Lead in oceanic islands: Faial, Azores and Trindade
Explore this paper's citation graph
- Type
- article
- Published
- 1971-05-01
- Cited by
- 27
- References
- 14
- OpenAlex
- https://openalex.org/W2033802391
- Semantic Scholar
- https://api.semanticscholar.org/CorpusID:128479377
Keywords
Geology, Geochemistry, Volcanic rock, Basalt, Mantle (geology)
References
- The petrology of the Las Canadas volcanoes, Tenerife, Canary islands
- ISOTOPIC ANALYSIS OF MICROGRAM QUANTITIES OF LEAD IODIDE USING AN ELECTRON- BOMBARDMENT SOURCE MASS SPECTROMETER.
- Chemical Analyses of Igneous Rocks
- The genesis of basaltic magmas
- Lead isotope compositions and uranium decay series disequilibrium in recent volcanic rocks
- The origin of basaltic and nephelinitic magmas in the earth's mantle
- Isotopic abundances of lead from a “frequently-mixed” source
- Lead isotopic analysis using a double spike
- Isotopic composition of lead in volcanic rocks from Tenerife, Canary Islands
- Isotopic Composition of Lead and Strontium from Ascension and Gough Islands
- A review of experimental evidence on the origin of basaltic and nephelinitic magmas
- Isotopic composition of lead in volcanic rocks from Hawaii, Iwo Jima, and Japan
- Genetic Relations of Oceanic Basalts as Indicated by Lead Isotopes
- ISOTOPIC COMPOSITION OF LEAD FROM OCEANIC ISLANDS.
Cited by
- Isotopic and incompatible element constraints on the genesis of island arc volcanics from Cold Bay and Amak Island, Aleutians, and implications for mantle structure
- Lead isotopic compositions of Tonga-Kermadec volcanics and their petrogenetic significance
- Evolutionary model for lead isotopes in conformable ores and in ocean volcanics
- Magmenevolution auf atlantischen Vulkaninseln
- A study of lateral inhomogeneities in the upper mantle by multiple Scs travel‐time residuals
- Geochemistry of highly-undersaturated ocean island basalt suites from the South Atlantic Ocean: Fernando de Noronha and Trindade islands
- Plume Convection with an Upper-Mantle Temperature Inversion
- Isostasy of aseismic tectonic units in the South Atlantic Ocean and geodynamic implications
- Origin of Ross Island basanitoids and limitations upon the heterogeneity of mantle sources for alkali basalts and nephelinites
- A large-scale isotope anomaly in the Southern Hemisphere mantle
- Oxygen isotope variations in ocean island basalt phenocrysts
- Oceanic island Pb: Two-stage histories and mantle evolution
- Geochemical evidence for the Trindade hotspot trace: Columbia seamount ankaramite
- Trindade and Martı́n Vaz Islands, South Atlantic: Isotopic (Sr, Nd, Pb) and trace element constraints on plume related magmatism
- Reassessment of a reported S-delay under Trindade
- Immiscible Transition from Carbonate-rich to Silicate-rich Melts in the 3 GPa Melting Interval of Eclogite + CO2 and Genesis of Silica-undersaturated Ocean Island Lavas
- Implantação da metodologia de espectrometria 'alfa' para a determinação de isótopos de U e Th em rochas ígneas: aplicação ao estudo do desequilíbrio radioativo na Ilha da Trindade
- Recent plate re-organization at the Azores Triple Junction: Evidence from combined geochemical and geochronological data on Faial, S. Jorge and Terceira volcanic islands
- Radiogenic isotope research
- Deep structure and geophysical processes beneath island arcs
Related papers
- Titania and Alumina Content of Oceanic and Circumoceanic Basalt
- THE SHUMAKER CREEK MEMBER AND BASALT OF POWATKA: TWO HIGH-BA WANAPUM BASALT FLOWS, COLUMBIA RIVER BASALT GROUP
- 87Sr/86Sr ratios in basalts from islands in the Indian Ocean
- Heterogeneous upper mantle Ne, Ar and Xe isotopic compositions and a possible Dupal noble gas signature recorded in basalts from the Southwest Indian Ridge
- An evaluation of major element heterogeneity in the mantle sources of basalts
- Os isotope systematics in ocean island basalts
- Role of the subducted oceanic crust in the origin of HIMU ocean island basalts : evidence from dehydration experiments and geochemistry of Polynesian basalts
- Segregated oceanic crust trapped at the bottom mantle transition zone revealed from ambient noise interferometry
- BORON ISOTOPE AS A TRACER IN THE STUDY OF CRUST-MANTLE EVOLUTION AND SUBDUCTION PROCESSES