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Redox Evolution of the Lithospheric Mantle beneath the North China Craton

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Acta Geologica Sinica(English Edition) 2016年第4期90卷 1539-1540页

作者： WANG Jian SONG Yue keiko hattori College of Earth Sciences Jilin University Department of Earth Sciences University of Ottawa

Objective The North China Craton （NCC） is a large Archean craton with a long geological history, yet very few studies have been carried out on the evolution of the redox conditions of its underlying mantle. Oxidation state of the mantle is critical in controlling the formation of metallic mineral deposits because metals can be readily released from the mantle to partial melt under oxidized conditions. In contrast, highly reduced and stable conditions are essential for the crystallization of diamond. The subcontinental lithospheric mantle （SCLM） beneath major cratons in the world has been stable since their formation and highly reduced in its oxidation state, but the SCLM below the NCC is different.

关键词： NCC Redox Evolution of the Lithospheric Mantle beneath the North China Craton

In situ characterization of forearc serpentinized peridotite from the Sulu ultrahigh-pressure terrane: Behavior of fluid-mobile elements in continental subduction zone

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Geoscience Frontiers 2021年第4期12卷 110-121页

作者： Zhipeng Xie keiko hattori Youpu Dong Jian Wang Department of Earth Sciences Kunming University of Science and TechnologyKunming 650093PR China Department of Earth and Environmental Sciences University of OttawaOttawa K1N 6N5Canada College of Earth Sciences Jilin UniversityChangchunJilin 130061PR China

Serpentinized peridotites in the Yangkou(YK),Suoluoshu(SLS) and Hujialin(HJL) areas in the Sulu ultrahighpressure terrane represent the relic of ancient subcontinental lithospheric mantle below the North China *** protoliths,harzburgite and dunite,were variably hydrated by aqueous fluids released from subducting Yangtze *** rocks are enriched in fluid-mobile elements(FME) including Sb(42–333 times the depleted mantle value) and Pb(30–476 times).The degrees of the FME enrichment are comparable to that of the Himalayan forearc serpentinites,and greater than forearc mantle serpentinites from Marianas,suggesting that the degrees of FME enrichment in the forearc serpentinites are greater in continental subduction zones than those in the oceanic subduction *** after olivine in the SLS serpentinite shows higher degrees of enrichment in Sb and As than those for antigorite after both olivine and orthopyroxene in the YK *** antigorite has highly enriched in Pb,U,Cs,and LREE,but not for the *** abundance of FME in two different species of serpentine reflects the different temperature of *** temperature lower than 300 ℃,formed lizardite at shallow depths of the mantle wedge incorporates elements that are fluid mobile at low temperatures,such as Sb and *** the temperature greater than 300 ℃,formed antigorite at a relatively deep mantle wedge incorporate more FME from the subducting continental slab(or fragments),including Pb,U,Cs,LREE as well as Sb and *** eventual breakdown of antigorite(600–700 ℃) in prograde metamorphism would discharge water as well as FME into the subducting channel and/or the overlying mantle.

关键词： Continental subduction channel Subcontinental lithospheric mantle Fluid-mobile element Serpentinite Antigorite Lizardite

Behavior of Siderophile and Chalcophile Elements in the Subcontinental Lithospheric Mantle beneath the Changbaishan Volcano,NE China

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Acta Geologica Sinica(English Edition) 2012年第2期86卷 407-422页

作者： WANG Jian LIU Jinlin hattori keiko XU Wenliang XIE Zhipeng SONG Yue College of Earth Sciences Jilin UniversityChangchun 130061China Department of Earth Sciences University of OttawaOttawaOntarioCanada KIN6N5

The mantle xenoliths in the Quaternary ChangbaishanVolcano in southern Jilin Province contain spinel-facies lherzolites. The equilibration temperatures for these samples range from 902℃ to 1064℃ based on the two-pyroxene thermometer of Brey and Kohler （1990）, and using the oxybarometry of Nell and Wood （1991）, the oxidation state was estimated from FMQ-1.32 to -0.38 with an average value of FMQ-0.81 （n = 8）, which is comparable to that of abyssal peridotites and the asthenospheric mantle. ThefO2 values of peridotites, together with their bulk rock compositions （e.g., Mg#, Al2O3, CaO, Ni, Co, Cr） and mineral compositions （e.g., Mg# of olivine and pyroxene, Cr# [=Cr/ [Cr＋Al]] and Mg# [=Mg/[Mg＋Fe2~] of spinel）, suggest that the present-day subcontinental lithospheric mantle （SCLM） beneath the Changbaishan Volcano most likely formed from an upwelling asthenosphere at some time after the late Mesozoic and has undergone a low degree of partial melting. The studied lherzolite xenoliths show low concentrations of S, Cu, and platinum group elements （PGE）, which plot a flat pattern on primitive-mantle normalized diagram. Very low concentrations in our samples suggest that PGEs occur as alloys or hosted by silicate and oxide minerals. The compositions of the studied samples are similar to those of peridotite xenoliths in the Longgang volcanic field （LVF） in their mineralogy and bulk rock compositions including the abundance of chalcophile and siderophile elements. However, they are distinctly different from those of peridotite xenoliths in other areas of the North China Craton （NCC） in terms of Cu, S and PGE. Our data suggest that the SCLM underlying the northeastern part of the NCC may represent a distinct unit of the newly formed lithospberic mantle.

关键词： Subcontinental lithospheric mantle siderophile and chalcophile elements oxidation state(fO2) upwelling asthenosphere Changbaishan Volcano

鲁西中生代高镁辉石闪长岩中超镁铁质捕虏体成因:氧化态和铂族元素证据

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吉林大学学报（地球科学版） 2012年第5期42卷 1390-1403页

作者：王建谢志鹏许文良 keiko hattori 吉林大学地球科学学院长春130061 渥太华大学地球科学系

鲁西莱芜晚中生代高镁闪长岩中含丰富的超镁铁质捕虏体,主要为纯橄岩(>80%),少量方辉橄榄岩(<5%)和橄榄辉石岩(<15%)。测定了代表性捕虏体的亲铁、亲铜元素含量,根据其矿物化学成分计算了捕虏体的氧化-还原状态。方辉橄榄岩遭受了不同... 详细信息

鲁西莱芜晚中生代高镁闪长岩中含丰富的超镁铁质捕虏体,主要为纯橄岩(>80%),少量方辉橄榄岩(<5%)和橄榄辉石岩(<15%)。测定了代表性捕虏体的亲铁、亲铜元素含量,根据其矿物化学成分计算了捕虏体的氧化-还原状态。方辉橄榄岩遭受了不同程度富Si熔体的交代,全岩富含Cr、Co、Ni和IPGE,高IPGE/PPGE值,是地幔深度部分熔融的残留。纯橄岩由铬铁矿和高Mg橄榄石组成,全岩富含Cr、Co、Ni,贫IPGE,低IPGE/PPGE值,可能为一种镁铁质熔体的堆晶岩。纯橄岩中橄榄石成分表现出一定的变化范围,局部镁橄榄石(Fo)成分高达94,可能是堆晶中橄榄石与足够的铬铁矿反应的结果,原始熔体可能为玻镁安山质岩浆。方辉橄榄岩和纯橄岩都显示高fO2值,FMQ+1.4～+2.4,与研究区早古生代相对还原的陆下岩石圈地幔(fO2低于C-CO2缓冲反应)形成鲜明对比。数据表明,中生代扬子大陆和华北克拉通碰撞之前,特提斯大洋板块和扬子大陆边缘相继俯冲到华北克拉通东缘之下,导致当时岩石圈地幔的fO2陡升。

关键词：晚中生代俯冲带铂族元素和氧化态高镁辉石闪长岩纯橄岩陆下岩石圈地幔鲁西岩石学

苏鲁超高压变质带胡家林超镁铁质岩成因及构造意义

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岩石学报 2018年第6期34卷 1539-1556页

作者：谢志鹏王建 hattori keiko 薛传东钟军伟王泽利昆明理工大学国土资源工程学院昆明650093 吉林大学地球科学学院长春130061 渥太华大学地球科学系山东科技大学地球科学与工程学院青岛266590

胡家林超镁铁质杂岩体产于苏鲁超高压变质带中部,纯橄岩和(石榴)单斜辉石岩呈不连续透镜体产于蛇纹石化橄榄岩中。纯橄岩遭受了部分蛇纹石化(烧失量=6.6%～13.2%),全岩富集强相容元素(Ni、Cr、Co)和Ir族PGE(IPGE;Ir、Os、Ru)及高IPGE/P... 详细信息

胡家林超镁铁质杂岩体产于苏鲁超高压变质带中部,纯橄岩和(石榴)单斜辉石岩呈不连续透镜体产于蛇纹石化橄榄岩中。纯橄岩遭受了部分蛇纹石化(烧失量=6.6%～13.2%),全岩富集强相容元素(Ni、Cr、Co)和Ir族PGE(IPGE;Ir、Os、Ru)及高IPGE/PPGE值,亏损Al、Ti、V,具高Mg~#橄榄石(Fo=91.7～92.4)和高Cr~#(0.68～0.76)尖晶石。纯橄岩高耐熔地球化学及矿物化学特征和古老的大陆岩石圈地幔相一致,表明其原岩来源于弧前地幔,代表了华北克拉通古老的大陆岩石圈地幔残留。(石榴)单斜辉石岩全岩呈相对低含量的强相容元素(Cr、Ni、Co)和IPGE,高含量的Al、Ti、V和流体迁移元素(Sr、Pb和Ba),球粒陨石标准化REE配分图呈明显"上凸"型,具低Mg~#橄榄石(Fo=76.6～76.8)和低Al_2O_3(<2.76%)和高SiO_2(54.56%～56.87%)的单斜辉石。全岩组成和矿物化学表明其原岩为俯冲带内超镁铁质火成堆晶岩,最初岩浆由地幔岩高程度部分熔融的熔体和俯冲带中富H_2O流体和/或熔体构成。(石榴)单斜辉石岩原岩曾被地幔流带入扬子大陆俯冲板片和上覆地幔楔之间的俯冲通道,经历了超高压变质作用和生成大量石榴石。(石榴)单斜辉石岩在折返过程中,与大陆岩石圈地幔楔剥离的蛇纹石化橄榄岩及纯橄岩相结合,形成超镁铁质杂岩体,整体被低密度的俯冲板片(主要由花岗质片麻岩和变质沉积岩组成)裹挟,折返至地壳浅部。

关键词：苏鲁超高压变质带铂族元素(PGE) 纯橄岩 (石榴)单斜辉石岩岩石成因

苏鲁超高压变质带中蛇纹岩成因:矿物化学和铂族元素证据

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吉林大学学报（地球科学版） 2012年第S3期42卷 119-131页

作者：谢志鹏王建 keiko hattori 吉林大学地球科学学院长春130061 渥太华大学地球科学系

苏鲁超高压变质带中部的仰口和梭罗树地区分布有大量蛇纹岩岩块和透镜体,矿物学和矿物化学表明它们的原岩分别为方辉橄榄岩和纯橄岩。蛇纹岩全岩亏损弱不相容元素(Al、Ti、V),富集强相容元素(Ni、Cr、Co)和Ir族PGE(IPGE:Ir、Os、Ru)以及... 详细信息

苏鲁超高压变质带中部的仰口和梭罗树地区分布有大量蛇纹岩岩块和透镜体,矿物学和矿物化学表明它们的原岩分别为方辉橄榄岩和纯橄岩。蛇纹岩全岩亏损弱不相容元素(Al、Ti、V),富集强相容元素(Ni、Cr、Co)和Ir族PGE(IPGE:Ir、Os、Ru)以及高IPGE/PPGE值。铬尖晶石具有高Cr#(0.57～0.79)。测试数据表明,蛇纹岩的原岩为华北克拉通边缘下部的弧前地幔橄榄岩。研究区的蛇纹岩与华北克拉通东部的地幔橄榄岩捕虏体对比显示,其与古老的岩石圈地幔地球化学特征相似,表明蛇纹岩的原岩为华北克拉通古老的岩石圈地幔残留。与区域内的石榴橄榄岩/石榴辉石岩不同,蛇纹岩未经历深俯冲过程及超高压变质作用,它们很可能在地幔楔部位与折返过程中的陆壳板片相结合,一起折返至地表。

关键词：苏鲁超高压变质带铂族元素大陆岩石圈地幔蛇纹岩岩石学

吉林东部汪清新生代玄武岩中地幔包体的矿物化学：对该地区岩石圈地幔形成过程的启示

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地学前缘 2013年第5期20卷 75-86页

作者：宋樾王建刘金霖谢志鹏 keiko H. hattori 吉林大学地球科学学院吉林长春130061 Department of Earth Sciences University of Ottawa Ottawa Ontario K1N 6N5 Canada

在对吉林汪清新生代玄武岩中橄榄岩包体进行全岩主、微量元素分析的基础上，重点分析了矿物的主、微量元素含量，讨论了华北克拉通东北缘与兴蒙造山带结合部位陆下岩石圈地幔所经历的部分熔融作用和地幔交代作用。橄榄石的Fo、单斜辉石... 详细信息

在对吉林汪清新生代玄武岩中橄榄岩包体进行全岩主、微量元素分析的基础上，重点分析了矿物的主、微量元素含量，讨论了华北克拉通东北缘与兴蒙造山带结合部位陆下岩石圈地幔所经历的部分熔融作用和地幔交代作用。橄榄石的Fo、单斜辉石以及尖晶石的Mg#和Cr#均表明该地区陆下岩石圈地幔相对饱满。对地幔橄榄岩透辉石微量元素模拟计算证实，汪清陆下岩石圈地幔经历了1％～3％的部分熔融作用，并遭受后期硅酸盐熔体交代作用。这些地幔特征与中国东部其他地区新生代主体岩石固相似。研究结果证明，吉林汪清中、新生代以来岩石圈性质的转变是在汇聚板块构造体制下通过“拆沉作用”实现的。

关键词：地幔橄榄岩矿物化学拆沉软流圈底辟汪清吉林东部

Associations among pain catastrophizing, muscle strength, and physical performance after total knee and hip arthroplasty

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World Journal of Orthopedics 2017年第4期8卷 336-341页

作者： Kazuhiro Hayashi Masato Kako Kentaro Suzuki keiko hattori Saori Fukuyasu Koji Sato Izumi Kadono Tadahiro Sakai Yukiharu Hasegawa Yoshihiro Nishida Department of Rehabilitation Nagoya University Hospital Department of Orthopaedic Surgery Nagoya University Graduate School and School of Medicine

AIM To investigate whether reductions in pain catastrophizing associated with physical performance in the early period after total knee arthroplasty(TKA) or total hip arthroplasty(THA).METHODS The study group of 46 participants underwent TKA or THA. The participants were evaluated within 7d before the operation and at 14d afterwards. Physical performance was measured by the Timed Up and Go(TUG) test, and 10-m gait time was measured at comfortable and maximum speeds. They rated their knee or hip pain using a visual analog scale(VAS) for daily life activities. Psychological characteristics were measured by the Pain Catastrophizing Scale(PCS). Physical characteristics were measured by isometric muscle strength of knee extensors and hip abductors on the operated side. The variables of percent changes between pre-and postoperation were calculated by dividing post-operation score by pre-operation *** Postoperative VAS and PCS were better than preoperative for both TKA and THA. Postoperative physical performance and muscle strength were poorer than preoperative for both TKA and THA. The percent change in physical performance showed no correlation with preoperative variables. In TKA patients, the percent change of PCS showed correlation with percent change of TUG(P = 0.016), 10-m gait time at comfortable speeds(P = 0.003), and 10-m gait time at maximum speeds(P = 0.042). The percent change of muscle strength showed partial correlation with physical *** percent change of VAS showed no correlation with physical performances. On the other hand, in THA patients, the percent change of hip abductor strength showed correlation with percent change of TUG(P =0.047), 10-m gait time at comfortable speeds(P = 0.001),and 10-m gait time at maximum speeds(P = 0.021). The percent change of knee extensor strength showed partial correlation with physical performances. The percent change of VAS and PCS showed no correlation with physical *** Changes

关键词： Gait Hip arthroplasty Knee arthroplasty Osteoarthritis Pain Pain management Postoperative care

Ultrahigh-pressure metamorphism and P-T-t path of Xiaoxinzhuang eclogites from the middle Sulu orogenic belt, eastern China

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Ultrahigh-pressure metamorphism and P-T-t path of Xiaoxinzhu...