The Alpine Dyke Swarm (ADS), intruding Haast Schist in the Southern Alps, New Zealand, comprises dykes, sills and diatremes of alkaline and ultramafic lamprophyres, phonolites and carbonatites.
Alan F. Cooper (4103437)
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Data on bulk rock compositions, geochemical and textural contrasts between central and marginal parts of dykes, and MELTS modeling of lamprophyre dykes in the Kola Alkaline Carbonatite Province (N Europe). [PDF]
Nosova AA +6 more
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Lithosphere architecture characterized by crust-mantle decoupling controls the formation of orogenic gold deposits. [PDF]
Hou Z +10 more
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Rare earth elements distribution in topsoil from Ditrău Alkaline Massif area, eastern Carpathians, Romania. [PDF]
Ion A, Cosac A.
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Calc–alkaline lamprophyres are known from several localities in the Malá Fatra Mountains. They form dykes (0.5–3 m) of varying degree of alteration that have intruded the surrounding granitoid rocks which are often incorporated xenoliths. Clinopyroxenes (
Vetráková Lucia +6 more
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A dozen ultramafic lamprophyre dykes have been identified in the eastern part of Ungava Bay, Québec. The dark grey dykes are composed of macrocrysts of olivine and phlogopite featuring tetraferriphlogopite rims.
Normand Goulet +4 more
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Interplay between oceanic subduction and continental collision in building continental crust. [PDF]
Zhu DC +8 more
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Oceanic and super-deep continental diamonds share a transition zone origin and mantle plume transportation. [PDF]
Doucet LS, Li ZX, Gamal El Dien H.
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Comparative orotomy of the Archean Superior and Phanerozoic Altaid orogenic systems. [PDF]
Kusky TM, Celâl Şengör AM.
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Widely-distributed lamprophyres in the Laowangzhai gold deposit were associated closely with gold ores. Phlogopite 40Ar/39Ar dating suggests that the emplacement age of lampro-phyric magma ranges from (30.8 0.4) to (34.3 0.2) Ma, and gold ...
Xie Guanghong (ڜۻ +7 more
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