We are improving our search experience. To check which content you have full access to, or for advanced search, go back to the old search.

Search

Please fill in this field.
Filters applied:

Search Results

Showing 921-940 of 940 results
  1. Subduction-related shoshonitic and ultrapotassic magmatism: a study of Siluro-Ordovician syenites from the Scottish Caledonides

    Syenites are important or predominant components of several plutonic complexes, emplaced between 456 and 415 Ma along the NW margin of the Caledonian...

    R. N. Thompson, M. B. Fowler in Contributions to Mineralogy and Petrology
    Article 01 December 1986
  2. The Vanuatu Island Arc: An Outline of the Stratigraphy, Structure, and Petrology

    Vanuatu (formerly the New Hebrides Anglo—French Condominium) forms one sector of a Cretaceous to Recent island arc system extending from New Britain...
    J. N. Carney, A. Macfarlane, D. I. J. Mallick in The Ocean Basins and Margins
    Chapter 1985
  3. Solomon Islands

    Solomon Islands form part of a complex of Melanesian island arcs and marginal basins that extend in a southeasterly direction across the southwest...
    Frank I. Coulson in The Ocean Basins and Margins
    Chapter 1985
  4. Piezomagnetic monitoring in the South Pacific region

    Data from an array of piezomagnetic stations in the South Pacific Islands indicate that noise limitations on piezomagnetic stress monitoring reported...

    Michael T. Gladwin in pure and applied geophysics
    Article 01 November 1984
  5. Field setting, mineralogy, chemistry, and genesis of arc picrites, New Georgia, Solomon Islands

    The field setting, petrography, mineralogy, and geochemistry of a suite of picrite basalts and related magnesian olivine tholeiites (New Georgia arc...

    W. R. H. Ramsay, A. J. Crawford, J. D. Foden in Contributions to Mineralogy and Petrology
    Article 01 December 1984
  6. Pacific Plate Motion Recorded by Linear Volcanic Chains

    Seamounts and islands are quite common features of the deep-ocean basins, particularly the Pacific Basin. A conspicuous but relatively small number...
    Robert A. Duncan, David A. Clague in The Ocean Basins and Margins
    Chapter 1985
  7. Earthquake distribution and volcanism in Kamchatka, Kurile Islands, and Hokkaido Part 3: Southern Kuriles and Hokkaido

    The morphology of the Wadati-Benioff zone in the region of Southern Kuriles and Hokkaido, based on the distribution of 4015 earthquake foci, verified...

    Václav Hanuš, Jiří Vaněk in Studia Geophysica et Geodaetica
    Article 01 September 1984
  8. The origin of reversed geochemical zoning in the northern New Hebrides volcanic arc

    Integration of petrographic and geochemical data on each island in the Banks Group, northern Vanuatu (New Hebrides) has revealed a decrease in K 2 O...

    M. Barsdell, I. E. M. Smith, K. B. Spörli in Contributions to Mineralogy and Petrology
    Article 01 December 1982
  9. Quaternary Pisoids of Lau, Fiji

    Pisoids, concentrically laminated grains between 2 mm and 10 mm in diameter, originate in a variety of environments and the word pisoid is now seldom...
    C. J. Burgess in Coated Grains
    Conference paper 1983
  10. Three Kings Ridge: a west-facing arc

    The Three Kings Ridge has been described as a remnant arc or an east-facing arc on the western side of the South Fiji Basin under which symmetric...

    L. W. Kroenke, J. V. Eade in Geo-Marine Letters
    Article 01 March 1982
  11. Announcements

    Article 01 September 1981
  12. d'Entrecasteaux Zone, trench and western chain of the central New Hebrides island arc: Their significance and tectonic relationship

    The absence of a trench and the existence of a separate, western chain of islands in the central New Hebrides island arc are a consequence of earlier...

    J. Daniel, H. R. Katz in Geo-Marine Letters
    Article 01 September 1981
  13. The Plate Tectonic Connection

    The Earth’s surface has four plate tectonic environments: divergent, convergent, and transform fault plate boundaries, and intra-plate locations....
    Chapter 1981
  14. Spatial and Temporal Variations in the Composition of Orogenic Andesites

    Comparing orogenic andesites within and between volcanic arcs or over time requires (1) choosing a reference point such as a specified wt.% SiO2 or...
    Chapter 1981
  15. Geophysical Setting of Volcanism at Convergent Plate Boundaries

    Active volcanoes occur at topographic highs approximately 60 to 500 km from convergent plate boundaries which usually are associated with ocean...
    Chapter 1981
  16. Bulk Chemical Composition of Orogenic Andesites

    Bulk chemical analyses of andesites are used primarily in two ways to evaluate andesite origins. First, average elemental and isotopic compositions...
    Chapter 1981
  17. Andesite Magmas, Ejecta, Eruptions, and Volcanoes

    Studies of the tectonic significance, petrography, and chemical composition of andesites have been more common than detailed investigations of the...
    Chapter 1981
Did you find what you were looking for? Share feedback.