Results 71 to 80 of about 446 (178)
This work reports a geochemical overview and modelling of the lavas erupted similar to 4.4 Ma ago at San Vincenzo (Tuscan Magmatic Province, TMP). Although these lavas cover a relatively small area (similar to 10 km(2)), they show very large geochemical ...
Perugini, Diego +5 more
core +1 more source
The Neoproterozoic shoshonitic and mildly alkaline bimodal volcanism of Southernmost Brazil is represented by rock assemblages associated to sedimentary successions, deposited in strike-slip basins formed at the post-collisional stages of the Brasilian ...
Sommer Carlos A. +4 more
doaj
Geochemical characterization of Gubanovskaya intrusion of rapakivi granites (Wiborg massif)
The paper presents new data on geology and composition of rapakivi granites of Gubanovskaya intrusion (Wiborg massif). Petrographic and geochemical characteristics of rapakivi granites of the second (ovoid) and third (trachytoid) phases of intrusion, as ...
Rogova I. V. +3 more
doaj +1 more source
High-K calc-alkaline and shoshonite Oligocene colcanics of the Cover Series of the Sesia Zone ccur within a volcano-sedimentary unit located in the internal part of the Sesia Zone in proximity of the Canavese Line.Published1 ...
Medeot, O. +3 more
core +1 more source
Whole-rock Chemistry of Inclusions in the Okueyama Granitic Batholith, Kyushu, SW Japan and Its Origin [PDF]
A lot of inclusions are included in the Okueyama granitic batholith; they are mafic inclusions, mafic double enclaves, xenoliths of gneiss or migmatite and country rocks. The inclusions are enriched in the later-intruded granite to granodiorite.
金丸, 龍夫 +2 more
core +1 more source
A model metasomatized lherzolite composition contains phlogopite and pargasite, together with olivine, orthopyroxene, clinopyroxene and spinel or garnet as subsolidus phases to 3 GPa. Previous works established that at ≥1.5 GPa, phlogopite is stable above the dehydration solidus, determined by the melting behaviour of pargasite and coexisting phases ...
Conceicao, R, Green, David
openaire +2 more sources
Geology, volcanic history and petrology of vulcano (central aeolian archipelago)
Vulcano is an active NW-SE-elongated composite volcano located in the central Aeolian archipelago. Based on available radiometric ages and tephrochronology, the exposed volcanism started at c.
De Astis, G. +18 more
core +1 more source
Lavas of the Quaternary Damavand volcano (Central Alborz, Northern Iran) have been analysed for major and trace elements. The shoshonitic character of this magmatic series is definitively confirmed and most samples correspond to banakites. The Nb, Ta and Ti negative anomalies observed in all lavas suggest that they derive from of a sub-continental ...
Hossein Mehdizadeh +2 more
openaire +1 more source
The active volcano of Ischia, an island off-shore the city of Naples, Southern Italy, has a discontinuous volcanic activity characterized by caldera-forming paroxysmal eruptions, lava flows, and lava domes, and thus offers the opportunity to study the ...
Tommasini, Simone +6 more
core +1 more source
International audienceThe style of volcanism of post-Eocene volcanism in the Alborz zone of northern Iran is different to that of Eocene volcanism (Karaj Formation).
Bardtinzeff, J.M +3 more
core +3 more sources

