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Transformation from Neoproterozoic Sinistral to Early Paleozoic Dextral Shearing for the Jingdezhen Ductile Shear Zone in the Jiangnan Orogen, South China

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Journal of Earth Science 2018年第2期29卷 376-390页

作者： xianbing xu Shoufa Lin Shuai Tang xuefen Zhang School of Earth Sciences China University of Geosciences Department of Earth and Environmental Sciences University of Waterloo School of Resources and Environment Hefei University of Technology No.266 Geological Party Nuclear Industry Geological Bureau of Jiangxi Province State Key Laboratory for Nuclear Resources and Environment East China Institute of Technology

The Jingdezhen ductile shear zone is evolved from the Neoproterozoic Zhangyuan ophiolite melange belt in the eastern Jiangnan Orogen, South China. Comprehensive study of geometry, kinematics, quartz c-axis fabric, temperature-pressure conditions and geochronology were conducted in this study. The Jingdezhen shear zone extends -180 km along the NE orientation with two groups of subvertical fo- liation and subhorizontal lineation. One group of foliation strikes NEN orientation whereas another one NEE orientation. Field investigation, microscopic observation and quartz c-axis fabric show that sinistral shearing along NEN-striking foliation occurred earlier than dextral shearing along NEE-striking foliation. Syn-tectonic staurolite porphyroblasts and deformation manner of feldspar imply that sinistral shearing occurred at 530-420 ℃ and 6-2 kbar. Deformation manner and c-axis fabric of quartz and pre-tectonic staurolite porphyroblasts indicate that dextral shearing took place at 420-300 ℃. LA-ICP-MS zircon U-Pb and mica ^40Ar/^39Ar dating indicate that the sinistral shearing occurred during Neoproterozoic oro- geny （830-800 Ma） whereas the dextral shearing at 447＋12 Ma. The sinistral shearing resulted from the Neoproterozoic final assembly between the Yangtze and Cathaysia blocks. The dextral shearing was caused by Early Paleozoic orogen parallel extension and clockwise rotation.

关键词： Jingdezhen ductile shear zone quartz c-axis fabric temperature-pressure condition geochronology Jiangnan Orogen South China.

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U-Pb Dating of Volcanic Rocks and Granites along the Wuyishan Belt:Constraints on Timing of Late Mesozoic Tectonic Events in Southeast China

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Acta Geologica Sinica(English Edition) 2011年第1期85卷 130-144页

作者： xu xianbing ZHANG Yueqiao JIA Dong SHU Liangshu School of Earth Sciences and Engineering Nanjing University Nanjing Jiangsu 210093 China Institute of Geomechanics Chinese Academy of Geological Sciences Beijing 100081 China

Five volcanic rock samples and two granite samples taken from the volcanic basins in western Fujian and southern Jiangxi were dated by using the zircon laser albation-inductively coupled plasma mass spectrometry U-Pb method. Together with previously dated ages, the dates obtained provide important constraints on the timing of late Mesozoic tectonic events in SE China. The volcanic rock samples yield ages of 183.1±3.5 Ma, ca. 141 Ma to 135.8±1.1 Ma, 100.4±1.5 to 97.6±1.1 Ma, confirming three episodes of late Mesozoic volcanic activities, which peaked at 180±5 Ma, 140±5 Ma and 100±5 Ma, respectively, along the Wuyishan belt. Moreover, based on field investigations of these volcano-sedimentary basins, we have recognized two compressional tectonic events along this belt. The early one was characterized by Upper Triassic to Middle Jurassic NNE-trending folds that were intruded by late Jurassic granites; and the late one caused the Lower Cretaceous volcano-sedimentary layer to be tilted. The dated age 152.9±1.4 Ma of the granitic samples from the Hetian granitic pluton in the Changting Basin and that from the Baishiding granitic pluton, 100.2±1.8 Ma, in the Jianning Basin, give the upper boundaries of these two tectonic events respectively. Hence, the late Mesozoic tectonic evolution of SE China was alternated between extension and compression.

关键词： Late Mesozoic volcanic rocks LA-ICP-MS U-Pb compressional events Wuyishan Belt SE China

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A comprehensive method to explore inhibitory kinetics and mechanisms of an anticoagulant peptide derived from Crassostrea gigas

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Food Science and Human Wellness 2022年第6期11卷 1491-1499页

作者： Shuzhen Cheng Di Wu Hanxiong Liu xianbing xu Beiwei Zhu Ming Du Department of Food Science and Engineering National Engineering Research Center of SeafoodDalian Polytechnic UniversityDalian 116034China Beijing Advanced Innovation Center for Food Nutrition and Human Health College of Food Science and Nutritional EngineeringChina Agricultural UniversityBeijing 100083China

A comprehensive method was applied to evaluate the anticoagulant activity of a novel anticoagulant peptide(NAESLRK)derived from oyster(Crassostrea gigas).The anticoagulant peptide drastically reduced the extrinsic clotting activity and also impaired the intrinsic clotting activity *** with clotting data,the thrombin peak height was reduced to 84.7 nmol/L from 123.4 nmol/L,and thrombin generation time was delayed to 4.67 min from 4.42 min when the extrinsic trigger was *** inhibitory kinetics of FⅪa,FⅨa,FⅩa,FⅡa,and APC in a purified component system rationally explained the reduction of extrinsic clotting activity and impairment of thrombin *** the inhibition of FⅩa and FⅡa activity,the activation processes of FⅩand FⅡby intrinsic/extrinsic tenase complex and prothrombinase were also *** anticoagulant activity in the plasma system was the result of comprehensive inhibition of various *** research provided a novel method for anticoagulant evaluation and inhibitory mechanism of bioactive peptides from food products.

关键词： Oyster Anticoagulant peptide Inhibitory kinetics Coagulation factor Non-specific inhibitor

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Campus Vibration in Nanwangshan Campus,China University of Geosciences at Wuhan Monitored by Short-Period Seismometers

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Journal of Earth Science 2020年第5期31卷 950-956页

作者： Lihui Wu Dun Wang Ziguang Lei Jing Fu Shuai Min xianbing xu Sarina Bao School of Management Hubei University of EducationWuhan 430205China Institute of Supply Chain Operation and Service Innovation Hubei University of EducationWuhan 430205China State Key Laboratory of Geological Processes and Mineral Resources School of Earth SciencesChina University of GeosciencesWuhan 430074China Department of Environmental Science and Policy University of CaliforniaCA 95616USA

Continuous seismic observations can record seismic waveforms, and ambient noise, for the purposes of earthquake researches and other applications. Here we deploy three digital seismometers(EPS-2) in and around the Nanwangshan Campus of the China University of Geosciences(Wuhan). This network was running from April 9 to May 9 of 2018. During this period, the seismometers recorded the May 4, 2018 M6.9 Hawaii earthquake. From the recorded waveforms, we could observe clearly the P and S arrivals, and the corresponding particle motions. Analysis of continuous observations of ambient noise shows obvious fluctuation of vibration intensity inside of the campus. The campus is quietest from 0 to 5 am. From 5 am on, the vibration intensity increases, and reaches the peak of entire day at 12 am. The amplitude then decreases to a very low level at 19:30 to 20:00 pm, and reaches another strong noisy time at 21:00 to 21:30 pm. After 21:30 pm, the intensity goes down slowly. We also observed seismic signals that were generated by the interaction of speed-control hump cars and ground. By taking the envelope and smooth operations, we observe different characteristics for different car speeds, which suggests that seismic monitoring approaches can be used for speed measurement of cars. This kind of small seismic network running in a real time fashion, would greatly help understanding of the sources of ambient noise at high frequency bands in interested areas. Analysis of a long-term observed dataset, and real time illustration will help to strengthen campus security and high-precision laboratory deployments, and also contribute to research atmosphere in earthquake science.

关键词： ambient noise vibration intensity seismic waves seismometers human activity

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Three novel umami peptides derived from the alcohol extract of the Pacific oyster(Crassostrea gigas):identification,characterizations and interactions with T1R1/T1R3 taste receptors

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Food Science and Human Wellness 2024年第1期13卷 146-153页

作者： Baifeng Fu Di Wu Shuzhen Cheng xianbing xu Ling Zhang Lishu Wang Heshanm REl-Seedi Hanxiong Liu Ming Du School of Food Science and Technology Dalian Polytechnic UniversityDalian 116034China Collaborative Innovation Center of Seafood Deep Processing Dalian Polytechnic UniversityDalian 116034China National Engineering Research Center of Seafood Dalian Polytechnic UniversityDalian 116034China Division of Hematology and Oncology Department of MedicineMedical College of WisconsinMilwaukee 53226USA Division of Pharmacognosy Department of Medicinal ChemistryBiomedical CentreUppsala UniversityUppsala SE-75123Sweden

Oyster(Crassostrea gigas),the main ingredient of oyster sauce,has a strong umami *** this study,three potential umami peptides,FLNQDEEAR(FR-9),FNKEE(FE-5),and EEFLK(EK-5),were identified and screened from the alcoholic extracts of the oyster using nano-HPLC-MS/MS analysis,i Umami-Scoring Card Method(i Umami-SCM)database and molecular docking(MD).Sensory evaluation and electronic tongue analysis were further used to confirm their *** threshold of the three peptides ranged from 0.38 to 0.55 mg/m *** with umami receptors T1R1/T1R3 indicated that the electrostatic interaction and hydrogen bond interaction were the main forces ***,the Phe592 and Gln853 of T1R3 were the primary docking site for MD and played an important role in umami *** with two Glu residues at the terminus had stronger umami,especially at the *** results contribute to the understanding of umami peptides in oysters and the interaction mechanism between umami peptides and umami receptors.

关键词： Oyster umami peptides iUmami-SCM Taste characterization Molecular docking

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Controlled coupling and characterization of oyster (Crassostrea gigas) ferritin with gold nanostars

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Food Science and Human Wellness 2024年第6期13卷 3202-3209页

作者： Han Li Xiaoyu Xia Shuzhen Cheng Jiachen Zang Zhenyu Wang xianbing xu Ming Du School of Food Science and Technology National Engineering Research Center of SeafoodCollaborative Innovation Center of Seafood Deep ProcessingDalian Polytechnic UniversityDalian 116034China College of Food Science and Nutritional Engineering China Agricultural UniversityBeijing 100083China

Ferritin has good thermal stability,resistance to certain acids and bases,and targeting,and has broad application prospects in the synthesis of gold nanostars(AuNS).In this study,we screened monodisperse AuNS with uniform particle size and morphology through a one-step synthesis method and coupled the synthesized AuNS with oyster ferritin(GF1).The results showed that the surface plasmon resonance(SPR)peaks of the coupled GF1@AuNS changed signifi cantly,and the changes in infrared spectra and potential confirmed the success of the synthesis,while the microscopic morphology showed an increase in particle size and surface peak ***,GF1@AuNS does not induce cell death in the 100µmol/L range,is highly stable in physiological environments,and exhibits good X-ray attenuation in micro-computed *** to the unique functional activity of ferritin and AuNS,GF1@AuNS has potential applications in food detection and drug development in the future.

关键词： Gold nanostars(AuNS) Oyster ferritin Synthesis Structure Micro-computed tomography

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Ferritin nanocage loading LYC for improving BBB transcytosis and attenuating D-gal-induced apoptosis in PC12 cells

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Food Science and Human Wellness 2023年

作者： Xiaoyu Xia Han Li xianbing xu Zhenyu Wang Junjie Yi Guanghua Zhao Ming Du School of Food Science and Technology， Dalian Polytechnic University Collaborative Innovation Centre of Provincial and Ministerial Co-construction for Seafood Deep Processing National Engineering Research Centre of Seafood Dalian Faculty of Food Science and Engineering， Kunming University of Science and Technology College of Food Science and Nutritional Engineering， China Agricultural University

Aging is a physiological process that leads to degeneration and functional decline of the brain. This is accompanied by intracellular peroxidation and neuronal apoptosis. Natural antioxidants possess a remarkable effect on attenuating the oxidative stress cascade and apoptosis of neurons; however， the challenge of using natural antioxidants for neuroprotection is fabricating a delivery system to overcome the blood-brain barrier (BBB) transport. Herein， we successfully created a stable delivery platform built on rigid ferritin nanocage loading natural lycopene (LYC) molecules， crossing the BBB in quantity and being taken up in neurons. This nanoparticle worked on D-galactose-induced senescence via alleviating neuronal hyperoxidation injury and weakening neuronal apoptosis in PC12 and BV2 cells. More importantly， this natural delivery system possesses inherent biocompatibility and potential application in improving the bioavailability of bioactive edible compounds with low water solubility. This study demonstrated the effectiveness of natural antioxidant nanomedicines in maintaining the defenses of intracerebral peroxidation and improve degenerating neurons， providing the potential to combat further imbalances of neuronal microenvironment in aging neuropathy.

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南岭构造带基础地质特征与成矿地质背景

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地球科学 2021年第4期46卷 1133-1150页

作者：徐先兵梁承华陈家驹徐亚东中国地质大学地球科学学院湖北武汉430074

南岭构造带横跨扬子地块、江南造山带以及华夏地块,是中国钨锡铅锌铀等有色金属和铌钽锂铯与稀土等关键金属成矿带.通过综述近十五年来的研究进展,总结了南岭构造带基础地质特征与成矿地质背景.扬子与华夏地块沿永州-桂林-柳州一线于新... 详细信息

南岭构造带横跨扬子地块、江南造山带以及华夏地块,是中国钨锡铅锌铀等有色金属和铌钽锂铯与稀土等关键金属成矿带.通过综述近十五年来的研究进展,总结了南岭构造带基础地质特征与成矿地质背景.扬子与华夏地块沿永州-桂林-柳州一线于新元古代拼合,但缺乏直接的地质证据,需对龙胜蛇绿混杂岩和鹰扬关混杂岩进行深入研究.新元古代至中生代花岗岩二阶段模式年龄T_(DM2)值揭示2.0~1.2 Ga为南岭构造带的主要地壳增生期.相似的花岗岩特征和构造线方向指示广西期和印支期造山机制均为陆内造山作用,是华南大陆南侧不同板块之间拼贴远程应力场的产物.燕山早期花岗岩ε_(Hf)(t)值沿南岭构造带自西向东显著减小,而T_(DM2)值明显增加,指示湘南-桂北-粤北地区在晚侏罗世经历了古太平洋板块断离和软流圈上涌并发育强烈的壳幔相互作用,为南岭构造带东段华夏地块上钨锡等多金属成矿提供了成矿物质来源和有利的伸展构造背景.南岭构造带西段扬子地块构造相对稳定且显生宙岩浆活动较弱,新元古代大塘坡组和寒武系底部页岩是良好的页岩气勘探目标.综合沉积、岩浆以及构造变形,华南中生代特提斯构造域向古太平洋构造域转换开始于晚三叠世.

关键词：南岭构造带华南板块基础地质成矿地质背景中生代构造转换构造学

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湘东南中泥盆统石英砂砾岩物源分析及其大地构造意义

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地球科学 2021年第10期46卷 3421-3434页

作者：陈家驹徐先兵梁承华徐亚东中国地质大学地球科学学院湖北武汉430074

早古生代江南隆起的形成与剥蚀作用可以用来制约华南广西期造山作用及其动力学机制.通过对江南隆起南侧湘东南南湾地区中泥盆统跳马涧组石英砂砾岩的碎屑锆石U-Pb年代学、锆石微量元素地球化学以及全岩地球化学的分析,讨论了其物源及其... 详细信息

早古生代江南隆起的形成与剥蚀作用可以用来制约华南广西期造山作用及其动力学机制.通过对江南隆起南侧湘东南南湾地区中泥盆统跳马涧组石英砂砾岩的碎屑锆石U-Pb年代学、锆石微量元素地球化学以及全岩地球化学的分析,讨论了其物源及其大地构造意义.4件样品的270颗有效碎屑锆石U-Pb年龄谱由430~440 Ma主峰与800~1 100 Ma、1 700~2 000 Ma和2 400~2 600 Ma次峰组成.锆石CL图像、Th/U比值以及稀土元素配分图指示碎屑锆石以岩浆锆石为主,仅有少量变质锆石和热液锆石.矿物形态、组成以及成熟度指示其源区为近源,沉积于滨海环境.综合源区分析表明,湘东南中泥盆统跳马涧组石英砂砾岩的物源来自其北侧的江南隆起.江南隆起形成于广西期陆内造山作用.早古生代岩浆锆石的微量元素地球化学特征表明其为大陆型锆石,形成于大陆弧构造环境.结合区域地质特征,华南广西期造山作用是其南侧大洋俯冲作用的产物,与冈瓦纳大陆的聚合有关.

关键词：中泥盆统跳马涧组碎屑锆石U-Pb年代学物源分析江南隆起华南广西期造山作用沉积学

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江南东段地区NE-SW向断裂带断层滑移矢量反演及其大地构造意义

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地球科学 2019年第5期44卷 1761-1772页

作者：梁承华徐先兵李启铭桂林汤帅中国地质大学地球科学学院湖北武汉430074 江西省核工业地质局二六六大队江西南昌330013

华南中-新生代构造演化受太平洋构造域和特提斯洋构造域的联合控制.以江南东段NE-SW向景德镇-歙县剪切带和球川-萧山断裂中发育的脆性断层为研究对象,利用野外交切关系和断层滑移矢量反演方法厘定了7期构造变形序列并反演了各期古构造... 详细信息

华南中-新生代构造演化受太平洋构造域和特提斯洋构造域的联合控制.以江南东段NE-SW向景德镇-歙县剪切带和球川-萧山断裂中发育的脆性断层为研究对象,利用野外交切关系和断层滑移矢量反演方法厘定了7期构造变形序列并反演了各期古构造应力场,讨论了断层活动的时代及其动力学.白垩纪至新生代研究区7期古构造应力场分别为:(1)早白垩世早期(136～125Ma)NW-SE向伸展;(2)早白垩世晚期(125～107Ma)N-S向挤压和E-W向伸展;(3)早白垩世末期至晚白垩世早期(105～86Ma)NW-SE向伸展;(4)白垩世中期(86～80Ma)NW-SE向挤压和NE-SW向伸展;(5)晚白垩世晚期至始新世末期(80～36Ma)N-S向伸展;(6)始新世末期至渐新世早期(36～30Ma)NE-SW向挤压和NW-SE向伸展;(7)渐新世早期至中新世中期(30～17Ma)NE-SW向伸展.结合区域地质研究表明,第1期至第4期古构造应力场与古太平洋构造域的板片后撤、俯冲以及微块体(菲律宾地块)间的碰撞作用有关;第5期伸展作用受控于新特提斯构造域俯冲板片后撤,而第6期和第7期古构造应力场主要与印-亚碰撞的远程效应有关.白垩纪至新生代,华南东部受伸展构造体制和走滑构造体制的交替控制.先存断裂的发育可能是导致华南晚中生代走滑构造体制的主要控制因素.

关键词：断层滑移矢量古构造应力场景德镇-歙县剪切带球川-萧山断裂华南中-新生代构造演化构造地质

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