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305篇 您的检索式:作者名="Farr S"
    题名 作者 年代 出处 被引量
1Degradation of Some Biorecalcitrant Pesticides by Homogeneous and Heterogeneous Photocatalytic Ozonation显示文摘FARRE M J FRANCH M I MALATO S 2005Chemosphere2005,58,:1
2Ni- tric oxide synthase inhibition and food intake effects on motivation to eat and in female mice 显示文摘MORLEY J E FARR S A SUAREZ M D 1995Pharma- cology Biochemistry and Behavior1995,50,3:1
3High value products from transgenic maize显示文摘NAQVI S RAMESSAR K FARRE G 2011Biotechnology Advances2011,29,1:1
4Pesticide toxicity assessment using an electrochemical biosensor with Pseudomonas putida and a bioluminescence inhibition assay with Vibrio fischeri显示文摘 Goncalves C Lacorte S 2002Anal Bioanal Chem2002,373,:1
5K-ras codon 12 mutation induces higher level of resistance to apoptosis and predisposition to anchorage-independent growth than codon 13 mutation or proto-oncogene overexpression显示文摘Guerrero S Casanoval I Farre L 2000Cancer Res2000,60,23:1
6Ghrelin controls hippocampal spine synapse density and memory performance 显示文摘Diano S Farr SA Benoit SC 2006Nat Neurosci2006,9,3:1
7Bioanalytical and chemical assessment of the disinfection by-product formation potential: Role of organic matter 显示文摘Farre M J Day S Neale P A 2013Water Research2013,47,:1
8Effect of alpha-lipoic acid on memory,oxidation,and lifespan in SAMP8 mice 显示文摘ERCAL N FARR S A PRICE T O 2012J Alzheimers Dis2012,32,2:1
9An integrative model of updating and performance 显示文摘Kozlowski S W J Farr J L 1988Human Performance1988,1,1:1
10The use of crystal orientation in mapping the electrodeposition of cobalt and copper 显示文摘EAGLETON S FARR J ASHWORTHA 2000Transaction of the Institute of Metal Finishing2000,78,2:1
11Antibodies to carbonic anhydrase and IgG4 levels in idiopathic chronic pancreatitis:relevance for diagnosis of autoimmune pancreatitis显示文摘APARISI L FARRE A GOMEZ-CAMBRONERO L et s 2005Gut2005,54,5:1
12Adsorption of sulphonates from detergent mixtures on potassium kaolinite显示文摘House W A Farr I S 1989Colloids and Surface1989,,40:1
13Bacterial defenses against oxidative stress 显示文摘Storz G Tartaglia L A Farr S B 1990Trends in Genetics1990,6,:1
14Fate and toxicity of emerging pollutants, their metabolites and transformation products in the aquatic environment 显示文摘FARRE M L PEREZ S KANTIANI L 2008TrAC Trends in Analytical Chemistry2008,27,11:1
15Spinal CT angiography:study of stenosis and calcification at the origin of the vetebral artery显示文摘 Magometschnig H Trattnig S 1996Neuroradiology1996,38,:1
16Ghrelin controls hippocampal spine synapse density and memory performance 显示文摘Diano S Farr SA Benoit SC 2006Nature Meuroscience2006,9,3:1
17Oxidative stress responses in Esche richia coli and Salmonella typhimurium 显示文摘Farr S B Kogoma T 1991Microbio- logical Reviews1991,55,4:1
18Use of magnetic resonance imaging to predict outcome after stroke: a review of experimental and clinical evidence显示文摘Farr TD Wegener S 2010Cereb Blood Flow Metab2010,,4:1
19Molybdate in corrosion inhibition - A review 显示文摘Vukassovich M S Farr J P G 1986Materials Performance1986,25,5:1
20Ophiolite hosted chromitite formed by supra-subduction zone peridotite–plume interaction显示文摘Chromitite bodies hosted in peridotites typical of suboceanic mantle(s.l.ophiolitic)are found in the northern and central part of the Loma Caribe peridotite,in the Cordillera Central of the Dominican Republic.These chromitites are massive pods of small size(less than a few meters across)and veins that intrude both dunite and harzburgite.Compositionally,they are high-Cr chromitites[Cr#=Cr/(Cr+Al)atomic ratio=0.71-0.83]singularly enriched in TiO2(up to 1.25 wt.%),Fe2 O3(2.77-9.16 wt.%)as well as some trace elements(Ga,V,Co,Mn,and Zn)and PGE(up to 4548 ppb in whole-rock).This geochemical signature is unknown for chromitites hosted in oceanic upper mantle but akin to those chromites crystallized from mantle plume derived melts.Noteworthy,the melt estimated to be in equilibrium with such chromite from the Loma Caribe chromitites is similar to basalts derived from different source regions of a heterogeneous Caribbean mantle plume.This mantle plume is responsible for the formation of the Caribbean Large Igneous Province(CLIP).Dolerite dykes with back-arc basin basalt(BABB)and enriched mid-ocean ridge basalt(E-MORB)affinities commonly intrude the Loma Caribe peridotite,and are interpreted as evidence of the impact that the Caribbean plume had in the off-axis magmatism of the back-arc basin,developed after the Caribbean island-arc extension in the Late Cretaceous.We propose a model in which chromitites were formed in the shallow portion of the back-arc mantle as a result of the metasomatic reaction between the supra-subduction zone(SSZ)peridotites and upwelling plume-related melts.Júlia Farré-de-Pablo Joaquín A.Proenza JoséMaría González-Jiménez Thomas Aiglsperger Antonio Garcia-Casco Javier Escuder-Viruete Vanessa Colás Francisco Longo 2020Geoscience Frontiers2020,11,6:1
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