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西藏冈底斯成矿带的斑岩-矽卡岩成矿系统:——来自斑岩矿床和矽卡岩型铜多金属矿床的Re-Os同位素年龄证据

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大地构造与成矿学 2005年第4期29卷 482-490页

作者：李光明刘波屈文俊林方成佘宏全丰成友中国地质科学院矿产资源研究所北京100037 中国地质调查局成都地质矿产研究所四川成都610082 中国地质科学院国家地质实验测试中心北京100037

笔者通过对冈底斯成矿带驱龙、厅宫斑岩铜矿区和甲马、知不拉等矽卡岩型铜多金属矿区的辉钼矿样品进行的Re-0s法同位素定年研究,获得驱龙、厅宫、甲马和知不拉等矿区的精确成矿年龄。4件驱龙斑岩铜矿区辉钼矿样品的Re-Os模式年龄介于(15... 详细信息

笔者通过对冈底斯成矿带驱龙、厅宫斑岩铜矿区和甲马、知不拉等矽卡岩型铜多金属矿区的辉钼矿样品进行的Re-0s法同位素定年研究,获得驱龙、厅宫、甲马和知不拉等矿区的精确成矿年龄。4件驱龙斑岩铜矿区辉钼矿样品的Re-Os模式年龄介于(15.75±0.42)Ma～(16.23±0.90)Ma之间,等时线年龄为(15.99±0.32)Ma;7件厅宫斑岩铜矿矿区辉钼矿样品的Re-Os模式年龄介于(15.5±0.3)Ma～(16.3±0.3)Ma之间,等时线年龄为(15.49±0.36)Ma;在矽卡岩型铜多金属矿区中,7件甲马矿区辉钼矿样品的Re-Os模式年龄介于(15.4±0.2)Ma～(15.5±0.2)Ma之间,等时线年龄为(15.18±0.98)Ma;5件知不拉矿区辉钼矿样品的Re-Os模式年龄介于(16.88±0.28)Ma～(17.06±0.27)Ma之间,等时线年龄为(16.90±0.64)Ma。斑岩铜矿区和矽卡岩型铜多金属矿区所获得的年龄数据基本一致,其年龄明显晚于中生代弧间盆地和碰撞型花岗岩的发育时间,同时矽卡岩型铜多金属矿床在空间上亦分布于斑岩铜矿床的外围。因此笔者认为甲马和知不拉等铜铅锌矿床与冈底斯成矿带新生代晚期大规模成矿形成的斑岩铜钼矿床属于统一的斑岩-矽卡岩成矿系统,是由深源花岗质岩浆的岩浆-热液系统在不同的围岩介质条件成矿的产物。

关键词：斑岩型铜矿矽卡岩型铜多金属矿床 Re^Os年龄喜马拉雅期斑岩-矽卡岩成矿系统

A nuclide identification method ofγspectrum and model building based on the transformer

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Nuclear Science and Techniques 2025年第1期36卷 80-93页

作者： Fei Li Chu-Yang Luo Ying-Zi Wen Sheng Lv feng Cheng Guo-Qiang Zeng Jian-feng Jiang Bing-Hai Li College of Nuclear Technology and Automation Engineering Chengdu University of TechnologyChengdu 610000China Applied Nuclear Technology in Geosciences Key Laboratory of Sichuan Province Chengdu 610000China Department of Physics Universitat Politècnica de CatalunyaBarcelona 08028Spain Airborne Survey and Remote Sensing Center of Nuclear Industry Shijiazhuang 050000China Hebei Key Laboratory of Airborne Detection and Remote Sensing Technology Shijiazhuang 050000China

In current neural network algorithms for nuclide identification in high-background,poor-resolution detectors,traditional network paradigms including back-propagation networks,convolutional neural networks,recurrent neural networks,etc.,have been limited in research on γ spectrum analysis because of their inherent mathematical *** is difficult to make progress in terms of training data requirements and prediction *** contrast to traditional network paradigms,network models based on the transformer structure have the characteristics of parallel computing,position encoding,and deep stacking,which have enabled good performance in natural language processing tasks in recent ***,in this paper,a transformer-based neural network (TBNN) model is proposed to achieve nuclide identification for the first ***,the Geant4 program was used to generate the basic single-nuclide energy spectrum through Monte Carlo simulations.A multi-nuclide energy spectrum database was established for neural network training using random matrices of γ-ray energy,activity,and *** on the encoder–decoder structure,a network topology based on the transformer was built,transforming the 1024-channel energy spectrum data into a 32×32 energy spectrum sequence as the model *** experiments and adjustments of model parameters,including the learning rate of the TBNN model,number of attention heads,and number of network stacking layers,the overall recognition rate reached 98.7%.Additionally,this database was used for training AI models such as back-propagation networks,convolutional neural networks,residual networks,and long shortterm memory neural networks,with overall recognition rates of 92.8%,95.3%,96.3%,and 96.6%,*** indicates that the TBNN model exhibited better nuclide identification among these AI models,providing an important reference and theoretical basis for the practical application of transformers in the qualitative and quantitativ

关键词： Nuclide identification Neural network Transformer

青海祁漫塔格虎头崖矿区花岗岩地球化学特征及构造意义

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地质学报 2014年第1期88卷 72-82页

作者：马圣钞丰成友李大新赵一鸣刘建楠中国冶金地质总局山东正元地质勘查院济南250101 中国地质科学院矿产资源研究所北京100037

位于青海东昆仑祁漫塔格构造带内的虎头崖矿区花岗岩形成于中-晚三叠世，岩性主要由黑云母二长花岗岩、正长花岗岩组成，局部含闪长质暗色包体。岩石高硅、高钾、富碱，SiO2含量为70．71％～77．67％；K2O含量平均为4．7％；Na2O＋K2O为... 详细信息

位于青海东昆仑祁漫塔格构造带内的虎头崖矿区花岗岩形成于中-晚三叠世，岩性主要由黑云母二长花岗岩、正长花岗岩组成，局部含闪长质暗色包体。岩石高硅、高钾、富碱，SiO2含量为70．71％～77．67％；K2O含量平均为4．7％；Na2O＋K2O为7．86％～9．10,4；K2O／Na2O平均为1．36。A／CNK比为1．01，KN／A比为0．86，属于高钾钙碱性系列的微过铝质I型花岗岩类。∑REE含量中等，平均为120．10×10；δEu值0．04～0．47；（La／Yb）N值为1．52～8．06。稀土元素球粒陨石标准化曲线显示Eu负异常、HREE较平坦的右倾“V”型特征。岩体富集LIL和HFS元素，而Ba、Sr、Nb、Ti、P元素明显的负异常。微量元素蛛网图和稀土元素球粒陨石标准化图解显示各花岗岩体具有相同的岩浆源区。结合区域地层岩性特征、A／MF-C／MF图解和岩体微量元素蛛网图，认为虎头崖矿区花岗岩是基性源区部分熔融和地壳物质混合的产物。结合地质特征、构造演化背景、元素判别图解等，认为该地区花岗岩类形成的构造环境为碰撞造山期后阶段。

关键词： I型花岗岩地球化学后碰撞虎头崖祁漫塔格

A PHYB-PIF4-auxin module promotes tomato graft formation in response to elevated ambient temperature

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Horticultural Plant Journal 2025年第1期11卷 227-238页

作者： Xianmin Meng feng Zhang Wencai Yang Qingmao Shang State Key Laboratory of Vegetable Biobreeding Key Laboratory of Horticultural Crop Biology and Germplasm Innovation(Ministry of Agriculture)Institute of Vegetables and FlowersChinese Academy of Agriculture SciencesBeijing 100081China Beijing Key Laboratory of Growth and Developmental Regulation for Protected Vegetable Crops Department of Vegetable ScienceCollege of HorticultureChina Agricultural UniversityBeijing 100193China

Grafting is an effective technique for increasing the resistance of vegetables to biotic and abiotic *** has been widely applied to produce solanaceous and melon *** is an important external factor affecting graft ***,the molecular mechanism by which external ambient temperature affects tomato graft formation remains *** this study,we demonstrated that elevating ambient temperature during grafting to 35℃ for more than 24 h after grafting accelerated vascular *** generated self-or heterografted combinations between phyB1B2 and pif4 loss-of-function mutant and wild-type plants,and were mutants unresponsive to graft formation at elevated ambient *** addition,elevated ambient temperature induced SlPIF4 expression during ***4 directly binds the promoters of auxin biosynthesis genes SlYUCCAs and activates their *** investigation revealed auxin accumulation in the graft junction under elevated ambient *** results illuminate the mechanism by which the PHYB-PIF4-auxin module promotes tomato graft formation in response to elevated ambient temperature.

关键词： Graft formation Tomato Temperature Vascular Auxin

青海格尔木驼路沟喷流沉积型钴(金)矿床的黄铁矿Re-Os定年

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地质学报 2006年第4期80卷 571-576页

作者：丰成友张德全屈文俊杜安道李大新佘宏全中国地质科学院矿产资源研究所北京100037 国家地质实验测试中心北京100037

青海驼路沟矿床是新近发现的中国西北首例独立大型喷流沉积型钴（金）矿床，赋矿岩石为富钠的热水沉积岩——石英钠长石岩。利用Re-Os同位素体系（ICP-MS方法）对不同类型矿石中的7件黄铁矿样品进行了定年，结果表明尽管它们的Re（0．12... 详细信息

青海驼路沟矿床是新近发现的中国西北首例独立大型喷流沉积型钴（金）矿床，赋矿岩石为富钠的热水沉积岩——石英钠长石岩。利用Re-Os同位素体系（ICP-MS方法）对不同类型矿石中的7件黄铁矿样品进行了定年，结果表明尽管它们的Re（0．122×10^-9～8．988×10^-9）和Os（0．00313×10^-9～0．05366×10^-9）的含量很低，但在两种相关图解上分别得到432±23Ma和442±17Ma较好等时线年龄。该Re-Os定年结果不仅进一步厘定区域纳赤台群地层的主体时代为早古生代，而且为确定东昆仑造山带晚奥陶世板块裂解及成矿作用提供了新的重要证据，对深入认识区域成矿规律和探讨地质构造演化具重要意义。

关键词： Re-Os定年黄铁矿钴矿床 SEDEX 驼路沟青海

HMGB2 knockdown ameliorates retinal ganglion cell injury by inhibiting NLRP3 inflammasome activation after retinal ischemia

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International Journal of Ophthalmology(English edition) 2025年第1期18卷 39-50页

作者： Lin-Ping Xue Hai-Song feng Hubei University of Chinese Medicine Wuhan 430065Hubei ProvinceChina Department of Encephalopathy Hubei Provincial Hospital of Traditional Chinese MedicineWuhan 430070Hubei ProvinceChina

AIM:To explore the neuroprotective effects of high mobility group box 2(HMGB2)knockdown on retinal ganglion cells(RGCs)in the retinal ischemia-reperfusion injury(RIRI).METHODS:Oxygen-glucose deprivation(OGD)-injured RGCs from postnatal three-day C57BL/6 mice pups and high intraocular pressure(IOP)-induced RIRI mice were used as cellular and animal models of *** expression of HMGB2 in the retina of RIRI mice and OGD-injured RGCs was detected through reverse transcription-polymerase chain reaction(RT-qPCR)and Western *** effects of HMGB2 silencing on the morphological changes,RGCs survival,and cell apoptosis in mouse retinal tissues were observed through H&E staining,immunofluorescence staining with RNA-binding protein with multiple splicing(RBPMS)antibody,and TUNEL staining,*** viability and apoptosis were examined by CCK-8 and flow cytometry *** levels of proteins associated with NOD-like receptor thermal protein domain associated protein 3(NLRP3)-mediated pyroptosis[NLRP3,Caspase-1,GSDMD-N,interleukin(IL)-1β,IL-18]in vivo and in vitro were measured by Western ***:HMGB2 protein and NLRP3 were upregulated in the retina of RIRI mice and OGD-injured RGCs(P<0.001).The retina was edematous,accompanied by disorganized cell arrangement and decreased thickness of all layers,and obvious vacuoles in ganglion cell ***2 silencing alleviated the reduction in total retinal thickness and the severity of retinal tissue damage as well as suppressed RGC loss and retinal cell apoptosis in RIRI ***-induced RGC apoptosis was ameliorated after downregulation of HMGB2 in *** injection of the AAV-sh-HMGB2 and si-HMGB2 resulted in significantly decrease of NLRP3,Caspase-1,GSDMD-N,IL-1β,and IL-18 protein levels in the retinal tissues of RIRI mice and OGD-injured RGCs,respectively(all P<0.001).CONCLUSION:HMGB2 knockdown protects against RGC apoptosis and pyroptosis after RIRI through suppressing NLRP3 inflammasome activ

关键词： HMGB2 retinal ischemia-reperfusion injury retinal ganglion cell apoptosis pyroptosis NLRP3 mice

Optimization of transverse unidirectional scattering by morphology modification of irregular V-shaped silicon nanoantennas

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Optoelectronics Letters 2025年第3期21卷 129-135页

作者： ZENG Ming ZHAO feng WANG Xianghui School of Electrical and Information Engineering Tianjin University Institute of Modern Optics Tianjin Key Laboratory of Micro-scale Optical Information Science and TechnologyNankai University

A scheme based on irregular V-shaped silicon nanoantennas is proposed to optimize transverse unidirectional scattering under plane wave irradiation. Traditional methods of designing regular shapes offer fewer parameters and higher search efficiency. However, due to the limitations of regular shapes, it is challenging to meet high-precision design requirements. Irregular shape design allows for a broader range of adjustments, but the complexity of shape parameters leads to lower search efficiency and a higher likelihood of converging to local optima.

关键词： A

青海驼路沟钴(金)矿床成矿物质来源的黄铁矿氦氩硫铅同位素示踪

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地质学报 2006年第9期80卷 1465-1473页

作者：丰成友佘宏全张德全李大新李进文崔艳合中国地质科学院矿产资源研究所

为查明青海驼路沟新型独立钴(金)矿床的成因和成矿物质来源,文章对矿区发育的块状、条带状和浸染状黄铁矿矿石进行了黄铁矿流体包裹体氦氩同位素和黄铁矿硫、铅同位素测试。结果表明,不同类型矿石的成矿流体氦、氩同位素组成基本一致,3H... 详细信息

为查明青海驼路沟新型独立钴(金)矿床的成因和成矿物质来源,文章对矿区发育的块状、条带状和浸染状黄铁矿矿石进行了黄铁矿流体包裹体氦氩同位素和黄铁矿硫、铅同位素测试。结果表明,不同类型矿石的成矿流体氦、氩同位素组成基本一致,3He/4He介于0.10~0.31Ra(平均0.21Ra),40Ar/36Ar比值为302~569(平均373),反映钴矿化流体主要来源于在赋矿岩系中深循环的大气降水;矿石黄铁矿硫同位素值分布集中且接近于零,δ34S变化于-4.5‰^+1.5‰,集中在-1.8‰^-0.2‰,显示深部来源;矿石铅以高放射性成因为特征(206Pb/204Pb>19.279、207Pb/204Pb>15.691、208Pb/204Pb>39.627),且自地层围岩→区域早古生代火山岩→矿石依次明显增大,可能指示高放射性成因矿石铅主要是由以深循环大气降水来源为主的热液不断从围岩地层中淋取而来。

关键词：氦氩硫铅同位素成矿物质来源黄铁矿大气降水钴矿床青海驼路沟

新疆维宝多金属矿区辉绿岩脉SIMS年代学和地球化学

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地质学报 2017年第4期91卷 762-775页

作者：钟世华丰成友李大新赵一鸣周建厚刘建楠王辉于淼中国地质科学院矿产资源研究所国土资源部成矿作用与资源评价重点实验室北京100037

东昆仑造山带海西期-印支期岩浆活动强烈,不仅出露大规模的中酸性侵入体,还发育数量较多的辉绿岩脉(墙)。相对于中酸性侵入体,目前对辉绿岩脉(墙)的研究还较薄弱。本文对新疆维宝多金属矿区辉绿岩脉进行了年代学和地球化学研究,确定了... 详细信息

东昆仑造山带海西期-印支期岩浆活动强烈,不仅出露大规模的中酸性侵入体,还发育数量较多的辉绿岩脉(墙)。相对于中酸性侵入体,目前对辉绿岩脉(墙)的研究还较薄弱。本文对新疆维宝多金属矿区辉绿岩脉进行了年代学和地球化学研究,确定了其形成时代,探讨了其形成的构造背景和岩石成因。SIMS锆石U-Pb测年结果显示:维宝多金属矿区辉绿岩形成于227.5±3.3Ma(1σ,MSWD=2.0),为晚三叠世。结合尚未发表的年代学资料,将维宝矽卡岩矿床成矿母岩侵位时间限定于232~227.5Ma之间,这一范围与祁漫塔格矽卡岩多金属矿床成矿母岩就位的峰期年龄一致。主量元素组成上,这些辉绿岩高SiO_2、K_2O,低MgO、Al_2O_3、CaO、FeO和Na_2O,大部分为钙碱性岩;轻重稀土元素分馏强,LaN/YbN>5,大部分样品δEu介于0.73和0.77之间,因此在稀土元素配分曲线上表现为具有明显Eu负异常的右倾型配分模式;在微量元素蛛网图上,相对于原始地幔选择性富集大离子亲石元素(如LREE)、亏损高场强元素(如Ti、P元素等)。尽管维宝多金属矿区辉绿岩地球化学组成具有弧岩浆岩的特征,但根据区域构造演化历史,本文认为维宝矿区辉绿岩形成于后碰撞拉伸环境。其稀土和微量元素所显示的弧岩浆特征可能来源于早期俯冲物质对源区的混染。印支晚期东昆仑祁漫塔格地区幔源岩浆底侵作用导致下地壳部分熔融并分异出长英质岩浆,二者在上升过程中发生混合作用并最终在维宝矿区形成时代接近、稀土和微量元素组成相似的花岗闪长岩和辉绿岩脉。

关键词：辉绿岩 SIMS 矽卡岩矿床维宝祁漫塔格东昆仑