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| 1 | A Temperature--Compensated Rotational Position Sensor Based on Fibre Bragg Gratings 显示文摘 | Montanini R Pirrotta S | 2006 | Sensors and Actuators A : Physical2006，132，2： | 1 |
| 2 | Multi-stage rodingitization of ophiolitic bodies from Northern Apennines(Italy): Constraints from petrography, geochemistry and thermodynamic modelling显示文摘The investigated mantle bodies from the External Ligurians(Groppo di Gorro and Mt.Rocchetta)show evidences of a complex evolution determined by an early high temperature metasomatism,due to percolating melts of asthenospheric origin,and a later metasomatism at relatively high temperature by hydrothermal fluids,with formation of rodingites.At Groppo di Gorro,the serpentinization and chloritization processes obliterated totally the pyroxenite protolith,whereas at Mt.Rocchetta relics of peridotite and pyroxenite protoliths were preserved from serpentinization.The rodingite parageneses consist of diopside+vesuvianite+garnet+calcite+chlorite at Groppo di Gorro and garnet+diopside+serpentine±vesuvianite±prehnite±chlorite±pumpellyite at Mt.Rocchetta.Fluid inclusion measurements show that rodingitization occurred at relatively high temperatures(264-334℃ at 500 bar and 300-380℃ at 1 kbar).Garnet,the first phase of rodingite to form,consists of abundant hydrogarnet component at Groppo di Gorro,whereas it is mainly composed of grossular and andradite at Mt.Rocchetta.The last stage of rodingitization is characterized by the vesuvianite formation.Hydrogarnet nucleation requires high Ca and low silica fluids,whereas the formation of vesuvianite does not need CO2-poor fluids.The formation of calcite at Groppo di Gorro points to mildly oxidizing conditions compatible with hydrothermal fluids;the presence of andradite associated with serpentine and magnetite at Mt.Rocchetta suggests Fe^3+-bearing fluids with fO2 slightly higher than iron-magnetite buffer.We propose that the formation of the studied rodingite could be related to different pulses of hydrothermal fluids mainly occurring in an oceancontinent transitional setting and,locally,in an accretionary prism associated with intra-oceanic subduction. | Emma Salvioli-Mariani Tiziano Boschetti Lorenzo Toscani Alessandra Montanini Jasmine Rita Petriglieri Danilo Bersani | 2020 | Geoscience Frontiers2020，11，6： | 1 |
| 3 | Aluminum foam sandwiches collapse modes under static and dynamic three-point bending 显示文摘 | Crupi V Montanini R | 2007 | International Journal of Impact Engineering2007，34，3： | 1 |
| 4 | Sr,Nd,Pb and trace element systematics of the New Caledonia harzburgites:Tracking source depletion and contamination processes in a SSZ setting显示文摘The New Caledonia ophiolite(Peridotite Nappe)consists primarily of harzburgites,locally overlain by mafic-ultramafic cumulates,and minor spinel and plagioclase lherzolites.In this study,a comprehensive geochemical data set(major and trace element,Sr-Nd-Pb isotopes)has been obtained on a new set of fresh harzburgites in order to track the processes recorded by this mantle section and its evolution.The studied harzburgites are low-strain tectonites showing porphyroclastic textures,locally grading into protomylonitic textures.They exhibit a refractory nature,as attested by the notable absence of primary clinopyroxene,very high Fo content of olivine(91-93 mol.%),high Mg#of orthopyroxene(0.91-0.93)and high Cr#of spinel(0.44-0.71).The harzburgites are characterised by remarkably low REE concentrations(<0.1 chondritic values)and display'U-shaped'profiles,with steeply sloping HREE(DyN/YbN=0.07-0.16)and fractionated LREE-MREE segments(LaN/SmN=2.1-8.3),in the range of modern fore-arc peridotites.Geochemical modelling shows that the HREE composition of the harzburgites can be reproduced by multi-stage melting including a first phase of melt depletion in dry conditions(15%fractional melting),followed by hydrous melting in a subduction zone setting(up to 15%-18%).However,melting models fail to explain the enrichments observed for some FME(i.e.Ba,Sr,Pb),LREE-MREE and Zr-Hf.These enrichments,coupled with the frequent occurrence of thin,undeformed films of Al2 O3,and CaO-poor orthopyroxene(Al2O3=0.88-1.53 wt.%,CaO=0.31-0.56 wt.%)and clinopyroxene with low Na2 O(0.03-0.16 wt.%),Al2 O3(0.66-1.35 wt.%)and TiO2(0.04-0.10 wt.%)contents,point to FME addition during fluid-assisted melting followed by late stage metasomatism most likely operated by subductionrelated melts with a depleted trace element signature.Nd isotopic ratios range from unradiogenic to radiogenic(-0.80<εNdi≤+13.32)and negatively correlate with Sr isotopes(0.70257≤87Sr/86Sr≤0.70770).Pb isotopes cover a wide range,trending from DMM toward enriched,sediment-like,compositions.We interpret the geochemical signature displayed by the New Caledonia harzburgites as reflecting the evolution of a highly depleted fore-arc mantle wedge variably modified by different fluid and melt inputs during Eocene subduction. | Arianna Secchiari Alessandra Montanini Delphine Bosch Patrizia Macera Dominique Cluzel | 2020 | Geoscience Frontiers2020，11，1： | 1 |
| 5 | Phylogenetic and functional analysis of the Cation Diffusion Facilitator (CDF) family: improved signature and prediction of substrate specificity 显示文摘 | MONTANINI B BLAUDEZ D JEANDROZ S | 2007 | BMC Genomics2007，8，： | 1 |
| 6 | A secretory pathway-localized cation diffusion facilitator confers plant manganese tolerance 显示文摘 | PEITER E MONTANINI B GOBERT A | 2007 | PLANT BIOLOGY2007，104，20： | 1 |
| 7 | MicroRNA cloning and se- quencing in osteosarcoma cell lines: differential role of miR-93 显示文摘 | Montanini L Lasagna L Barili V | 2012 | Cell Oncol( Dordr)2012，35，1： | 1 |
| 8 | Aluminium foam sandwiches collapse modes under static and dynamic three-point bending显示文摘 | CRUPI V Montanini R | | 0，，03： | 1 |
| 9 | Petrology and geochemistry of ultrapotassic rocks from the Montefiascone volcanic complex (central Italy): Magmatic evolution and petrogenesis显示文摘 | Battistini G D Montanini A Vemia L Bargossi G M Castorina F | 1998 | Lithos1998，43，3： | 1 |
| 10 | Aluminium foam sandwiches collapse modes under static and dynamic three-point bending显示文摘 | CRUPI V MONTANINI R | 2007 | International Journal of Impact Engineering2007，34，： | 1 |
| 11 | The expanded family of ammonium transporters in the perennial poplar plant 显示文摘 | Couturier J Montanini B Martin F | 2007 | New Phytol2007，174，1： | 1 |
| 12 | The expanded family of ammonium transporters in the perennial poplar plant显示文摘 | Couturier J Montanini B Martin F | 2007 | New Phytologist2007，，： | 1 |
| 13 | Phylo- genetic and function analysis of the cation diffusion facilitator (CDF) family: improved signature and prediction of substrate specificity显示文摘 | MONTANINI B BLAUDEZ D JEANDROZ S | 2007 | BMC Genomics2007，8，2： | 1 |
| 14 | Aluminium Foam Sandwiches colapse modes under static and dynamic three-point bending 显示文摘 | Crupi V Montanini R | 2007 | Impact Engineering2007，34，3： | 1 |
| 15 | A secretory pathway-localized cation diffusion facilitator confers plant manganesetolerance显示文摘 | Peiter E Montanini B Gobert A | 2007 | Proc Natl Acad Sci USA2007，104，20： | 1 |
| 16 | MicroRNA cloning and sequencing in osteosarcoma cell lines:differential role of miR-93显示文摘 | MONTANINI L LASAGNA L BARILI V | 2012 | Cell Oncol(Dordr)2012，35，： | 1 |
| 17 | Aluminum foam sandwiches collapse modes under static and dynamic three-point bending显示文摘 | CRUPI V MONTANINI R | 2007 | International Journal of Impact Engineering2007，34，3： | 1 |
| 18 | Epilepsy in multipie sclerosis显示文摘 | Montanini R Basso PF | 1990 | European Neurology1990，30，： | 1 |
| 19 | Genome-wide search and functional identif-ication of transcription factors in the mycorrhizal fungus Tubermelanosporum显示文摘 | Montanini B Levati E Bolchi A Kohler A Morin E TisserantE Martin F | 2011 | New Phytol2011，189，3： | 1 |
| 20 | Measurement of Strain Rate Sensitivity of Aluminium Foams for Energy Dissipation显示文摘 | Roberto Montanini | 2005 | International Journal of Mechanical Sciences2005，47，： | 1 |
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