Search Results - "Rollinson, H."

Petrology of a Late Archaean, Highly Potassic, Sanukitoid Pluton from the Baltic Shield: Insights into Late Archaean Mantle Metasomatism by Lobach-Zhuchenko, S. B., Rollinson, H., Chekulaev, V. P., Savatenkov, V. M., Kovalenko, A. V., Martin, H., Guseva, N. S., Arestova, N. A.

“…The late Archaean Panozero pluton in Central Karelia (Baltic Shield) is a multi-phase high-Mg, high-K intrusion with sanukitoid affinities, emplaced at 2·74…”
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Petrogenesis of early cretaceous carbonatite and ultramafic lamprophyres in a diatreme in the Batain Nappes, Eastern Oman continental margin by Nasir, S., Al-Khirbash, S., Rollinson, H., Al-Harthy, A., Al-Sayigh, A., Al-Lazki, A., Theye, T., Massonne, H.-J., Belousova, E.

“…Allochthonous carbonatite and ultramafic lamprophyre occur in a diatreme at the beach of the Asseelah village, northeastern Oman. The diatreme consists of…”
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A Metamorphosed, Early Archaean Chromitite from West Greenland: Implications for the Genesis of Archaean Anorthositic Chromitites by ROLLINSON, HUGH, APPEL, PETER W. U., FREI, ROBERT

“…An early Archaean (>3·81 Ga) chromitite–ultramafic layered body from the Ujaragssuit nunât area, west Greenland, may represent the Earth’s oldest chromitite…”
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Cyanide from gold mining and its effect on groundwater in arid areas, Yanqul mine of Oman by Abdalla, Osman A. E., Suliman, F. O., Al-Ajmi, H., Al-Hosni, T., Rollinson, H.

“…The use of cyanide (CN), which is characterized by volatility, toxicity and high odor, in gold mining is scarcely addressed in the literature and remain…”
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Enhanced molecular identification of Botrytis spp. from New Zealand onions by Khan, M. Ikram, Marroni, Virginia, Keenan, Sandi, Scott, Ian A. W, Viljanen-Rollinson, Suvi L. H, Bulman, Simon

“…Botrytis spp. associated with neck rot disease were isolated from New Zealand onions. The fungi were identified using molecular sequences of the ribosomal…”
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The magmatic, metamorphic and tectonic evolution of the northern marginal zone of the Limpopo Belt in Zimbabwe by Rollinson, H, Blenkinsop, T

“…This zone comprises an assemblage of granitic rocks, including a distinctive suite of porphyroclastic granites and a much less abundant supracrustal assembalge…”
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The use of the area under the disease-progress curve (AUDPC) to assess quantitative disease resistance in crop cultivars by JEGER, M. J, VILJANEN-ROLLINSON, S. L. H

“…Calculation of the area under the disease-progress curve (AUDPC) as a measure of quantitative disease resistance entails repeated disease assessments. For…”
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The Archaean sanukitoid series of the Baltic Shield: geological setting, geochemical characteristics and implications for their origin by Lobach-Zhuchenko, S.B., Rollinson, H.R., Chekulaev, V.P., Arestova, N.A., Kovalenko, A.V., Ivanikov, V.V., Guseva, N.S., Sergeev, S.A., Matukov, D.I., Jarvis, K.E.

“…Archaean high-Mg granitoids (sanukitoids) occur in the Karelian granite–greenstone terrain in the Baltic Shield in two distinct zones. In the west of the…”
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Techniques for the treatment, removal and disposal of host material during programmes for plant pathogen eradication by Sosnowski, M.R, Fletcher, J.D, Daly, A.M, Rodoni, B.C, Viljanen-Rollinson, S.L.H

“…Eradication of plant pathogen incursions is very important for the protection of plant industries, managed gardens and natural environments worldwide. The…”
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Geology and petrology of the archean high-K and high-Mg Panozero massif, Central Karelia by Lobach-Zhuchenko, S. B., Rollinson, H., Chekulaev, V. P., Guseva, N. S., Arestova, N. A., Kovalenko, A. V.

“…The high-K and high-Mg Panozero central-type intrusion is located on the shore of Lake Segozero, Central Karelia, and has an age of 2737 ± 10 Ma. Detailed…”
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Archaean Intracrustal Differentiation from Partial Melting of Metagabbro--Field and Geochemical Evidence from the Central Region of the Lewisian Complex, NW Scotland by Johnson, T. E., Fischer, S., White, R. W., Brown, M., Rollinson, H. R.

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Oxygen isotopes of an Early Archaean layered ultramafic body, southern West Greenland: implications for magma source and post-intrusion history by Lowry, D., Appel, P.W.U., Rollinson, H.R.

“…A large number of metamorphosed ultramafic bodies are found in the region SW of the Isua Greenstone Belt in southern West Greenland, enclosed in Archaean…”
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The Triangle Shearzone, Zimbabwe, revisited: new data document an important event at 2.0 Ga in the Limpopo Belt by Kamber, B.S., Kramers, J.D., Napier, R., Cliff, R.A., Rollinson, H.R.

“…The Limpopo Belt in Southern Africa has been used to demonstrate that modern-style continent-continent collision operated during the Late Archaean (2.6–2.7…”
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Chromite in the mantle section of the Oman ophiolite: A new genetic model by Rollinson, Hugh

“…This paper reviews the compositional data (major elements, platinum group element [PGE] concentrations, Os‐ and O‐isotopes) for chromites from the mantle…”
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Metamorphic history suggested by garnet-growth chronologies in the Isua Greenstone Belt, West Greenland by Rollinson, Hugh

“…Compositional maps for garnets from the five tectonic domains of the Isua Greenstone Belt in West Greenland are used to identify episodes of garnet growth…”
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Eclogite xenoliths in west African kimberlites as residues from Archaean granitoid crust formation by Rollinson, Hugh

“…Eclogites are a comparatively rare but petrologically important member of kimberlite xenolith suites. Their broadly basaltic chemistry has led many authors to…”
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Ratio Correlations and major element mobility in altered basalts and komatiites by ROLLINSON, H. R, ROBERTS, C. R

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Geodynamic controls on adakite, TTG and sanukitoid genesis: implications for models of crust formation: Introduction to the Special Issue by Rollinson, Hugh, Martin, Hervé

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Zonation of supracrustal relics in the Archaean of Sierra Leone, Liberia, Guinea and Ivory Coast by ROLLINSON, H. R

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The Archean komatiite-related Inyala Chromitite, southern Zimbabwe by Rollinson, Hugh

“…The chromitites at the Inyala mine, Zimbabwe, form part of a layered intrusion enclosed within the Archean granulite facies gneisses of the north marginal zone…”
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