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Acta Geochimica 2019年第2期38卷 277-291页

作者： Lihua Qian Jianqing Lai shugen zhang Lifang Hu Rong Cao Shilong Tao Key Laboratory of Metallogenic Prediction of Nonferrous Metals and Geological Environment Monitoring Ministry of Education School of Geosciences and Info-Physics Central South University

The Longtoushan hydrothermal gold deposit is located in the southwestern region of the Dayaoshan *** is widespread in the Longtoushan gold deposit and is mainly distributed in the rhyolite porphyry and associated cryptoexplosive breccia. The spatial distribution of tourmaline enrichment is similar to that of the gold orebody. Feldspar has been largely replaced by tourmaline in the rhyolite porphyry and cryptoexplosive *** microprobe analysis revealed that tourmalines in the Longtoushan deposit belong mainly to the alkali group and partly to the X-vacant group; they mostly fell in the schorl-dravite series field. Two distinct sets of dominant substitutions were observed: MgFe_(-1) and Al□(NaR2+)-1,where R = Fe, Mg. In addition, minor substitutions include(CaMg)(NaAl)_(-1) and FeAl_(-1). The calculated d11 B value for the mineralizing fluids ranged from-12.8 to-9.7%,which is typical of S-type granites, and boron-enriched fluids predominantly derived from rhyolitic melt. Part of the tourmaline from the rhyolite porphyry crystallized during the magmatic-hydrothermal stage, whereas most tourmalines from the deposit formed in the post-magmatic hydrothermal stage. The tourmalines were deposited from a relatively reduced and acidic fluid system, and the gold predominantly precipitated during the post-magmatic hydrothermal stage in the Longtoushan deposit.

关键词： Longtoushan gold deposit Tourmaline Oreforming fluids Boron isotopes

Formation and destruction processes of upper Sinian oil-gas pools in the Dingshan-Lintanchang structural belt, southeast Sichuan Basin, China

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Petroleum Science 2010年第3期7卷 289-301页

作者： Liu shugen zhang Zhijing Huang Wenming Wang Guozhi Sun Wei Xu Guosheng Yuan Haifeng zhang Changjun Deng Bin State Key Laboratory of Oil and Gas Reservoir Geology and Exploitation Chengdu University of Technology Sichuan610059 China

The lower Cambrian Niutitang Formation hydrocarbon source rocks at the Dingshan- Lintanchang structure in the southeast Sichuan Basin were of medium-good quality with two excellent hydrocarbon-generating centers developed in the periphery areas, with a possibility of forming a medium to large-sized oil-gas field. Good reservoir rocks were the upper Sinian （Dengying Formation） dolomites. The mudstone in the lower Cambrian Niutitang Formation with a good sealing capacity was the cap rock. The widely occurring bitumen in the Dengying Formation indicates that a paleo oil pool was once formed in the study area. The first stage of paleo oil pool formation was maturation of the lower Cambrian source rocks during the late Ordovician. Hydrocarbon generation from the lower Cambrian source rocks stopped due to the Devonian-Carboniferous uplifting. The lower Cambrian source rocks then restarted generation of large quantities of hydrocarbons after deposition of the middle Permian sediments. This was the second stage of the paleo oil pool formation. The oil in the paleo oil pool began to crack during the late Triassic and a paleo gas pool was formed. This paleo gas pool was destroyed during the Yanshan-Himalayan folding, uplifting and denudation. Bitumen can be widely seen in the Dengying Formation in wells and outcrops in the Sichuan Basin and its periphery areas. This provides strong evidence that the Dengying Formation in the Sichuan Basin and its periphery areas was once an ultra-large structural-lithologic oil-gas field, which was damaged during the Yanshan-Himalayan period.

关键词： Sinian oil-gas pool Dingshan-Lintanchang structural belt Sichuan Basin

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地热流体成矿作用分析

矿床地质 1998年第1期17卷 91-96页

作者：张术根中南工业大学资源环境与建筑工程学院

依据地热流体成矿作用基本要素的特殊性、成矿控制因素及其控矿特点，对地壳演化运动的成矿控制及其规律性等方面进行了较系统的分析。研究结果表明，地热流体是特殊的热液成矿作用类型。

关键词：成矿作用控矿因素地热流体热液矿床

南岭中段诸广山复式花岗岩岩石学及其控矿作用

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中国有色金属学报 2014年第6期24卷 1585-1598页

作者：张术根袁莹姚翠霞中南大学有色金属成矿预测教育部重点实验室长沙410083 中南大学地球科学与信息物理学院长沙410083 北京矿产地质研究院北京100012

南岭中段诸广山复式岩体是地洼激烈期(燕山期)花岗质岩浆多次侵入产物。燕山早期主体与燕山晚期补体分别形成于地洼演化剧烈期的前半期和后半期,为古元古代陆壳物质批式部分熔融的产物,但它们动力学环境、演化过程及控矿作用差异明显。... 详细信息

南岭中段诸广山复式岩体是地洼激烈期(燕山期)花岗质岩浆多次侵入产物。燕山早期主体与燕山晚期补体分别形成于地洼演化剧烈期的前半期和后半期,为古元古代陆壳物质批式部分熔融的产物,但它们动力学环境、演化过程及控矿作用差异明显。选择仁化县城口一红山地区为重点研究地段,基于地洼学说研究方法,通过现场地质调查、岩相学、岩石地球化学研究,就诸广山燕山早期主体及燕山晚期补体成岩构造环境、岩石学及控矿作用进行较详细的研究。结果表明,两期次花岗岩随构造动力环境演化,表现出不同的岩石学和地球化学特征,岩体含矿性及控矿性也有差异。燕山早期花岗岩产生于岩石圈膨胀伸展环境,以高硅、富碱、w(K_2O)>w(Na_2O)、准铝质、∑REE含量高为特征,成岩物质主要来源于元古代陆壳,且有幔源岩浆的混入,属A型花岗岩,与Pb-Zn-Sb-Ag矿化有关;燕山晚期花岗岩产生于岩石圈拉张减薄环境,为钙碱性,过铝质,贫Ba、Sr和Eu,属S型花岗岩,经历了高度分异演化和岩浆-流体相互作用过程,是W-Sn-Mo-(Bi)矿床的成矿母岩。

关键词：花岗岩岩石学地球化学构造环境控矿作用诸广山

METALLOGENIC CONDITIONS OF GOLD-BEARING SKARN DEPOSITS ALONG THE MIDDLE-LOW ER REACHES OF THE YANGTZE RIVER

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Journal of Central South University 1996年第1期8卷 78-80页

作者： zhang shugen Wang Dawei(Department of Geology, Central South University ofTechnology, Changsha 410083, China)

The authors discussed the metallogenic conditions of goldbearing skarn deposits along the middlelower Yangtze River reaches. Gold was enriched in mantleoriginated magmas while copper was enriched in crustoriginated magmas. So the enrichment of gold in skarn deposits was decided by the M/C ratios of the intrusive rocks. The distribution of these deposits was controlled not only by the localization of the intrusive rocks which were decided by Mesozoic Eradeveloped largescaled and deepseated faults, but also by the favorable stratigraphic horizons.

关键词： goldbearing skarn deposit metallogenic condition the middlelower Yangtze River reaches

Screening of Potential Functional Pepper Proteins in Response to Pepper Mild Mottle Virus Infection

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Screening of Potential Functional Pepper Proteins in Respons...

宁镇地区燕山期矽卡岩矿床成矿系统稀土元素地球化学研究

中国植物病理学会2023年学术年会

作者： HUA Xia zhang Hao zhang shugen DU Kaitong YAN Qin DENG Xiaomei XING Yongping WANG Zhenquan zhang Qin zhang Junmin ZHOU Tao Department of Plant Pathology China Agricultural University

Pepper( Capsicum annuum L.) is an important economic crop worldwide, and the planting area ranks first among vegetables in *** mild mottle virus(PMMoV), a member of genus Tobamovirus, infects mainly vegetables of Solanaceous and causes serious production loss on *** of functional proteins in response to PMMoV infection will provide potential resistance genes for cultivation of antiviral pepper *** this study, we performed proteomie analyses on upper leaves infected by PMMoV on a susceptible pepper cultivar using Tandem Mass Tags( TMT)*** expressed proteins( DEPs) were analyzed with or without PMMoV *** total number of 677( ～57%) proteins were significantly up-regulated, and 520(～43%) proteins were *** Ontology(GO) enrichment analysis indicated that DEPs were mainly associated with biological processes, such as photosynthesis and light reaction, gene expression, cellular nitrogen compound biosynthetic process, peptide biosynthetic process, and amide biosynthesis *** addition, several essential pathways including Hippo signaling pathway, ribosome,spliceosome, glycolysis/gluconeogenesis were significantly enriched through the Kyoto Encyclopedia of Genes and Genomes(KEGG) pathway analyses, which are consistent with the above analysis results.

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中国稀土学报 2010年第5期28卷 626-632页

作者：张术根李桂秀石得凤韩世礼中南大学地学与环境工程学院湖南长沙410083

通过宁镇地区燕山期矽卡岩矿床成矿系统的稀土元素特征研究,了解了矽卡岩矿床成矿系统的稀土元素地球化学演化规律特征及其制约机制,为矽卡岩型多金属矿床成矿规律及成矿预测研究提供新的地质地球化学信息依据。研究表明,矽卡岩矿床成... 详细信息

通过宁镇地区燕山期矽卡岩矿床成矿系统的稀土元素特征研究,了解了矽卡岩矿床成矿系统的稀土元素地球化学演化规律特征及其制约机制,为矽卡岩型多金属矿床成矿规律及成矿预测研究提供新的地质地球化学信息依据。研究表明,矽卡岩矿床成矿系统稀土演化规律为:矽卡岩期,干矽卡岩阶段到湿矽卡岩阶段稀土组分含量增加;矽卡岩期晚期到热液期早期降低;热液期,汽成热液氧化物阶段到高中温硫化物阶段增加,到中低温硫化物阶段降低。演化规律主要是受自身富集稀土元素的强度、流体含矿性、运移分配及成矿的物理化学条件的影响。矽卡岩矿床成矿系统主要矽卡岩化的发育及其分带性所具有成矿专属性等特点,都为进一步寻找矽卡岩型多金属矿床提供新的地质地球化学信息。

关键词：矽卡岩矿床多金属矿成矿机理稀土元素聚类分析

闽中丁家山铅锌矿床同位素地球化学及其地质意义

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矿床地质 2013年第5期32卷 1003-1010页

作者：石得凤张术根韩世礼徐忠发湖南科技大学土木工程学院湖南湘潭411201 中南大学有色金属成矿预测教育部重点实验室地球科学与信息物理学院湖南长沙410083 华东有色地质调查集团江苏南京210007

通过铅、硫、铷、锶同位素地球化学特征的系统分析,对闽中丁家山铅锌矿床的成矿物质来源、成矿时代及矿床成因进行了深入研究。围岩全岩及矿石内方铅矿的Pb同位素变化范围较宽,方铅矿的^206Pb/^204Pb比值在18.182-18.605之间,^207Pb/^20... 详细信息

通过铅、硫、铷、锶同位素地球化学特征的系统分析,对闽中丁家山铅锌矿床的成矿物质来源、成矿时代及矿床成因进行了深入研究。围岩全岩及矿石内方铅矿的Pb同位素变化范围较宽,方铅矿的^206Pb/^204Pb比值在18.182-18.605之间,^207Pb/^204Pb比值在15.010-15.932之间,^208Pb/^204Pb比值在38.331-39.666之间,具有明显的壳-幔混合来源特征,可能由龙北溪组地层和燕山期重熔型花岗岩共同提供。黄铁矿、磁黄铁矿、闪锌矿、方铅矿的δ34S组成为-1.7‰-5.6‰,平均值为2.7‰,具有向正值偏移的塔式分布特征;系统δ34S初始值为3.97‰,深源硫特征明显,说明硫由燕山期重熔型花岗岩提供。成矿期的石英铷-锶等时线年龄为（146.15±3.95）Ma,成矿时间属燕山早期第三阶段。以上结果进一步证实,丁家山铅锌矿床为马面山群龙北溪组上段经区域变质的富钙质沉积岩与燕山期重熔型花岗岩发生接触交代作用,形成的矽卡岩型矿床。

关键词：地球化学成矿物质来源成矿时代矽卡岩型矿床丁家山铅锌矿

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推拿联合葛根素治疗颈性眩晕的疗效观察

按摩与康复医学 2010年第11期1卷 30-31页

作者：张树根上海市黄浦区中西医结合医院上海200010

目的：探讨推拿联合葛根素治疗颈性眩晕的临床疗效。方法：针对颈性眩晕的发病机制及相关病因，运用中医辩证将65例颈性眩晕患者分为：①肝火上炎型20例；②风痰夹瘀型23例；③气血亏虚夹瘀型：22例。各组患者均以400mg葛根素注射液加5... 详细信息

目的：探讨推拿联合葛根素治疗颈性眩晕的临床疗效。方法：针对颈性眩晕的发病机制及相关病因，运用中医辩证将65例颈性眩晕患者分为：①肝火上炎型20例；②风痰夹瘀型23例；③气血亏虚夹瘀型：22例。各组患者均以400mg葛根素注射液加5％葡萄糖注射液500ml静滴，1次／d，1周为一个疗程。间隔2d后行第二个疗程。同时联合推拿疗法。在治疗期间停用其他扩血管药物，用药两个疗程后进行疗效评定。结果：肝火上炎组共20例，其中显效有15例，有效有3例，无效有2例，总有效率为90．00％；风痰夹瘀组共23例，其中显效有17例，有效有3例，无效有3例，总有效率为86．96％；气血亏瘀组共22例，其中显效有5例，有效有11例，无效有6例，总有效率为72．73％。结论：根据颈性眩晕的相关病因，针对性地采用推拿联合葛根素治疗，取得了理想的临床效果，值得临床大力推广应用。

关键词：颈性眩晕病因病机推拿葛根素

以Fe_2O_3作晶核剂的尾矿玻璃陶瓷晶化研究

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硅酸盐通报 1999年第4期18卷 76-80页

作者：张术根韦奇王大伟中南工业大学

运用差热分析（ＤＴＡ）、扫描电镜（ＳＥＭ）、Ｘ射线衍射（ＸＲＤ）、能谱分析（ＥＤＡＸ）等测试手段，研究了以Ｆｅ２Ｏ３作晶核剂时ＣａＯ－Ａｌ２Ｏ３－ＳｉＯ２系统尾矿玻璃陶瓷析晶特征。结果表明，Ｆｅ２Ｏ３降低了玻璃整体析... 详细信息

运用差热分析（ＤＴＡ）、扫描电镜（ＳＥＭ）、Ｘ射线衍射（ＸＲＤ）、能谱分析（ＥＤＡＸ）等测试手段，研究了以Ｆｅ２Ｏ３作晶核剂时ＣａＯ－Ａｌ２Ｏ３－ＳｉＯ２系统尾矿玻璃陶瓷析晶特征。结果表明，Ｆｅ２Ｏ３降低了玻璃整体析晶温度，并在热处理时诱导玻璃分相，从而促进成核和晶相生长。

关键词：玻璃陶瓷分组成核析晶氧化铁晶核剂晶化