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华北克拉通新太古代晚期岩浆作用:对构造体制和克拉通化的启示

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地学前缘 2024年第1期31卷 77-94页

作者：万渝生董春艳颉颃强李鹏川刘守偈李源王宇晴王堃力刘敦一中国地质科学院地质研究所北京离子探针中心北京100037 吉林大学地球科学学院吉林长春130061 江西应用技术职业学院自然资源部离子型稀土资源与环境重点实验室江西赣州341000

在对华北克拉通太古宙基底作简要介绍的基础上,本文总结了华北克拉通新太古代晚期(主要为2.55~2.5 Ga期间)岩浆岩的锆石年龄分布模式、地球化学和Nd-Hf-O同位素组成特征。华北克拉通新太古代晚期变质基底的主要特征如下:(1)新太古代晚... 详细信息

在对华北克拉通太古宙基底作简要介绍的基础上,本文总结了华北克拉通新太古代晚期(主要为2.55~2.5 Ga期间)岩浆岩的锆石年龄分布模式、地球化学和Nd-Hf-O同位素组成特征。华北克拉通新太古代晚期变质基底的主要特征如下:(1)新太古代晚期岩石在华北克拉通广泛分布,但许多地区都存在中太古代晚期—新太古代早期地质记录。(2.岩浆锆石年龄主要变化于2.55~2.5 Ga,年龄峰值约为2.52.Ga。(3.与新太古代早期以前(>2.6 Ga)的英云闪长岩-奥长花岗岩-花岗闪长岩(TTG)相比,新太古代晚期英云闪长岩和花岗闪长岩比例明显增大。富钾花岗岩、闪长-辉长岩(包括闪长岩、辉长岩及两者之间过渡岩石)、赞岐岩(Sanukite,主体为富镁闪长岩)分布范围和规模也明显增大。大规模富钾花岗岩主要分布于华北克拉通东部,构成新太古代晚期双岩浆岩带的富钾花岗岩带。(4)在新太古代晚期变质基底分布区,几乎都有变质表壳岩存在。它们以较小规模存在于TTG和富钾花岗岩中。岩石类型包括变玄武质岩石、变质安山质-英安质火山岩/火山碎屑岩和变质碎屑沉积岩。一些地区存在变质超基性岩。(5)总体上,新太古代晚期地质事件存在如下演化规律:首先是表壳岩形成,然后是TTG侵入,最后是变质变形和富钾花岗岩形成。2.6~2.55 Ga为华北克拉通岩浆构造的“寂静期”。(6)新太古代晚期TTG岩石的Sr/Y和La/Yb比值存在很大变化,中-高压TTG岩石大量形成表明新太古代晚期陆壳规模、厚度发生了明显增大。至少部分富钾花岗岩在形成过程中有沉积物参与。(7)不同类型TTG岩石具有类似的全岩Nd同位素和岩浆锆石Hf同位素组成,Nd-Hf同位素亏损地幔模式年龄主要分布在3.0~2.5 Ga,与中太古代晚期—新太古代早期岩石的模式年龄相近或稍偏年轻。富钾花岗岩Nd-Hf同位素组成特征受物源区早期形成演化历史制约。岩浆锆石O同位素组成与全球太古宙岩浆锆石类似,但显示更大的变化范围。结合其他研究,上述证据表明:(1)中太古代晚期—新太古代早期是华北克拉通陆壳增生最重要时期,这与全球其他许多克拉通类似,不同之处在于华北克拉通遭受了新太古代晚期构造岩浆热事件强烈改造;(2.在华北克拉通,类似于现代板块运动的构造体制在新太古代晚期开始启动;(3.规模最大的BIF(条带状铁建造)沿华北克拉通东部古老陆块西缘的双岩浆岩带分布,鞍本和冀东之间、冀东和鲁西之间是BIF找矿重要靶区;(4)华北克拉通在新太古代晚期完成初始克拉通化。

关键词：华北克拉通新太古代晚期岩浆作用 Nd-Hf-O同位素构造体制

AGE OF THE ALTYN TAGH STRIKE—SLIP FAULT

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地学前缘 2000年第S1期7卷 208-209页

作者： Li Haibing 1, Yang Jingsui 1, Xu Zhiqin 1, Wu Cailai 1, Zhang Jianxin 1, wan Yushen 1, Shi Rendeng 1, Juhn G. Liou 2.Trevor R. Ireland 2.(1 {3. of {2., chinese {3. of geological Sciences, Beijing 10003., China 2.Department of

A 100～500m\|wide mylonite zone in the Altun Group of Lower Proterozoic age was discovered along the Altyn Tagh strike\|slip fault. The zone is mainly composed of amphibolitic and granitic mylonites. The planar joints of the rocks strike in NE70 and dip steeply (nearly vertical), coincident with the striking of Altyn Tagh fault zone, and their stretched lineations are nearly horizontal. Shear strains are well developed and show sinistral sheared. The amphibolitic and granitic mylonites are most probably the products of deep\|seated melting caused by sinistral strike\|slip shearing as suggested by the evidence below: (1) The migmatization is intensely developed and spatially controlled by the shear zone, and the rock has a set of NNE perspective foliation which is in accord with the direction of the Altyn Tagh strike\|slip fault zone. (2. The recrystallized hornblende aggregate is distributed in band with obvious nebulous texture, indicating the characteristics of anatexis, and the hornblendes are oriented and form the nearly horizontal stretching lineation; some hornblendes have titanite inclusions, and magmatic long\|columnar zircons are in directional arrangement.(3. The banded felsic material is developed, and the plagioclase is characteristic of high\|temperature plastic deformation and shows sinistral shear stain. (4) In mylonites, all the axis C fabric of quartz shows the feature of sinistral shearing and the majority is generally middle to low temperature fabric, but there also exists high temperature fabric, which suggests that high temperature shearing occur in the early stage of strike\|slip deformation and it is characterized by middle to low temperature shearing at the beginning of anatexis or in the late stage of the deformation. (5) On the XZ plane of mylonite and mylonitized rocks, there exists the consistent sinistral shear stain, which suggests the products of the same strike\|slip *** were separated from three samples of mylonitized gra

关键词： Altyn Tagh fault Tibet plateau SHRIMP dating mylonite

Characteristics and genesis of groundwater salinization in coastal areas of the Lower Reaches of Oujiang Basin

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Journal of Groundwater Science and Engineering 2024年第2期12卷 190-204页

作者： Mei-hui Zhang Shi-yang Zhou Dan-dan liu Ying Zhang Yu-xi Zhang Xi Chen Hui-wei wang Bei Li Wei Kang Bing Yi wan-peng Shi institute of Hydrogeology and Environmental geology Chinese Academy of Geological SciencesShijiazhuang 050061China Fujian Provincial Key Laboratory of Water Cycling and Eco–geological Processes Xiamen 361021FujianChina China University of Geosciences(Beijing) Beijing 100083China Changsha Center of Natural Resources Comprehensive Survey China Geological SurveyChangsha 410600China Hydrogeological Environmental geological Survey Center of China geological Survey Tianjin 071501China China University of Geosciences Wuhan 430074China

The coastal areas of the lower reaches of Oujiang River Basin are rich in groundwater ***,the unsustainable exploitation and utilization of groundwater have led to significant changes in the groundwater *** the characteristics and genesis of groundwater salinization is crucial for preventing its deterioration and ensuring sustainable *** this study,a comprehensive approach combining the ion ratio method,mineral saturation index method and multivariate statistical analysis was employed to investigate the hydrochemical characteristics and main controlling factors in the study *** findings reveal that:(1)Groundwater samples in study area exhibit a neutral to slightly alkaline *** predominant chemical types of unconfined water are HCO_(3.-Ca·Na,HCO_(3.·Cl-Na·Ca and HCO_(3.·SO_(4)-Ca·Na,while confined water mainly exhibits Cl·HCO_(3.-Na and Cl-Na types.(2.Salinity coefficients indicate an increase in salinity from unconfined to confined ***,Na^(+)and Cl^(–)concentrations show an increasing trend from mountainous to coastal areas in unconfined water,while confined water displays variability in TDS,Na^(+)and Cl^(–)concentrations.(3.Groundwater salinity is mainly influenced by water-rock interactions,including the dissolution of halite and gypsum,cation exchange,and seawater intrusion ***,human activities and carbonate dissolution contribute to salinity in unconfined *** intrusion is identified as the primary factor leading to higher salinity in confined water compared to unconfined water,with increasing cation exchange and seawater interaction observed from unconfined to confined water.

关键词： Hydrochemical Multivariate statistical analysis Seawater intrusion

Geochemistry and SHRIMP U-Pb Zircon Dating of Mafic Rocks North of Zunhua City, Eastern Hebei, North China Craton： Paleoproterozoic Gabbro rather than Neoarchean Ophiolite

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Acta Geologica Sinica(English Edition) 2018年第3期92卷 1024-1040页

作者： XIE Hangqiang DONG Chunyan Alfred KRONER liu Shoujie BAI Wenqian liu Dunyi {2. {3. Beijing SHRIMP Center Institute of Geology Chinese Academy of Geological Sciences Beo'ing 10003 7 China Department of Geosciences University of Mainz D-55099 Mainz Germany

Abundant mafic-ultramafic blocks and dikes occur in the area north of Zunhua City, eastern Hebei Province, and were previously suggested to be part of a late Archean ophiolitic assemblage. We employed SHRIMP zircon dating and a geochemical study on these mafic and surrounding rocks to test the ophiolite hypothesis. The SHRIMP data suggest that three metagabbro samples were metamorphosed at ～1.8 Ga. Numerous ～2.5 Ga zircons display strong oscillatory zoning, characteristic of zircons from granitoid rocks but not from gabbro, so we suggest that these are xenocrystic grains. The age of these xenocrystic zircons and their metamorpbic rims suggests that these mafic blocks formed in Paleoproterozoic. The surrounding gneiss of intermediate composition also contains 2.5 Ga zircons with oscillatory zoning and 1.8 Ga metamorphic rims. Fractionated REE patterns and Nb, Ta, Zr, Hf negative anomalies to variable extent were observed in the mafic blocks and surrounding rocks, also supporting a significant difference in the chemistry of ophiolitic rocks. Our data suggest that many mafic blocks in northern Zunhua are not part of a late Archean ophiolite complex but part of a tectonically dismembered Paleoproterozoic intrusive gabbro complex. This study shows that late Paleoproterozoic metamorphism occurred in the western part of eastern Hebei Province.

关键词： metagabbro ophiolite SHRIMP zircon dating Zunhua North China Craton

Archean Basement and a Paleoproterozoic Collision Orogen in the Huoqiu Area at the Southeastern Margin of North China Craton: Evidence from Sensitive High Resolution Ion Micro-Probe U-Pb Zircon Geochronology

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Acta Geologica Sinica(English Edition) 2010年第1期84卷 91-104页

作者： wan yusheng DONG Chunyan wanG Wei XIE Hangqiang {3. Dunyi Beijing SHRIMP Center Institute of Geology Chinese Academy of Geological Sciences Beijing 10037 China

This paper reports sensitive high resolution ion micro-probe U-Pb zircon ages for the ＂Huoqiu Group＂ and granitoids of the Early Precambrian basement in the Huoqiu area, southeastern margin of the North China Craton. The ＂Huoqiu Group＂ is similar in rock association and metamorphism to the khondalite series, apart from it containing considerable amounts of banded iron formation. All detrital zircons from the ＂Huoqiu Group＂ meta-sedimentary rocks are 3.0 Ga and 2.75 Ga, without any 2.5 Ga and younger ones, as is commonly found in Paleoproterozoic khondalite series in other areas of the North China Craton. In the Huoqiu area, 2.75 Ga and 2.56 Ga granitoids have also been identified. This basement assemblage underwent strong metamorphism during the late Paleoproterozoic （-1.84 Ga） tectonothermal event that is widely developed in the North China Craton. Thus the formation time of the ＂Huoqiu Group＂ can be constrained between 2.75 and 1.84 Ga in terms of detrital and metamorphic zircon ages. It is considered, combined with regional data, that there may be a Paleoproterozoic collision orogen extending in a NWW-SEE direction to the southern margin of the North China Craton.

关键词： khondalite series trondhjemite-tonalite-granodiorite sensitive high resolution ion micro-probe U-Pb dating Archean Paleoproterozoic collision orogen North China Craton

基于Hsp70基因的绵羊肺炎支原体TaqMan检测方法的建立及其遗传演化分析

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畜牧兽医学报 2024年第4期55卷 1684-1695页

作者：江锦秀张靖鹏林裕胜刘维巍胡奇林万春和福建省农业科学院畜牧兽医研究所福州350013 福建农林大学动物科学学院(蜂学学院) 福州350002

热休克蛋白70 (heat shock protein 70,Hsp70)是绵羊肺炎支原体(Mycoplasma ovipneumoniae, Movi)的重要膜蛋白,是机体内高度保守的生物分子,但在种间差异大,可作为分子生物学检测的候选靶区。为建立基于Hsp70基因的Movi通用型TaqMan实... 详细信息

热休克蛋白70 (heat shock protein 70,Hsp70)是绵羊肺炎支原体(Mycoplasma ovipneumoniae, Movi)的重要膜蛋白,是机体内高度保守的生物分子,但在种间差异大,可作为分子生物学检测的候选靶区。为建立基于Hsp70基因的Movi通用型TaqMan实时荧光定量PCR(qPCR)检测方法,并进一步了解其遗传变异情况,本研究基于GenBank中Movi的Hsp70基因特征,设计特异性的引物及探针,建立了基于Hsp70基因的绵羊肺炎支原体qPCR检测方法。应用建立的检测方法对88份山羊鼻拭子样品及43.疑似羊支原体性肺炎(Mycoplasmal pneumonia of sheep and goats, MPSG)病料进行检测。将检测结果为Movi阳性的肺组织样品进行分离鉴定,并对分离株Hsp70基因进行序列分析。结果显示,建立的qPCR检测方法其相关系数为1.00,扩增效率为96.0%,斜率为-3.411,Y轴截距为3..2.。特异性强,与丝状支原体山羊亚种(Mycoplasma mycoides ***, Mmc)、山羊支原体山羊肺炎亚种(Mycoplasma capricolum ***, Mccp)、莱氏无胆甾原体(Acholeplasmalaidlawii, AL)、无乳支原体(Mycoplasma agalactiae, Maga)、伪结核棒状杆菌(Corynebacterium pseudotuberculosis, CP)、羊口疮病毒(orf virus, ORFV)、牛支原体(Mycoplasma bovis, Mb)等牛羊常见病原均无交叉反应;敏感性高,最低检测限为5.72.copies·μL^(-1);重复性优,组内变异系数和组间变异系数均小于1.00%。6株Movi分离株Hsp70基因全长均为1 818 bp,与其它Movi参考株核苷酸和氨基酸同源性分别为96.0%~99.4%和98.0%~100.0%;进一步分析发现,山羊源Movi均比绵羊源多1个N-糖基化位点。遗传演化分析表明,其均处于ClusterⅠA亚分支(均为山羊源)。综上,本研究建立了特异性强、敏感性高、重复性优的基于Hsp70基因的Movi的qPCR检测方法。序列分析发现,不同来源Movi的Hsp70基因核苷酸同源性高;遗传演化分析证实,Movi福建株与山羊源分离株遗传关系较近。本研究不仅为Movi临床诊断提供了技术支持,更为进一步了解Movi遗传演化规律提供参考。

关键词：绵羊肺炎支原体 Hsp70基因 TaqMan实时荧光定量PCR方法序列分析

考虑SOC的混合储能功率分配与自适应虚拟惯性控制

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电力系统保护与控制 2024年第5期52卷 83-93页

作者：马文忠王立博王玉生万蓉蓉王昕睿王嘉星中国石油大学(华东)新能源学院山东青岛266580 中国石油天然气股份有限公司规划总院北京100083

电力电子化的直流配电网存在低惯性问题,不利于系统稳定运行。混合储能设备可向电网提供虚拟惯性,但不同类型的储能之间存在功率协调问题,并且储能的荷电状态(state of charge, SOC)对虚拟惯性的调节也有约束作用。针对上述问题,提出了... 详细信息

电力电子化的直流配电网存在低惯性问题,不利于系统稳定运行。混合储能设备可向电网提供虚拟惯性,但不同类型的储能之间存在功率协调问题,并且储能的荷电状态(state of charge, SOC)对虚拟惯性的调节也有约束作用。针对上述问题,提出了一种自适应时间常数的分频控制策略,时间常数根据混合储能系统(hybridenergy storage system, HESS)的SOC而动态调整以改变功率分配。首先,通过分析储能SOC与虚拟惯性的关系,并考虑储能充放电极限问题,研究兼顾SOC、电压变化率以及电压幅值的自适应虚拟惯性控制策略,提高系统惯性。然后,建立控制系统的小信号模型,分析虚拟惯性系数对系统的影响。最后,基于Matlab/Simulink搭建直流配电网仿真模型,验证了所提控制策略能合理分配HESS功率,提高超级电容器利用率,改善直流电压与功率稳定性。

关键词：直流配电网混合储能功率分配荷电状态虚拟惯性

Formation Age of the Sujiagou Komatiites in Western Shandong: Further Constraints from SHRIMP U-Pb Zircon Dating on Granitic Dykes

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Acta Geologica Sinica(English Edition) 2020年第4期94卷 877-883页

作者： wan yusheng DONG Chunyan XIE Hangqian wanG Shijin Beijing SHRIMP Center Institute of GeologyChinese Academy of Geological SciencesBeijing 100037China Shandong geological Survey institute Jinan 250013China

Komatiites are presented as direct evidence for higher mantle temperatures during the Archean. In the North China Craton, komatiites with spinifex structure have been identified only at one locality, i.e. the Sujiagou area, western Shandong. They were considered as formed during the early Neoarchean mainly based on their association with supracrustal rocks considered to be that age. This study carried out SHRIMP U-Pb zircon dating on metamorphosed trondhjemitic and monzogranitic dykes intruding the Sujiagou komatiites, and they have magmatic zircon ages of 2.92.± 12.Ma and 2.86 ± 13.Ma respectively. This provides direct evidence that the komatiites formed during the early Neoarchean.

关键词： granitic dyke SHRIMP U-Pb zircon dating Sujiagou komatiite Neoarchean western Shandong

Provenance of Carboniferous sedimentary rocks in the northern margin of Dabie Mountains,central China and the tectonic significance:constraints from trace elements,mineral chemistry and SHRIMP dating of zircons

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Provenance of Carboniferous sedimentary rocks in the norther...