Showing 1 - 20 results of 36 for search '"Igneous rock"', query time: 0.09s Refine Results
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    The Extraordinary SVD by Martin, C, Porter, M

    Published 2012
    “…The SVD can be used to characterize political positions of congressmen, measure the growth rate of crystals in igneous rock, and examine entanglement in quantum computation. …”
    Journal article
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    Lithium-isotope fractionation during continental weathering processes by Pistiner, J, Henderson, G

    Published 2003
    “…This may reflect dissolution of secondary minerals from the granite, or differences in the Li-isotope composition of primary minerals in this more evolved igneous rock. Significant Li-isotope fractionation was also observed during sorption onto mineral surfaces in the laboratory, although this was highly dependent on sample mineralogy. …”
    Journal article
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    Coeval calc-alkaline and alkaline Cadomian magmatism in the Bafq, central Iran: Insights into their petrogenesis by Sepidbar, F, Ghorbani, G, Zoheir, B, Palin, R, Homam, SM, Zafar, T, Ma, J, He, L

    Published 2021
    “…The Chah-Gaz and Mishdovan areas in the Bafq magmatic complex, central Iran, contain thick series of terrigenous sediments (the Rizu-Dezu complex), and arc-related calc-alkaline and alkaline igneous rocks. Geochemical analyses of igneous rocks from both areas indicate two distinct rock clans: (1) high-K, calc-alkaline-shoshonitic rocks with strong depletions in Nb, P, and Ti, and (2) an alkaline quartz gabbro-diorite, with trace element patterns resembling oceanic island basalts (OIB). …”
    Journal article
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    The formation of three-grain junctions during solidification. Part I: observations by Fowler, AC, Holness, MB

    Published 2022
    “…The thermodynamic equilibrium dihedral angle at grain junctions in crystalline rocks is set by the grain boundary interfacial surface energies, but the long times required to attain equilibrium mean that the observed dihedral angles in igneous rocks are generally set by the kinetics of crystallisation. …”
    Journal article
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    Hf and Nd isotopes in marine sediments: Constraints on global silicate weathering by Bayon, G, Burton, K, Soulet, G, Vigier, N, Dennielou, B, Etoubleau, J, Ponzevera, E, German, C, Nesbitt, R

    Published 2009
    “…Fine-grained sediments define a diffuse trend, between that for igneous rocks and the 'seawater array', which we refer to as the 'zircon-free sediment array' (εHf = 0.91 εNd + 3.10). …”
    Journal article
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    Cretaceous volcanogenic sediments of the Nauru Basin, Deep Sea Drilling Project, Leg 61. by Moberly, R, Jenkyns, H

    Published 1981
    “…Sedimentary rocks of Barremian through early Maestrichtian age recovered on DSDP Leg 61 had their principal source in the complex of igneous rocks with which they are interlayerd in the Nauru Basin. …”
    Journal article
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    Ion exchange chromatography and high precision isotopic measurements of zirconium by MC-ICP-MS by Schonbachler, M, Rehkamper, M, Lee, D, Halliday, A

    Published 2004
    “…The presented method has been successfully applied to terrestrial igneous rocks, meteorites and mineral separates including samples with high Ti contents.…”
    Journal article
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    Low-blank isotope ratio measurement of small samples of lithium using multiple-collector ICPMS by Magna, T, Wiechert, U, Halliday, A

    Published 2004
    “…Elution schemes are presented for a range of igneous rocks and minerals. δ 7Li values for standards from the U.S. …”
    Journal article
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    Determination of olivine cooling rates from metal-cation ordering by Redfern, S, Henderson, C, Wood, B, Harrison, R, Knight, K

    Published 1996
    “…The mineral olivine - (Fe,Mg,Mn)2SiO4 - is the dominant phase in the Earth's upper mantle, and is also present in a wide range of igneous rocks. Metal cations in olivine crystals are partitioned between two structurally distinct octahedral sites, a property which could in principle be used to obtain important information regarding the thermal history of the host rock. …”
    Journal article
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    Volcanism on Mars controlled by early oxidation of the upper mantle. by Tuff, J, Wade, J, Wood, B

    Published 2013
    “…Detailed information about the chemical composition and evolution of Mars has been derived principally from the SNC (shergottite-nakhlite-chassignite) meteorites, which are genetically related igneous rocks of Martian origin. They are chemically and texturally similar to terrestrial basalts and cumulates, except that they have higher concentrations of iron and volatile elements such as phosphorus and chlorine and lower concentrations of nickel and other chalcophile (sulphur-loving) elements. …”
    Journal article
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    Magma reservoir dynamics at Toba caldera, Indonesia, recorded by oxygen isotope zoning in quartz by Budd, D, Troll, V, Deegan, F, Jolis, E, Smith, V, Whitehouse, M, Harris, C, Freda, C, Hilton, D, Halldórsson, S, Bindeman, I

    Published 2017
    “…Quartz is a common phase in high-silica igneous rocks and is resistant to post-eruptive alteration, thus offering a reliable record of magmatic processes in silicic magma systems. …”
    Journal article
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    Petrogenesis of Proterozoic lamproites and kimberlites from the Cuddapah Basin and Dharwar Craton, southern India by Rao, N, Gibson, SA, Pyle, D, Dickin, A

    Published 2004
    “…Proterozoic mafic potassic and ultrapotassic igneous rocks implaced at the Cuddapah Basin and Dharwar Craton of the southern Indian shield are among the earliest recorded on Earth. …”
    Journal article
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    Crustal-lithospheric structure and continental extrusion of Tibet by Searle, M, Elliott, J, Phillips, R, Chung, S

    Published 2011
    “…We conclude that despite being prominent geomorphological features sometimes with wide mylonite zones, the faults cut earlier formed metamorphic and igneous rocks and show limited offsets. Concentrated strain at the surface is dissipated deeper into wide ductile shear zones. © The Geological Society of London.…”
    Journal article
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    International Ocean Discovery Program Expedition 392 preliminary report: Agulhas Plateau Cretaceous Climate: drilling the Agulhas Plateau and Transkei Basin to reconstruct the Cret... by Uenzelmann-Neben, G, Bohaty, SM, Childress, LB, Archontikis, OA

    Published 2022
    “…Recovery of basement rocks and sedimentary sequences from the Agulhas Plateau sites and a thick sedimentary sequence in the Transkei Basin provides a wealth of new data to (1) determine the nature and origin of the Agulhas Plateau; (2) significantly advance the understanding of how Cretaceous temperatures, ocean circulation, and sedimentation patterns evolved as CO2 levels rose and fell and the breakup of Gondwana progressed; (3) document long-term paleoceanographic variability through the Late Cretaceous and Paleogene; and (4) investigate geochemical interactions between igneous rocks, sediments, and pore waters through the life cycle of a large igneous province (LIP). …”
    Journal article
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    Magma reservoir dynamics at Toba caldera, Indonesia, recorded by oxygen isotope zoning in quartz by Budd, DA, Troll, VR, Deegan, FM, Jolis, EM, Smith, VC, Whitehouse, MJ, Harris, C, Freda, C, Hilton, DR, Halldórsson, SA, Bindeman, IN

    Published 2017
    “…Quartz is a common phase in high-silica igneous rocks and is resistant to post-eruptive alteration, thus offering a reliable record of magmatic processes in silicic magma systems. …”
    Journal article
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    Quantifying metasomatic high-field-strength and rare-earth element transport from alkaline magmas by Sokół, K, Finch, AA, Hutchison, W, Cloutier, J, Borst, AM, Humphreys, MCS

    Published 2021
    “…Alkaline igneous rocks host many global high-field-strength element (HFSE) and rare-earth element (REE) deposits. …”
    Journal article
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    Pore-fluid Fe isotopes reflect the extent of benthic Fe redox recycling: Evidence from continental shelf and deep-sea sediments by Homoky, W, Severmann, S, Mills, R, Statham, P, Fones, G

    Published 2009
    “…The Fe isotope compositions of Crozet region pore fluids are significantly less fractionated (δ56Fe = +0.12‰ to -0.01‰) than the Eel River shelf (δ56Fe = -0.65‰ to -3.40‰) and previous studies of pore-fluid Fe isotopes, relative to average igneous rocks. Our data represent the first measurements of Fe isotope compositions in pore fluids from deep-sea sediments. …”
    Journal article