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K-Ar Ages of Volcanic Rocks in Southwest Washington W.M

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K-Ar Ages of Volcanic Rocks in Southwest Washington W.M K-Ar ages of volcanic rocks in southwest Washington W.M. Phillips, M.A. Korosec, H.W. Schasse, J.L. Anderson, and R.A. Hagen Isochron/West, Bulletin of Isotopic Geochronology, v. 47, pp. 18-24 Downloaded from: https://geoinfo.nmt.edu/publications/periodicals/isochronwest/home.cfml?Issue=47 Isochron/West was published at irregular intervals from 1971 to 1996. The journal was patterned after the journal Radiocarbon and covered isotopic age-dating (except carbon-14) on rocks and minerals from the Western Hemisphere. Initially, the geographic scope of papers was restricted to the western half of the United States, but was later expanded. The journal was sponsored and staffed by the New Mexico Bureau of Mines (now Geology) & Mineral Resources and the Nevada Bureau of Mines & Geology. All back-issue papers are available for free: https://geoinfo.nmt.edu/publications/periodicals/isochronwest This page is intentionally left blank to maintain order of facing pages. 18 K-Ar AGES OF VOLCANIC ROCKS IN SOUTHWEST WASHINGTON WILLIAM M. PHILLIPS MICHAEL A. KOROSEC Division of Geology and Earth Resources, Department of Natural Resources, Oiympia, WA 98504 HENRY W. SCHASSE JAMES L. ANDERSON Center for Earth Sciences, University of Southern California, Los Angelas, CA 90007 RANDY A. HAGEN Department of Geology, University of Oregon, Eugene, OR 97403 The K-Ar age determinations reported here support geo complicates the interpretation of K-Ar ages. Because of logic mapping and compilations undertaken for production of alteration and the typical presence of glass or the products the southwest quadrant of the Washington state geologic of devitrification of glass in the groundmass of hypocrystal- map (Walsh and others, in press). Age assignments are line rocks, all our samples required treatment with dilute HP basically from the COSUNA time scale (Salvador, 1985); and/or HNO3. the age of the Eocene-Oligocene boundary is that of Major and minor element concentrations were deter Montanari and others (1985) and Prothero and Armentrout (1985). Geochemical classification of volcanic rocks follows mined for all our samples except sample 35 by x-ray Zanettin (1984). Additional K-Ar ages for rocks in south fluorescence. These data are presented in table 1. Volcanic west Washington are presented in Evarts and others (in rocks were named on the basis of the geochemical data preparation), Vance and others (in press), Frizzell and following the classification of Zanettin (1984). others (1985), Hammond (1980), and Laursen and Samples were processed for K-Ar determinations by one Hammond (1974, 1979). of three laboratories. Samples 1 through 1 8 and sample 35 were run by Krueger Enterprises, Inc., Geochron Lab oratories Division. For these samples, the whole rock was GEOLOGIC BACKGROUND crushed and sieved through 80 and 200-mesh-size (0.1 80-0.075 mm) sieves. Material between 80 and 200 Sampled rocl<s were collected primarily from the south- mesh was treated with dilute HF and HNO3 to remove alteration products and/or glass. Argon measurements r Washington (fig. 1). In this were made by isotope dilution, and argon analyses were Ihm?mhthrough lowerIn Miocene, pyroxene-phyricdominantly of upperandesitic Eocene to performed on a MS-10-type mass spectrometer. Potas sium was measured by flame photometry. Analytical un foods''Quart, r"' volcaniclastic sedimentary certainties for the calculated ages were based on both the estimated standard deviation of precision for the sample (Cox and Dalrymple, 1967) and extensive replication experiments at the laboratory (Hal Krueger, personal com aS tegon"fZ'lr SS munication, 1 986). Samples 1 9 through 30 were processed at the College of Oceanography, Oregon State University under the direction ou.hypabvssal, Miocre''5;oS7o possibly subvokanic '"Lh'"". Plutons. Pliocene of Kristine R. McElwee. Whole-rock samples were crushed ent in the Columbia River Gorge P^eS" and sieved through 10 and 30-mesh-size (2.00-0.6 mm) sieves. Material between 10 and 30 mesh was ultrasoni- andesitic to dacitic stratov"lcan imposing cally cleaned in distilled water, then treated with dilute HF Saint Helens, and Mourn and HNO3 to remove alteration products and/or volcanic Cascade Range; a Pliocene to P®''^ of the glass. Sample 22 is a plagioclase separate prepared by re canic complex is also nrpc Polygenetic vol- moving the non-feldspar components of the rock with standard magnetic and heavy-liquid methods. The plagio Qoa,e™,y'^ba.a|,io,,va-!l^^^^^^^^^^volcanoes, cinder cones ann oharacterized1°" byl«9- shield "■ clase was then washed in dilute HF for 1 0 minutes, fol at Indian Heaven. The Sim systems are present lowed by ultrasonic cleaning in distilled water. Argon Pliocene through early PleistocLo contains measurements were made by isotope dilution, and argon characterized bv voluminn oool^-SfC volcanic rocks analyses were performed by en AEI MS-10S mass spec lesser amounts of basaltin olivine basalt flows with trometer. Potassium concentrations were determined by Most of our K-Ar aS L ^^Yolite. atomic absorption. Analytical uncertainties for the calcu Eocene to lower Miocene vok^ln1^'°"® "PP®"" lated ages were based on the estimated standard deviation which range from 2 to more than k These strata, of precision (Cox and Dalrymple, 1967). ness, commonly lack areallv » . • oSSfegate thick- Teledyne Isotopes processed samples 31 through 34. Whole-rock samples were crushed and sieved through 20 fossiliferous horizons and henrl ly® beds or and 40 mesh-size (0.85-0.425 mm) sieves. Material between 20 and 40 mesh was treated with dilute HF to remove alteration products and/or volcanic glass. Argon measurements were made by isotope dilution, and argon analyses were performed on a MS-10-type mass spec trometer. Potassium concentrations were determined by procedures flame photometry. Analytical uncertainties for the calcu lated ages are based upon the estimated standard deviation Rock alteration resulting from deep burial, contact meta- of precision (Cox and Dalrymple, 1967). Constants used for all of the calculations are = 4.962 morphism near intrusives, or hydrothermal systems is X 10-^0 yr-\ Xe = 0.581 x 10;^° yr-\ and ^^K/Kto^ai = widespread in the southern Washington Cascades and 1.167 X 1Q""* atom percent (Steiger and Jager, 1 977). IISOCHRON/WEST, no. 47, December 1986) 19 ^MtJRalnle Adams Helens Mtns QPv 4' WASHINGTON 20 miles 32 kilometers Location Map 123 122® 12r EXPLANATION Gu Quaternary deposits, undifferentiated Qv Quaternary andesitic to dacitic pyroclastic flows, basalt to basaltic andesite lava flows, and volcaniclastic sediments QPc Quaternary-Pliocene continental sedimentary rocks QPv Quaternary-Pliocene basaltic to andesitic lava flows, dacite and rhyolite domes,and tuffs Pi Pliocene intrusive rocks Mf Middle to upper Miocene Columbia River Basalt Group flood basalt lava flows and inter- bedded continental sedimentary rocks Mc Lower to middle Miocene continental sedimentary rocks Mv Lower to middle Miocene andesite and basaltic andesite lava flows, andesitic to dacitic tuffs daclte plugs and flows, and volcaniclastic sedimentary rocks Mi Miocene granitic to dioritic intrusive rocks 0m Oljgocene tuffaceous marine sedimentary rocks 0v Oligocene andesite and basaltic andesite lava flows, tuffs, and volcaniclastic sedimentary rocks 0Ev Qligocene-Eocene basaltic-andesite and andesite lava flows, tuffs, and volcaniclastic sedimentary rocks Ec Eocene continental sedimentary rocks ^ rocKs En Middle to upper Eocene near-shore marine sedimentary rocks Ev Middle to upper Eocene basalt and basaltic andesite lava flows PT Pre-Tertiary sedimentary and igneous rocks •15 K-Ar sample locality FIGURE 1 Generalized geologic map of southwestern Washington showing location of K-Ar aoe determination samples (modified from Walsh and others, in press). "t i\. Mr age [ISOCHRON/WEST, no. 47, December 1986] 20 TABLE 1. Geochemical data for K-Ar samples. Sample ID SiOa AL2O3 TiOj FeO' MnO CaO MgO K2O Na^O P2O6 1 KK0904855 54.51 15.89 1.64 1 1.69 0.18 8.68 4.09 0.24 2.92 0.16 2 BP0816851 52.13 17.39 1.08 9.70 0.17 10.44 5.92 0.30 2.75 0.14 3 MM0903851 52.99 15.35 1.92 13.10 0.21 8.60 4.34 0.46 2.81 0.23 4 MK8586 53.18 18.27 1.54 9.76 0.16 8.94 4.39 0.61 2.87 0.25 5 MK85817 58.75 15.81 1.09 8.21 0.16 8.20 4.20 0.40 3.00 0.16 6 MK85814 59.76 18.52 1.05 7.13 0.14 7.13 2.07 0.55 3.44 0.20 7 MK8578 60.50 16.75 1.25 8.29 0.14 6.73 2.27 1.09 2.80 0.20 8 MK98415 56.44 17.02 1.27 8.65 0.13 8.72 4.23 0.36 3.00 0.21 9 CC0827851 52.04 16.76 1.27 9.65 0.17 10.96 5.56 0.67 2.69 0.24 10 TW061985D 64.00 17.02 1.03 5.40 0.10 5.15 1.72 2.27 2.94 0.35 11 CC0712852 66.27 13.86 0.84 5.28 0.1 1 5.02 2.54 2.65 3.14 0.30 12 MK8597 52.79 17.06 2.13 10.98 0.18 8.92 4.28 0.85 2.51 0.31 13 BP0604851 50.63 14.03 3.80 13.34 0.20 9.36 4.78 0.49 2.86 0.51 14 MK8589 61.04 16.22 1.14 7.25 0.1 1 6.43 3.32 1.36 2.93 0.20 15 BP0814851 55.99 16.51 1.58 9.25 0.15 8.45 4.08 0.50 3.17 0.31 16 BP0814856 53.62 16.92 1.08 9.24 0.14 9.53 6.47 0.24 2.58 0.16 17 HS0515852 62.62 15.84 1.37 7.80 0.15 4.69 1.85 1.65 3.56 0.49 18 HSRH14623 59.96 17.82 0.95 7.18 0.13 6.95 3.16 0.50 3.15 0.19 19 JA84057 51.02 15.60 2.91 12.24 0.16 8.43 5.60 0.92 2.66 0.46 20 JA84015 55.16 16.93 1.99 9.16 0.13 7.61 4.43 1.44 2.83 0.32 21 JA84017 77.36 12.37 0.1 1 1.43 0.01 0.04 0.00 4.67 3.98 0.03 22 BP1004842 59.32 16.24 1.12 7.55 0.14 6.96 3.63 1.41 3.43 0.22 23 HS0612851 63.33 16.70 0.93 5.64 0.10 6.1 5 2.66 1.22 3.09 0.18 24 MK85546 57.21 18.58 1.09 8.03 0.23 7.95 2.99 0.53 3.20 0.19 25 MK85635 68.04 14.79 0.92 5.50 0.1 1 3.74 1.07 2.41 3.20 0.22 26 MK85627 57.37 19.19 1.12 7.56 0.14 7.75 2.29 1.05 3.26 0.25 27 MK85523 65.97 17.43 0.61 4.19 0.08 5.57 1.71 0.95 3.32 0.16 28 MK8551 67.35 17.08 0.49 3.87 0.08 4.95 1.48 0.92 3.62 0.16 29 MK88412 53.20 17.93 1.45 9.16 0.16 9.81 4.19 0.56 3.28 0.25 30 BP0619851 55.25 16.14 1.06 8.32 0.15 9.16 6.45 0.86 2.44 0.18 31 BP0516851 54.10 17.64 1.51 9.04 0.16 9.27 4.62 0.42 2.97 0.27 32 MM0904851 53.33 16.55 2.31 11.58 0.18 8.08 4.25 0.76 2.66 0.30 33 HS0116853 56.06 16.88 1.43 9.97 0.15 7.96 3.61 0.47 3.24 0.22 34 HS0117851A 57.52 17.57 1.29 7.79 0.12 7.81 3.48 0.90 3.21 0.31 Analyses by XRF, Department of Geology, Washington State University.
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