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		题名	作者	年代	出处	被引量
	1	Platinum-group elements as petrological indications in mafic-ultramafic complexes of the central and southern Urals:preliminary results显示文摘	Garuti G Fershtater G Bea F Montero P Pushkarev E V Zaccarini F		0，，：	1
	2	Phtinum-group element mineralogy and geochemistry of chromitite of the Khichevskoy ophiolite complex, central Urals 显示文摘	Zaccarini F Pushkarev E Garuti G	2008	Ore Geology P eviews2008，33，：	1
	3	Platinum-group elements as petrological indicators in mafic-ultramafic complexs of the central and southern U rals: Preliminary results显示文摘	Fershtater G Bea F Montero P Pushkarev E V Zaccarini F	1997	Tectonophysics1997，276，：	1
	4	Chromite Composition and Platinum-group Mineral Assemblage in the Uktus Alaskan-type Complex (Central Urals, Russia) 显示文摘	Garuti G Pushkarev E V Zaccarini F	2003	Mineralium Deposita2003，38，：	1
	5	Marked inhibition of retinal neovascularization in rats following soluble-flt-1 gene transfer显示文摘	Rota R Riccioni T Zaccarini M	2004	J Gene Med2004，6，9：	1
	6	Marked inhibition of retinal neovascularization in rats following soluble-flt-1 gene transfer显示文摘	Rota R Riccioni T Zaccarini M	2004	J Gene Med2004，6，9：	1
	7	Paragenesis and composition of laurite from chromitite of othrys (Greece) :implications for Os-Ru fractionation in ophiolitic upper mantle of the Balkan Peninsula 显示文摘	Garuti G Zaccarini F Economou-Eliopoulos M	1999	Mineralium Deposita1999，34，：	1
	8	Deformation history and processes during accretion of seamounts in subduction zones:The example of the Durkan Complex(Makran,SE Iran)显示文摘The Durkan Complex is a tectonic element of the Makran Accretionary Prism(SE Iran)that includes fragments of Late Cretaceous seamounts.In this paper,the results of map-to micro-scale structural studies of the western Durkan Complex are presented with the aim to describe its structural and tectonometamorphic evolution.The Durkan Complex consists of several tectonic units bordered by mainly NNW-striking thrusts.Three main deformation phases(D_(1),D_(2),and D_(3))are distinguished and likely occurred from the Late Cretaceous to the Miocene–Pliocene.D_(1) is characterized by sub-isoclinal to close and W-verging folds associated with an axial plane foliation and shear zone along the fold limbs.This phase records the accretion of fragments of the seamount within the Makran at blueschist facies metamorphic conditions(160–300℃ and 0.6–1.2 GPa).D_(2) is characterized by open to close folds with subhorizontal axial plane that likely developed during the exhumation of previously accreted seamount fragments.An upper Paleocene–Eocene siliciclastic succession unconformably sealed the D_(1) and D_(2) structures and is,in turn,deformed by W-verging thrust faults typical of D_(3).The latter likely testifies for a Miocene–Pliocene tectonic reworking of the accreted seamount fragments with the activation of out of sequence thrusts.Our results shed light on the mechanism of accretion of seamount materials in the accretionary prisms,suggesting that seamount slope successions favour the localization and propagation of the basal décollement.This study further confirms that the physiography of the subducting plates plays a significant role in the tectonic evolution of the subduction complexes.	Edoardo Barbero Maria Di Rosa Luca Pandolfi Morteza Delavari Asghar Dolati Federica Zaccarini Emilio Saccani Michele Marroni	2023	Geoscience Frontiers2023，14，2：	0

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