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Palaeogeography Palaeoclimatology Palaeoecology 01/2011; 307(1):129-149. · 2.39 Impact Factor
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Gondwana Research 01/2011; 19(3):594-607. · 6.66 Impact Factor
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Geological Society of America Bulletin 01/2010; 122:1463-1479. · 3.79 Impact Factor
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Geosphere 01/2010; 6:225-236. · 2.12 Impact Factor
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EGU General Assembly Conference Abstracts; 01/2010
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ABSTRACT: Geodynamic models for the Antarctic sector of the active Early Palaeozoic Palaeo-Pacific margin of Gondwana are based on the nature and age of the deep crust of the Robertson Bay terrane, the outermost lithotectonic unit of the margin. As this crustal block is covered with thick turbidite deposits, the only way to probe the deep crust is through the analysis of granulite xenoliths from Cenozoic scoria cones. Low-K felsic xenoliths yield the oldest (Middle Cambrian) laser-probe U–Pb ages on zircon areas with igneous growth zoning. This finding, along with the positive whole-rock εNd(500Ma), suggests that these felsic rocks derived from a juvenile magma formed during the Early Palaeozoic Ross orogenic cycle. Mafic xenoliths have geochemical-isotopic compositions similar to those of modern primitive island arcs, suggesting the involvement of subducted oceanic crust in their magma genesis and accretion of juvenile crust at the Antarctic margin of Gondwana.
Terra Nova 04/2009; 21(3):151 - 161. · 2.34 Impact Factor
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ABSTRACT: In eastern Elba Island (Tuscany, Italy), a shallow crustal level felsic, tourmaline-bearing, dyke-sill swarm of Late Miocene age is associated with abundant tourmaline-quartz hydrothermal veins and metasomatic masses. Development of these veins and masses in the host rocks demonstrates multiple hydro-fracturing by magmatic, boron-rich saline fluid. Tourmalines in felsic dykes are schorl, whereas in veins and metasomatic masses, tourmaline composition ranges from schorl-dravite through dravite to uvite. This compositional shift is evidence for an increasing contribution to the magmatic boron-rich fluids by a Mg-Ca-Ti-rich external component represented by biotite-rich and amphibolite host rocks. This system can be envisaged as an exposed proxy of the high temperature hydrothermal system presently active in the deepest part of the Larderello-Travale geothermal field (Tuscany).
Terra Nova 07/2008; 20(4):318 - 326. · 2.34 Impact Factor
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01/2008: pages 131-148;
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01/2007: pages 227-243;
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01/2006: pages 249-258;
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Terra Antartica Reports. 01/2006; 12:73-80.
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SPECIAL PAPERS-GEOLOGICAL SOCIETY OF AMERICA. 01/2005; 388:435.
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01/2004: pages 61-66;
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Lithos 01/2004; 78:101-118. · 3.25 Impact Factor
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01/2004: pages 195-213;
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Atlantic Geology 01/2003; 39:147-162. · 0.54 Impact Factor
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Terra Antartica Reports. 01/2003;
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Geological Magazine 01/2002; 139(3):257-279. · 1.76 Impact Factor
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Geology. 01/2002; 30(11):983-986.
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Journal of Geophysical Research-Part B-Solid Earth. 01/2002; 107(9).