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Sr,Nd,Pb and trace element systematics of the New Caledonia harzburgites:Tracking source depletion and contamination processes in a SSZ setting

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Geoscience Frontiers 2020年第1期11卷 37-55页

作者： Arianna Secchiari Alessandra Montanini Delphine Bosch Patrizia Macera dominique cluzel Dipartimento di Scienze Chimiche della Vita e della SostenibilitàAmbientaleUniversitàdi ParmaItaly Geosciences Montpellier Universitéde MontpellierFrance Dipartimento di Scienze della Terra Universitàdi PisaItaly Institut des Sciences Exactes et Appliquées Universitéde la Nouvelle-CalédonieNew Caledonia

The New Caledonia ophiolite(Peridotite Nappe)consists primarily of harzburgites,locally overlain by mafic-ultramafic cumulates,and minor spinel and plagioclase *** 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 *** studied harzburgites are low-strain tectonites showing porphyroclastic textures,locally grading into protomylonitic *** 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 *** 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(***,Sr,Pb),LREE-MREE and *** 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 *** 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,trendi

关键词： Intra-oceanic arcs Depleted mantle sections Fore-ac harzburgites New Caledonia ophiolite Sr-Nd-Pb isotopes Subduction zones

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Toward a unified model of Altaids geodynamics:Insight from the Palaeozoic polycyclic evolution of West Junggar(NW China)

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Science China Earth Sciences 2016年第1期59卷 25-57页

作者： Flavien CHOULET Michel FAURE dominique cluzel CHEN Yan LIN Wei WANG Bo XU Bei UMR6249 Chrono-EnvironnementCNRS/Universite de Bourgogne Franche-ComteBesangonFrance UMR 7327 Institut des Sciences de la Terre d'OrleansBRGM/CNRS/Universite d'OrleansOrleansFrance POle Pluridisciplinaire de la Matiere et de l'Environnement Universite de la Nouvelle CaledonieNoumeaFrance Institute of Geology and Geophysics Chinese Academy of SciencesBeijing 100029China Department of Earth Science University of NanjingNanjing 210093China Key Laboratory of Orogenic Belts and Crustal Evolution Peking UniversityBeijing 100871China

The Altaid tectonic collage extends over Central Asia, exposing numerous accretionary orogens that can account for the Palaeozoic continental crust growth. A pluridisciplinary approach, using geochronological, geochemical, structural and palaeomagnetic tools was carried out to unravel the architecture and the evolution of West Junggar(Northwestern China), a segment of the Altaid Collage. A polycyclic geodynamic evolution is inferred and includes:(1) an Early Palaeozoic cycle, characterized by the closure of two oceanic basins bounded by island-arc systems;(2) an Early Devonian subduction jamming resulting in a minor-scale collision documented by thrusting, syntectonic sedimentation and subsequent crutal thinning associated with alkaline magmatism;(3) a Late Palaeozoic cycle, driven by the evolution of two opposite subduction zones developed upon the Early Palaeozoic basement. Detailed structural analysis and paleomagnetic data provide constraints for the late evolution of Junggar in the frame of the development of the Late Palaeozoic Kazakh orocline, which led to oblique subduction and transpression in the West Junggar accretionary complex. Progressive buckling of the Kazakh orocline further resulted in Late Carboniferous to Permian wrench tectonics, and lateral displacement of lithotectonic units. Block rotations that continued after the Late Triassic are due to diachronous intraplate reactivation. This scenario mirrors the Palaeozoic geodynamics of the Altaid Collage. Multiple Early Palaeozoic collisions of intra-oceanic arcs and micro continents have contributed to the formation of the Kazakhstan Microcontinent. Since the Late Palaeozoic, subductions formed around this microcontinent and the final oblique closure of oceanic domains resulted in the transcurrent collage of Tarim and Siberia cratons. Palaeozoic strike-slip faults were later reactivated during Mesozoic intracontinental tectonics.

关键词：早古生代西准噶尔演化过程多旋回动力学模型西北洞察力哈萨克斯坦

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New Caledonia Ophiolite, Marginal Rifting to Fore-arc Evolution

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Acta Geologica Sinica(English Edition) 2020年第S1期94卷 9-10页

作者： dominique cluzel Jonathan AITCHISON Arianna SECCHIARI Alessandra MONTANINI Delphine BOSCH Universitéde la Nouvelle-Calédonie NouméaNew Caledonia School of Earth and Environmental Sciences University of Queensland QLD 4072Australia University of Parma Parco Area delle Scienze 157/a 43124 ParmaItaly Earth Sciences Department Géosciences Montpellier UMR-CNRS 5243-Univ.Montpellier II France

The New Caledonia Ophiolite(Peridotite Nappe), represents about one third of the island’s surface(i.e. 5 500 km2). The ophiolite is composed of harzburgites, dunites, lherzolites, minor mafic-ultramafic cumulates, and various dykes and sills. The mantle section underwent a polyphase evolution, which involved prominent depletion and re-fertilization. The oldest events are probably recorded by abyssal-type lherzolites of the northern massifs, which bear traces of moderate partial melting. Plagioclase lherzolites were formed by shallow entrapment of highly depleted MORB melt in residual spinel lherzolites. Nd isotope compositions are consistent with derivation from an asthenospheric mantle source that experienced a recent MORB-producing depletion. This evolution was most likely accomplished during the late Cretaceous breakup of the eastern Australian margin. The harzburgite-dunite association, which forms the bulk of Peridotite Nappe was probably formed through a multistage magma-producing process. Harzburgites composition may have be obtained by a first phase of ~15% dry fractional melting, followed by 15%–18% hydrous melting in a supra-subduction zone setting. Variable εNd negatively correlate with 87Sr/86Sr, while Pb isotopes cover a wide range, trending from depleted mantle towards enriched, sediment-like, compositions. Such signatures likely reflect the evolution of a highly depleted forearc mantle wedge variably modified by different fluid and melt inputs during Eocene subduction. The harzburgite-dunite set is overlain by a dunite transition zone ~300 m thick, in turn discontinuously covered by cumulate lenses consisting of layered pyroxenites, dunites, and wherlites at the base and gabbronorites/websterites on top. The mafic cumulates crystallized from primitive, ultra-depleted melts in the nascent lower fore-arc crust. In particular, FME enrichments and Nd-Pb isotopes support an origin from a refractory mantle source modified by slab fluids for the gabbronorite

关键词： ophiolite supra-subduction slab fluids metasomatism

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Palaeozoic tectonic evolution of the Tianshan belt,NW China

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Science China Earth Sciences 2011年第2期54卷 166-184页

作者： Jacques CHARVET SHU LiangShu Sebastien LAURENT-CHARVET WANG Bo Michel FAURE dominique cluzel CHEN Yan Koen De JONG ISTO Universite d'Orleans B.P. 6759 45067 Orleans Cedex 2 France State Key Laboratory for Mineral Deposits Research School of Earth Sciences and Engineering Nanjing University Nanjing 210093 China Institut Polytechnique LaSalle Beauvais Departement Geosciences BP 30313 60026 Beauvais Cedex France PPME Universite de la Nouvelle Caledonie Noumea New Caledonia School of Earth and Environmental Sciences College of Natural Sciences Seoul National University Seoul 151-747 Korea

The Chinese Tianshan belt is a major part of the southern Central Asian Orogenic Belt,extending westward to Kyrgyzstan and *** Paleozoic tectonic evolution,crucial for understanding the amalgamation of Central Asia,comprises two stages of *** first collisional stage built the Eo-Tianshan Mountains,before a Visean unconformity,in which all structures are verging *** implied a southward subduction of the Central Tianshan Ocean beneath the Tarim active margin,that induced the Ordovician-Early Devonian Central Tianshan arc,to the south of which the South Tianshan back-arc basin *** the Late Devonian,the closure of this ocean led to a collision between Central Tianshan arc and the Kazakhstan-Yili-North Tianshan Block,and subsequently closure of the South Tianhan back-arc basin,producing two suture zones,namely the Central Tianshan and South Tianshan suture zones where ophiolitic mélanges and HP metamorphic rocks were emplaced *** second stage included the Late Devonian-Carboniferous southward subduction of North Tianshan Ocean beneath the Eo-Tianshan active margin,underlined by the Yili-North Tianshan arc,leading to the collision between the Kazakhstan-Yili-NTS plate and an inferred Junggar Block at Late Carboniferous-Early Permian *** North Tianshan Suture Zone underlines likely the last oceanic closure of Central Asia Orogenic Belt;all the oceanic domains were consumed before the Middle *** amalgamated units were affected by a Permian major wrenching,dextral in the *** correlation with the Kazakh and Kyrgyz Tianshan is *** Kyrgyz South Tianshan is equivalent to the whole part of Chinese Tianshan(CTS and STS) located to the south of Narat Fault and Main Tianshan Shear Zone;the so-called Middle Tianshan thins out toward the *** South Tianshan Suture of Kyrgyzstan correlates with the Central Tianshan Suture of Chinese *** evolution of this southern domain remains similar

关键词：中天山构造演化古生代中国吉尔吉斯斯坦哈萨克斯坦中亚造山带塔里木地块

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伊犁北部博罗霍努岩体年代学和地球化学研究及其大地构造意义

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岩石学报 2007年第8期23卷 1885-1900页

作者：王博舒良树 dominique cluzel Michel FAURE Jacques CHARVET 南京大学地球科学系南京210093 法国奥尔良大学地球科学研究所法国奥尔良45067

博罗霍努岩体是发育在新疆伊犁北部的一个大型海西期花岗岩体,总体沿近 SE—NW 向分布,出露面积逾2000km^2。该岩体主要包括三类花岗岩:灰黑色辉石闪长岩、浅色黑云母花岗岩和紫红色黑云母钾长花岗岩。锆石 U—Pb La-ICP-MS 定年表明,... 详细信息

博罗霍努岩体是发育在新疆伊犁北部的一个大型海西期花岗岩体,总体沿近 SE—NW 向分布,出露面积逾2000km^2。该岩体主要包括三类花岗岩:灰黑色辉石闪长岩、浅色黑云母花岗岩和紫红色黑云母钾长花岗岩。锆石 U—Pb La-ICP-MS 定年表明,辉石闪长岩的年龄为301±7Ma,黑云母花岗岩的年龄范围为294±7～285±7Ma,而黑云母钾长花岗岩则形成于280±5～266±6Ma。岩石地球化学分析显示,黑云母花岗岩和钾长花岗岩以准铝或弱过铝Ⅰ型花岗岩为主,个别属于弱过铝 S 型花岗岩。在微量元素方面,这些花岗岩均富集轻稀土而亏损重稀土,但来自两个剖面的花岗岩具有不同的稀土元素配分模式,可能代表它们的岩浆源区有所不同,因此需要进一步对这些花岗岩进行同位素地质学研究。相对于洋脊花岗岩而言,博罗霍努岩体的花岗岩明显富集 K,Rb,Ba 和 Th,同时,显著亏损 Nb,Ta,Y 和 Yh。以上地球化学特征及微量元素判别图表明,这些花岗岩类形成于俯冲有关的火山岛弧环境。结合伊犁及邻区岩浆岩的特征及其时代,可以认为博罗霍努岩体的形成与天山北部洋壳向南的俯冲造山作用有关。西天山北部俯冲造山作用最终在中二叠世结束,并在中一晚二叠世进入陆内造山和伸展拉张阶段。

关键词：天山伊犁海西期花岗岩锆石U-Pb定年微量元素地球化学

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科克苏-穹库什太古生代构造-岩浆作用及其对西南天山造山时代的约束

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岩石学报 2007年第6期23卷 1354-1368页

作者：王博舒良树 MichelFAURE dominiquecluzel JacquesCHARVET Michel FAURE dominique cluzel Jacques CHARVET 南京大学地球科学系南京210093 法国奥尔良大学地球科学研究所

天山造山带是古生代多期碰撞增生作用的产物,其确切的造山时代是当前争议较多的热点问题。分布在西南天山的科克苏-穹库什太剖面经历了复杂的构造变形,最明显的两期变形事件分别为朝北的推覆作用和 NE-SW 韧性走滑作用。本剖面可分为伊... 详细信息

天山造山带是古生代多期碰撞增生作用的产物,其确切的造山时代是当前争议较多的热点问题。分布在西南天山的科克苏-穹库什太剖面经历了复杂的构造变形,最明显的两期变形事件分别为朝北的推覆作用和 NE-SW 韧性走滑作用。本剖面可分为伊犁岩浆岛弧、伊犁结晶基底、高压变质杂岩三个岩石-构造单元。野外可见黑云母花岗闪长岩侵入到绿片岩相变质岩中,岩脉切穿绿片岩中面理构造。通过锆石 U-Pb LA-ICPMS 测年,科克苏剖面钾长花岗岩的年龄为341±6Ma 和338±8Ma,穹库什太黑云母花岗闪长岩的年龄为313±4Ma。其中,花岗闪长岩发生了黑云母定向排列,通过对黑云母进行^(40)Ar/^(39)Ar 测年,获得坪年龄为263.4±0.6Ma,表明该花岗闪长岩受过后期热事件的干扰。地球化学分析表明,黑云母花岗闪长岩属于钙碱性系列,Nb 和 Ta 含量低而 Rb,Ba 和 Th 含量很高,与俯冲作用有关的岛弧岩浆岩地球化学组成非常相似。结合前人对该地区高压变质岩、花岗岩和火山岩的研究成果,本文提出,西南天山俯冲-碰撞造山作用发生在晚石炭世之前,研究区后碰撞区域走滑作用标志着西南天山碰撞造山作用在二叠纪之前全部结束。

关键词：天山造山带花岗岩古生代锆石U-Pb定年 40Ar/39Ar定年地球化学

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Going straight for the gut:gut-brain axis pathology and treatment of Parkinson's disease

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Neural Regeneration Research 2024年第10期19卷 2111-2112页

作者： dominique Ebedes Cesar V.Borlongan University of South Florida Morsani College of Medicine TampaFLUSA Center of Excellence for Aging and Brain Repair Department of Neurosurgery and Brain RepairUniversity of South Florida Morsani College of MedicineTampaFLUSA

This perspective focuses on the recent literature regarding the role of the gut-brain axis(GBA) in fecal microbiota transplantation(FMT) and stem cell therapy(SCT) in Parkinson's disease(PD).PD is the second most common neurodegenerative disease in the United States,yet therapies remain *** research suggests that the GBA may play a role in the pathogenesis of *** FMT as well as SCT offer promising new avenues for PD *** bing the interactions between FMT and SCT with the GBA may reveal novel therapeutics for PD.

关键词： straight pathology pathogenesis

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Numerical study of convective heat transfer in static arrangements of particles with arbitrary shapes:A monolithic hybrid lattice Boltzmann-finite difference-phase field solver

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Particuology 2024年第2期85卷 186-197页

作者： Reza Namdar Mohammadhassan Khodsiani Hesameddin Safari Tanya Neeraj Seyed Ali Hosseini Frank Beyrau Benoit Fond dominique Thevenin Fathollah Varnik Interdisciplinary Centre for Advanced Materials Simulation(ICAMS) Ruhr-University BochumBochum44801Germany Laboratory of Technical Thermodynamics University of Magdeburg"Otto von Guericke"Magdeburg39106Germany Laboratory of Fluid Dynamics and Technical Flows University of Magdeburg"Otto von Guericke"MagdeburgD-39106Germany Department of Mechanical and Process Engineering ETH ZurichZurich8092Switzerland ONERA The French Aerospace Lab Department of AerodynamicsAeroelasticity and Acoustics(DAAA)Paris-Saclay UniversityMeudon92190France

A compressible lattice Boltzmann-finite difference method is extended by the phase-field approach into a monolithic scheme to study fluid flow and heat transfer through regular arrangements of solid bodies of circular,elliptical and irregular *** advantage of using the phase-field method is demon-strated both in its simplicity of accounting for flow and thermal boundary conditions at solid surfaces with irregular shapes and in the capability of generating such complex-shaped *** an array of discs,numerical results for the overall solid-to-gas heat transfer rate are validated via experiments on flow through arrays of hot *** thus validated compressible LB-FD-PF hybrid scheme is used to study the dependence of heat transfer on flow and thermal boundary conditions(Reynolds number,temperature difference between the hot solid bodies and the inlet gas),porosity as well as on the shape of solid *** are rationalized in terms of the residence time of the gas close to the solid body and downstream variations of gas velocity and *** for further applications of the proposed methodology are also discussed.

关键词： Lattice Boltzmann method Finite difference scheme Convective heat transfer Diffuse interface Thermal compressible flow

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Health Systems Strengthening to Tackle the Global Burden of Pediatric and Congenital Heart Disease: A Diagonal Approach

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Congenital Heart Disease 2024年第2期19卷 131-138页

作者： dominique Vervoort Amy Verstappen Sreehari Madhavankutty Nair Chong Chin Eu Bistra Zheleva Institute of Health Policy Management and EvaluationUniversity of TorontoTorontoCanada Division of Cardiac Surgery University of TorontoTorontoCanada Global Alliance for Rheumatic and Congenital Hearts PhiladelphiaUSA Department of Health Services Government of KeralaKeralaIndia Ministry of Health PutrajayaMalaysia Children’s HeartLink MinneapolisUSA

1 Background Congenital heart disease(CHD)is the most common major congenital anomaly,affecting approximately one in every 100 live births[1].Among congenital anomalies,66%of preventable deaths are due to CHD,and 58%of the avertable morbidity and mortality due to congenital anomalies would result from scaling congenital heart surgery services[2].Every year,nearly 300,000 children and adults die from CHD,the majority of whom live in low-and middle-income countries(LMICs)[3].Approximately 49%of all individuals with CHD will require surgical or interventional care at some point in their lifetime[4];as a result of advances in access to and the delivery of such services,over 95%of children born with CHD in high-income countries now live into adulthood[3].Here,adults have surpassed children in the number of CHD cases at a ratio of 2:1[5].

关键词： Congenital heart disease pediatric heart disease global health health systems health policy

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Protein-S-100-beta is increased in patients with decompensated cirrhosis admitted to ICU

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Journal of Intensive Medicine 2024年第2期4卷 222-230页

作者： Nicolas Weiss Simona Tripon Maxime Mallet Françoise Imbert-Bismut Mehdi Sakka dominique Bonnefont-Rousselot Philippe Sultanik Sarah Mouri Marika Rudler dominique Thabut Sorbonne Université AP-HP.Sorbonne UniversitéHôpital de la Pitié-SalpêtrièreDépartement de NeurologieUnitéde Médecine Intensive RéanimationàOrientation NeurologiqueParisFrance Brain Liver Pitié-Salpêtrière(BLIPS)Study Group INSERM UMR_S 938Centre de recherche Saint-AntoineMaladies métaboliquesBiliaires et Fibro-Inflammatoire du FoieInstitute of Cardiometabolism and Nutrition(ICAN)ParisFrance Groupe de Recherche Clinique en REanimation et Soins intensifs du Patient en Insuffisance Respiratoire aiguE(GRC-RESPIRE)Sorbonne Université ParisFrance Assistance Publique-Hôpitaux de Paris AP-HP.Sorbonne UniversitéHôpital de la Pitié-SalpêtrièreService d'hépato-GastroentérologieUnitéde Soins Intensifs d'HépatologieParisFrance Assistance Publique-Hôpitaux de Paris AP-HP.Sorbonne UniversitéService de Biochimie MétaboliqueHôpitaux Universitaires Pitié-Salpêtrière-Charles FoixDMU BioGeMParis F-75013France UniversitéParis Cité UFR de PharmacieCNRSInsermUTCBSParisFrance

Background Hepatic encephalopathy(HE)is highly prevalent in patients with liver *** pathophysiology of HE is centered on the synergic role of hyperammonemia and systemic ***,some data suggest altered functioning of the blood–brain barrier(BBB).Assessing BBB function is challenging in clinical practice and at the ***-S-100 Beta(PS100-Beta)could be a useful peripheral marker of BBB permeability in *** study aimed to assess plasmatic PS100-Beta levels in a prospective cohort of patients admitted to the intensive care unit(ICU)with decompensated cirrhosis with and without overt *** We retrospectively evaluated a prospective cohort of cirrhotic patients admitted to the ICU from October 2013 to September 2015 that had an available plasmatic PS100-Beta *** with previous neurological impairment or limitation of intensive or resuscitative measures were *** HE was defined as West-Haven grades 2 to *** patients were compared to a control cohort of outpatient clinic cirrhotic and non-cirrhotic patients explored for isolated elevation of liver *** ICU discharge,the patients were followed for at least 3 months for the occurrence of overt *** outcomes(liver transplantation or death)were *** ability of PS100-Beta–in combination with other factors–to predict overt HE was evaluated in a multivariate analysis using logistic *** ratios were used to determine the effects and calculate odds ratios(OR).Survival analysis was performed by using the Kaplan–Meier method and survival between groups was compared using a Log-rank *** A total of 194 ICU patients and 207 outpatients were included in the *** levels of plasmatic PS100-Beta were detected in the ICU decompensated cirrhotic patients compared with the outpatients([0.15±0.01]mg/L vs.[0.08±0]mg/L,P<0.001).ICU patients with overt HE had higher levels of PS100-Beta([0.19±0.03]mg/L)compared with the

关键词： Cirrhosis Hepatic encephalopathy Blood-brain barrier PS100-Beta Liver disease

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