH2-151Basalt yesyesyes
TCH2-169Basalt yesyesyes
TCH2-197Basalt yesyesyes
TCH2-252Basalt yesyesyes
TCH2-252Basalt yesyesyes
TCH2-296Basalt yesyesyes
TCH2-366Basalt yesyesyes
TCH2-465Basalt yesyesyes
TCH2-636Basalt yesyesyes
TCH2-1113Basalt yesyesyes
TCH1-53Basalt yesyes
TCH1-82Basalt yesyes
TCH1-87Basalt yesyes
TCH1-94Basalt yesyes
TCH1-102Basalt yesyes
TCH1-162Basalt yesyes
TCH1-198Basalt yesyes
TCH1-240Basalt yesyes
TCH1-264Basalt yesyes
TCH1-288Basalt yesyes
TCH1-305Basalt yesyes
TCH1-323Basalt yesyes
TCH1-425Basalt yesyes
TCH1-465Basalt yesyes
TCH1-502Basalt yesyes
TCH1-533Basalt yesyes
TCH1-571Basalt yesyes
TCH2-83Basalt yesyes
TCH2-119Basalt yesyes
TCH2-133Basalt yesyes
TCH2-139Basalt yesyes
TCH2-232Basalt yesyes
TCH2-327Basalt yesyes
TCH2-433Basalt yesyes
TCH2-518Basalt yesyes
TCH2-534Basalt yesyes
TCH2-559Basalt yesyes
TCH2-591Basalt yesyes
TCH2-752Basalt yesyes
TCH2-903Basalt yesyes
TCH2-1017Basalt yesyes
GIN6-71Basalt yesyes
GIN6-112Basalt yesyes
GIN6-159Basalt yesyes
GIN6-168Basalt yesyes
GIN6-199Basalt yesyes
2A-45Basalt yesyes
2A-266Basalt yesyes
2A-333Basalt yesyes
2A-352Basalt yesyes
2A-443Basalt yesyes
2A-462Basalt yesyes
2A-495Basalt yesyes
2A-513Basalt yesyes
2A-543Basalt yesyes
2A-608Basalt yesyes
2A-618Basalt yesyes
2A-655Basalt yesyes
2A-666Basalt yesyes
2A-678Basalt yesyes
2A-756Basalt yesyes
2A-770Basalt yesyes
2A-779Basalt yesyes
2A-808Basalt yesyes
2A-843Basalt yesyes
2A-930Basalt yesyes
2A-955Basalt yesyes
2A-1170Basalt yesyes
2A-1190Basalt yesyes
2A-1212Basalt yesyes
2A-1234Basalt yesyes
2A-1242Basalt yesyes
2A-1284Basalt yesyes
2A-1302Basalt yesyes
2A-1324Basalt yesyes
2A-1335Basalt yesyes
2A-1575Basalt yesyes
2A-1613Basalt yesyes
2A-1777Basalt yesyes
2A-1911Basalt yesyes
2A-1946Basalt yesyes
2A-1984Basalt yesyes
2A-2039Basalt yesyes
2A-2076Basalt yesyes
2A-2096Basalt yesyes
2A-2140Basalt yesyes
2A-2156Basalt yesyes
2A-2201Basalt yesyes
2A-2224Basalt yesyes
2A-2269Basalt yesyes
2A-2305Basalt yesyes
2A-2354Basalt yesyes
2A-2377Basalt yesyes
2A-2392Basalt yesyes
2A-2403Basalt yesyes
2A-2416Basalt yesyes
2A-2424Basalt yesyes
2A-2446Basalt yesyes
2A-2468Basalt yesyes
2A-2482Basalt yesyes
2A-2512Basalt yesyes
2A-2582Basalt yesyes
2A-2609Basalt yesyes
23-48Basalt yesyes
23-65Basalt yesyes
23-86Basalt yesyes
23-101Basalt yesyes
23-138Basalt yesyes
23-179Basalt yesyes
23-200Basalt yesyes
23-215Basalt yesyes
23-234Basalt yesyes
23-248Basalt yesyes
23-266Basalt yesyes
23-291Basalt yes
23-306Basalt yesyes
23-327Basalt yesyes
23-350Basalt yesyes
23-364Basalt yesyes
23-384Basalt yesyes
23-419Basalt yesyes
23-462Basalt yesyes
23-479Basalt yesyes
23-502Basalt yesyes
23-520Basalt yesyes
23-548Basalt yesyes
23-575Basalt yesyes
23-608Basalt yesyes
23-628Basalt yesyes
23-647Basalt yesyes
23-663Basalt yesyes
23-688Basalt yesyes
23-715Basalt yesyes
23-732Basalt yesyes
80-45Basalt yesyes
80-51Basalt yesyes
80-69Basalt yesyes
80-91Basalt yesyes
80-118Basalt yesyes
80-135Basalt yesyes
80-154Basalt yesyes
80-188Basalt yesyes
80-203Basalt yesyes
TRA5-79Basalt yesyes
TRA5-85Basalt yesyes
TRA5-109Basalt yesyes
TRA5-120Basalt yesyes
TRA5-140Basalt yesyes
TRA5-166Basalt yesyes
TRA5-195Basalt yesyes
TRA5-204Basalt yesyes
TRA5-235Basalt yesyes
TRA5-249Basalt yesyes
TRA5-295Basalt yesyes
2A-2526Basalt yesyes
2A-2555Basalt yesyes
126A-16Basalt yesyes
126A-31Basalt yesyes
126A-38Basalt yesyes
126A-48Basalt yesyes
126A-60Basalt yesyes
126A-73Basalt yesyes

First 200 shown; open the results for all.