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The Taylor Creek Rhyolite of New Mexico: a rapidly emplaced field of lava domes and flows

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Abstract

The Tertiary Taylor Creek Rhyolite of southwest New Mexico comprises at least 20 lava domes and flows. Each of the lavas was erupted from its own vent, and the vents are distributed throughout a 20 km by 50 km area. The volume of the rhyolite and genetically associated pyroclastic deposits is at least 100 km3 (denserock equivalent). The rhyolite contains 15%–35% quartz, sanidine, plagioclase, ±biotite, ±hornblende phenocrysts. Quartz and sanidine account for about 98% of the phenocrysts and are present in roughly equal amounts. With rare exceptions, the groundmass consists of intergrowths of fine-grained silica and alkali feldspar. Whole-rock major-element composition varies little, and the rhyolite is metaluminous to weakly peraluminous; mean SiO2 content is about 77.5±0.3%. Similarly, major-element compositions of the two feldsparphenocryst species also are nearly constant. However, whole-rock concentrations of some trace-elements vary as much as several hundred percent. Initial radiometric age determinations, all K−Ar and fission track, suggest that the rhyolite lava field grew during a period of at least 2 m.y. Subsequent 40Ar/39Ar ages indicate that the period of growth was no more than 100 000 years. The time-space-composition relations thus suggest that the Taylor Creek Rhyolite was erupted from a single magma reservoir whose average width was at least 30 km, comparable in size to several penecontemporaneous nearby calderas. However, this rhyolite apparently is not related to a caldera structure. Possibly, the Taylor Creek Phyolite magma body never became sufficiently volatile rich to produce a large-volume pyroclastic eruption and associated caldera collapse, but instead leaked repeatedly to feed many relatively small domes and flows.

The new 40Ar/39Ar ages do not resolve preexisting unknown relative-age relations among the domes and flows of the lava field. Nonetheless, the indicated geologically brief period during which Taylor Creek Rhyolite magma was erupted imposes useful constraints for future evaluation of possible models for petrogenesis and the origin of trace-element characteristics of the system.

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References

  • Bacon CR (1989) Crystallization of accessory phases in magmas by local saturation adjacent to phenocrysts. Geochim Cosmochim Acta 53:1055–1066

    Google Scholar 

  • Bacon CR, Macdonald R, Smith RL, Baedecker PA (1981) Pleistocene high-silica rhyolites of the Coso volcanic field, Inyo Country, California. J Geophys Res 86:10223–10241

    Google Scholar 

  • Christiansen RL, Lipman PW (1966) Emplacement and thermal history of a rhyolite lava flow near Fortymile Canyon, Southern Nevada. Geol Soc Am Bull 77:671–684

    Google Scholar 

  • Dalrymple GB (1989) The GLM continuous laser system for 40Ar/39Ar dating: description and performance characteristics. US Geol Surv Bull 1890:89–96

    Google Scholar 

  • Dalrymple GB, Alexander EC Jr, Lanphere MA, Kraker GP (1981) Irradiation of samples for 40Ar/39Ar dating using the Geological Survey TRIGA reactor. US Geol Surv Prof Pap 1176:55p

  • Dalrymple GB, Duffield WA (1988) High precision 40Ar/39Ar dating of Oligocene rhyolites from the Mogollon-Datil volcanic field using a continuous laser system. Geophys Res Lett 15:463–466

    Google Scholar 

  • Duffield WA, Richter DH, Priest SS (1987) Preliminary geologic map of the Taylor Creek Rhyolite, Catron and Sierra Countries, New Mexico. US Geol Surv Open-file Report 87-515, scale 1:50 000

  • Duffield WA, Ruiz J, Nealy LD (1988) Trace element and isotope variations within the Taylor Creek Rhyolite, southwestern New Mexico. Geol Soc Am Abstr with Prog 20, 7:A281

  • Oggleston TL (1987) The Taylor Creek district, New Mexico: Geology, petrology, and tin deposits. PhD Thesis, New Mexico Institute of Mining and Technology, Socorro, 473 p

  • Elston WE (1968) Terminology and distribution of ash flows of the Mogollon-Silver City-Lordsburg region, New Mexico. Arizona Geol Soc Guiedebook III to southern Arizona: 231–240

  • Elston WE (1976) Glossary of stratigraphic terms of the Mogollon-Datil volcanic province, New Mexico. New Mexico Geol Soc Spec Publ 5:131–151

    Google Scholar 

  • Fries C Jr, Butler AP (1943) Geologic map of the Black Range tin district, New Mexico. US Geol Surv Open-file Map, scale 1:62 500

  • Heyl AV, Maxwell CH, Davis LL (1983) Geology and mineral deposits of the Priest Tank Quadrangle, Sierra Country, New Mexico. US Geol Surv Misc Field Studies Map MF-1665

  • Hurford AJ, Hammerschmidt K (1985) 40Ar/39Ar and K/Ar dating of the Bishop and Fish Canyon Tuffs: calibration ages for fission-track dating standards. Chem Geol 58:23–32

    Google Scholar 

  • Lanphere MA (1988) High-precision 40Ar/39Ar chronology of Oligocene volcanic rocks, San Juan Mountains, Colorado. Geochim Cosmochim Acta 52:1425–1434

    Google Scholar 

  • Lawence VA (1985) A study of the Indian Peaks tin-bearing rhyolite dome-flow complex, northern Black Range, New Mexico. MS Thesis, University of Colorado, Boulder, 112 p

  • Lipman PW (1965) Chemical comparison of glassy and crystalline volcanic rocks. US Geol Surv Bull 1201-D:1–24

    Google Scholar 

  • Lufkin JL (1972) Tin mineralization within rhyolite flow domes, Black Range, New Mexico. PhD Thesis, Stanford University, Stanford, California, 148 p

  • Marvin RF, Naeser CW, Bikerman M, Mehnert HH, Ratte JC (1987) Isotopic ages of post-Paleocene igneous rocks within and bordering the Clifton 1°×2° quadrangle, Arizona-New Mexico. New Mexico Bureau of Mines and Mineral Resources Bull 118, 63 p

  • Maxwell CH, Foord EE, Oakman MR, Harvey DB (1986) Tin deposits in the Black Range tin district. New Mexico Geol Soc Guidebook 37:273–281

    Google Scholar 

  • McIntosh WC, Sutter JF, Chapin CE, Osburn GR, Ratte JC (1986) A stratigraphic framework for the eastern Mogollon-Datil volcanic field based on paleomagnetism and high-precision 40Ar/39Ar dating of ignimbrites — a progress report. New Mexico Geol Soc Guidebook 37:183–195

    Google Scholar 

  • McIntosh WC (1989) Timing and distribution of ignimbrite volcanism in the Eocene-Miocene Mogollon-Datil volcanic field. New Mexico Bureau of Mines and Mineral Res Mem 46:58–59

    Google Scholar 

  • Noble DC (1967) Sodium, potassium and ferrous iron contents of some secondarily hydrated natural silicic glasses. Am Min 52:280–286

    Google Scholar 

  • Ratte JC, Marvin RF, Naeser CW, Bikerman M (1984) Calderas and ash flow tuffs of the Mogollon Mountains, southwestern New Mexico. J Geophys Res 89:8713–8732

    Google Scholar 

  • Reece C, Ruiz J, Duffield WA, Patchett PJ (in press) Origin of Taylor-Creek-Rhyolite magma, Black Range, New Mexico based on Nd−Sr isotope studies. Geol Soc Am Spec Pap 246

  • Richter DH (1978) Geologic Map of the Spring Canyon Quadrangle, Catron County, New Mexico. US Geol Surv Map MF-966:scale 1:24 000

  • Richter DH, Eggleston TL, Duffield WA (1986a) Geologic Map of the Wall Lake Quadrangle, Catron County, New Mexico. US Geol Surv Map MF-1909: scale 1:24 000

  • Richter DH, Lawrence VA, Duffield WA (1986b) Geologic map of the Indian Peaks East Quadrangle, Catron County, New Mexico. US Geol Surv Map MF-1850: sacle 1:24 000

  • Ross CS, Smith RL (1961) Ash-flow tuffs: their origin, geologic relations, and identification. US Geol Surv Prof Pap 366:81 p

  • Samson SD, Alexander EC Jr (1987) Calibration of the interlaboratory 40Ar/39Ar dating standard, MMhb-1. Chem Geol (Isotope Geoscience Section) 66:27–43

    Google Scholar 

  • Smith RL (1960) Zones and zonal variations in welded ash flows. US Geol Surv Prof Pap 354-F:149–159

    Google Scholar 

  • Swanson DA, Dzurisin D, Holcomb RT, Iwatsubo EY, Chadwick WW Jr, Casadevall TJ, Ewert JW, Heliker CC (1987) Growth of the lava dome at Mount St Helens, Washington, (USA), 1981–1983. Geol Soc Am Spec Pap 212:1–16

    Google Scholar 

  • Swanson DA, Holcomb RT (1989) Regularities in growth of the Mount St Helens dacite dome, 1980–1986. In: Jon Fink (ed) The mechanics of lava flow emplacement and dome growth. IAVCEI Proceedings in Vocanology, Springer Berlin Heidelberg New York Tokyo 2:1–24

    Google Scholar 

  • Taylor JR (1982) An introduction to error analysis. Mill Valley, California, University Science Books, 269 p

    Google Scholar 

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Authors and Affiliations

  1. U. S. Geological Survey, 2255 North Gemini Drive, 86001, Flagstaff, AZ, USA

    Wendell A Duffield

  2. U. S. Geological Survey, 345 Middlefield Road, 94025, Menlo Park, CA, USA

    G Brent Dalrymple

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  1. Wendell A Duffield
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  2. G Brent Dalrymple
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Duffield, W.A., Dalrymple, G.B. The Taylor Creek Rhyolite of New Mexico: a rapidly emplaced field of lava domes and flows. Bull Volcanol 52, 475–487 (1990). https://doi.org/10.1007/BF00268927

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