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| 1 | The antiviral and antimicrobial activities of licorice, a widely-used Chinese herb显示文摘Licorice is a common herb which has been used in traditional Chinese medicine for centuries.More than 20 triterpenoids and nearly 300 flavonoids have been isolated from licorice. Recent studies have shown that these metabolites possess many pharmacological activities, such as antiviral,antimicrobial, anti-inflammatory, antitumor and other activities. This paper provides a summary of the antiviral and antimicrobial activities of licorice. The active components and the possible mechanisms for these activities are summarized in detail. This review will be helpful for the further studies of licorice for its potential therapeutic effects as an antiviral or an antimicrobial agent. | Liqiang Wang Rui Yang Bochuan Yuan Ying Liu Chunsheng Liu | 2015 | Acta Pharmaceutica Sinica B2015，5，4： | 64 |
| 2 | Research advances in the Mesozoic tectonic regimes during the formation of Jiaodong ore cluster area显示文摘在诺思中国的东方区域在中生代时代在 Jiaodong 矿石簇区域和相关构造政体转变把构造政体的进展基于研究,在这篇论文,我们首先总结要求后面被学习的一些关键问题。然后,我们建议一条途径到处理这些问题。在 Jiaodong 矿石的金存款聚类区域,这被知道,它具有不同矿化作用式样,空间 istributions 和地质的背景,可能作为从在中生代的至少一个地质的事件的结果。到现在为止,特别在上述事件的 geodynamic 机制上,关于时间的进化和空间迁居顺序的这种研究是远非足够的。而且,描述行动模式和构造动态政体的时间空间的框架并且提出每构造动态政体的相对贡献因为 metallogensis 是静止的质问到地质学家在 Jiaodong 的形成上学习的份量上矿石簇区域。根据地区性的构造分析,结构的动力学,观察和矿化作用网络的探索的解释,我们建议有一些的一个 geological-physical-chemical 模型抑制从全面分析发源。我们然后使用这个模型模仿结构的变丑,热运输,液体流动和化学反应的联合过程。获得的结果显示模型在进一步在 Jiaodong 矿石簇区域并且在进一步理解集体 metallogensis 的性质分析构造政体的时间空间的进化小道是有效的。 | DENG Jun YANG Liqiang GE Liangsheng WANG Qingfei ZHANG Jing GAO Bangfei ZHOU Yinghua JIANG Shaoqing | 2006 | Progress in Natural Science:Materials International2006，16，8： | 51 |
| 3 | Coupling Effects on Gold Mineralization of Deep and Shallow Structures in the Northwestern Jiaodong Peninsula, Eastern China显示文摘为在金矿化作用上理解可能的深层的过程和 geodynamicconstrains,全面物理化学并且金矿化作用的 geochemical 研究在这篇论文从 Jiaodong 半岛的西北的部分在 metallogenicepoch 期间在 paleo 岩石圈框架以内被承担了。尽管它被 post-metallogenictectonic 运动附加了并且改过, thepaleo 外壳的一幅一般图象被仍然是。金矿存款通常在本地人发生高举,坡度系上带子展示拐弯从对陡峭在花岗石变形的接触变质带轻轻,亲戚 Curler 等温的接口的坡度地区高举,等深线被等温线垂直地切的莫霍断绝和区域的消沉。金矿化作用和石版印刷开始被高温度,低压力和热流动的高力量描绘。从 0.8 ~ 4.5 km 的矿化作用范围的深度。在 metallogenic 时代的花岗石的建筑群的最高的接口的深度是大约 3 km。在有到 19.5 km 的深度结束的上地壳的底部有低速度的层(LVL ) ,它可以是在外壳中的一条分开带。LVL 的外观显示 paleo 过高热的液体的存在或熔融的岩浆储源的遗物,它反映在 diagenetic 和 metallogenic 时代和 Tanlu 断层带砍的走向滑倒的重叠效果期间的在外壳以内的部分融化。莫霍的沉淀可能被归因于在 NorthChina 和扬采·布洛克之间的 NW-SE 大陆碰撞的联合过程, Tanlu 差错的走向滑倒运动在 Jiaodong 半岛的西北的部分伴随了披风岩浆的 withunderplating。在披风的 plating 下面,岩浆可以导致部分融化并且向上做花岗石岩浆转移。这为 metallogenic 材料从的迁居是有利的对深对浅被充实形成存款。联合在 Tanlu 差错的走向滑倒之间的相互作用,在披风岩浆的 plating 下面,在外壳,和过高热的液体以内的部分融化,等等可以是在 metallogenic 系统控制金矿化作用和空间结构的重要因素。 | YANG Liqiang DENG Jun WANG Qingfei ZHOU Yinghua | 2006 | Acta Geologica Sinica(English Edition)2006，80，3： | 42 |
| 4 | The Structure of Ore-controlling Strain and Stress Fields in the Shangzhuang Gold Deposit in Shandong Province,China显示文摘Shangzhuang 改变岩石的类型金牌矿石存款位于中间的片断并且在 Jiaodong 金省的西北的部分由 Wang'ershan 差错地区控制了,中国。在 Shangzhuang 存款的变丑进化,紧张的结构和压力地和它的控制矿石的效果在这份报纸被讨论。变丑进化主要经历了四个阶段,这被揭示:早可锻的变丑,第二 NE 惹人注目水平简单砍,第三 NE 惹人注目的压缩砍和最后的 NW 惹人注目的压缩。矿化作用发生在在的第三个阶段期间最大的主要压力逐渐地从 NE 的 transited 到 NW。 3-D 压力地的数字模拟证明在最大的主要压力是NE惹人注目的条件上,在差错地区的破裂发展被赞成,当时当最大的主要压力是NW惹人注目的时,差错地区是相对 extensional 和它对形成矿石的液体的流入和炮兵阵地合适。压缩砍紧张地被类型结构在矿化作用期间描绘,积极的花结构,等等。Orebodies 等距离地主要位于 dilatational 空格,它在不可分的有压缩性的情形是分布式的。并且在差错态度变化的地方, dilatational 空格被开发或砍联合系统发展。在全面压缩砍应力地里,紧张地在多重规模忍受自我类似,包括 orebody,矿石存款和 orefield。结构的自我类似在各种各样的规模在一样的规模和破裂的类似的形状包括破裂的 subequidistant 分发。由于特殊地质的结构,然而, orebodies 主要在 Shangzhuang 存款位于挂的墙它与在 Jiaodong 金省的大多数存款不同。在存款的控制矿石的压力和紧张地的分析为寻求的沉积物提供一个重要基础。 | DENG Jun WANG Qingfei YANG Liqiang ZHOU Lei GONG Qingjie YUAN Wanming XU Hao GUO Chunying LIU Xiangwei | 2008 | Acta Geologica Sinica(English Edition)2008，82，4： | 41 |
| 5 | Research on trusted computing and its development显示文摘Trusted computing is a novel technology of information system security. It has become a new tide in worldwide information security area and achieved inspiring accomplishment. In China, the initiative research of trusted computing is not late, and the achievements are plentiful and substantial. Our country is in the front rank of the world in trusted computing. This paper comprehensively illustrates the recent development in theory and technology of trusted computing, introduces some improvements in trusted computing in our country, and proposes our opinions and viewpoints towards the existing problems in trusted computing and its future development. | SHEN ChangXiang ZHANG HuanGuo WANG HuaiMin WANG Ji ZHAO Bo YAN Fei YU FaJiang ZHANG LiQiang XU MingDi | 2010 | Science China(Information Sciences)2010，53，3： | 37 |
| 6 | Sediment-hosted Pb-Zn Deposits in Southwest Sanjiang Tethys and Kangdian Area on the Western Margin of Yangtze Craton显示文摘Yangtze Craton 的西方的边缘作为重要招待沉积的基础金属的总数簇被知道,特别为在中国的 PbZn 存款,例如 Jinding, Daliangzi, Tianbaoshan, Kuangshanchang 和 Qinlinchang 存款。与在世界上的经典 MVT 存款比较,基于招待沉积的 Pb-Zn 存款的基本地质学,这份报纸集中于这存款的 temporalspatial 分发进一步讨论它的大规模矿化作用和构造进化历史。在 SW Sanjiang Thethys, Jinding 沉积物典型地在沙岩和忍受角砾岩的沙岩主要是控制差错、招待的戳,而 MVT 类型存款被岩性学控制并且为招待碳酸盐的岩石与强壮的偏爱差错 / 破裂。最重要地, Jinding PbZn 沉积物不同于它在一个大陆人碰撞地区以内在强烈使变形的低岬盆在被形成的招待沉积的 PbZn 存款的另外的类型。在 Kangdian 区域,招待沉积的 PbZn 存款沿着 Yangtze Craton 在大陆人 orogenic 带的方面上在 extensional 盆被形成。与经典 MVT 存款相比,在 Kangdian 区域的 PbZn 存款属于 MVT 存款。这份报纸是重要的不仅因为招待沉积的 PbZn 的开始的解释扔而且因为利用大贱金属在大沉积目标区域扔。 | WANG Changming DENG Jun ZHANG Shouting XUE Chunji YANG Liqiang WANG Qingfei SUN Xiang | 2010 | Acta Geologica Sinica(English Edition)2010，84，6： | 33 |
| 7 | Metallogenic epoch and genesis of the gold deposits in Jiaodong Peninsula, Eastern China: a regional review显示文摘金存款被多来源,重迭,大规模和时间空间的集中在 Jiaodong 半岛描绘,东方中国。在这篇论文,我们在 metallogenic 年表和金存款的开始上考察历史和学习的发展,总结附加 metallogenesis 的主要特征,提供中生代复杂 metallogenic 系统的证据,并且从一个地区性的看法为 Jiaodong 金存款簇的进一步的研究指出一些问题。尽管金存款在基因类型,形成矿石的材料和地质的背景是不同的,我们的研究显示形成矿石的材料的累积和炮兵阵地 temporally 空间地被专注于大规模,和 Jiaodong 金存款的主要 metallogenic 时代在中生代被集中。Metallogenic 年表和 geological-geochemical 数据显示有金矿化作用的二个时期在 Jiaodong 分别地发生在 130-110 妈和 90-80 妈矿石簇。从 polygenetic 矿化作用的重迭的金存款簇结果,和进一步的学习被需要调查中生代复杂 metallogenic 系统的形成和进化。 | YANG Liqiang DENG Jun GE Liangsheng WANG Oingfei ZHANG Jing GAO Bangfei J IANGShaoqing XU Hao | 2007 | Progress in Natural Science:Materials International2007，17，2： | 30 |
| 8 | Effects of clay and calcium ions on coal flotation显示文摘The microflotation of three single minerals,mixed coal–kaolinite and mixed coal–montmorillonite were examined to study the effects of clay and calcium ions on coal flotation.The results show that the ash content of flotation concentrate increases by 3%in the presence of clay minerals,and the ash content would further increase by 3%in co-presence of clay minerals and high concentration of Ca2+.Scanning electron microscope(SEM)images and elemental spectrum analysis indicate that fne clay particles that coat on the coal surface,which is called slime coating,can affect the coal flotation.The slime coating would be induced much more easily in the presence of Ca2+. | Zhang Zhijun Liu Jiongtian Xu Zhiqiang Ma Liqiang | 2013 | International Journal of Mining Science and Technology2013，23，5： | 24 |
| 9 | Clinical features and outcomes of diffuse large B-cell lymphoma based on nodal or extranodal primary sites of origin:Analysis of 1,085 WHO classified cases in a single institution in China显示文摘Objective: To explore the clinicobiologic features and outcomes of diffuse large B-cell lymphoma(DLBCL)patients in China according to the primary site.Methods: A total of 1,085 patients diagnosed with DLBCL in National Cancer Center/Cancer Hospital, Chinese Academy of Medical Sciences and Peking Union Medical College during a 6-year period were enrolled. Their clinical characteristics and outcomes were analyzed according to the primary site.Results: In the 1,085 patients, 679(62.6%) cases were nodal DLBCL(N-DLBCL) and 406 cases(37.4%) were extranodal DLBCL(EN-DLBCL). The most common sites of N-DLBCL were lymphonodus(64.8%), Waldeyer's ring(19.7%), mediastinum(12.8%) and spleen(2.7%), while in EN-DLBCL, stomach(22.4%), intestine(16.0%),nose and sinuses(8.9%), testis(8.4%), skin(7.9%), thyroid(6.9%), central nervous system(CNS)(6.4%), breast(5.7%), bone(3.4%), and salivary gland(2.7%) were most common. N-DLBCL patients tend to present B symptoms, bulky disease, and elevated LDH more often, while age >60 years, extranodal sites >1, Ann Arbor stage I or II, bone marrow involvement, and Ki-67 index >90% were usually seen in EN-DLBCL. The 5-year overall survival(OS) rate and progression-free survival(PFS) rate for all patients were 62.5% and 54.2%. The 5-year OS rate for patients with N-DLBCL and EN-DLBCL were 65.5% and 56.9%(P=0.008), and the 5-year PFS were57.0% and 49.0%(P=0.020). Waldeyer's ring originated DLBCL possessed the highest 5-year OS rate(83.6%) and PFS rate(76.9%) in N-DLBCL. The top five EN-DLBCL subtypes with favorable prognosis were stomach,breast, nose and sinuses, lung, salivary gland, with 5-year OS rate: 70.3%, 69.6%, 69.4%, 66.7% and 63.6%,respectively. While CNS, testis, oral cavity and kidney originated EN-DLBCL faced miserable prognosis, with 5-year OS rate of 26.9%, 38.2%, and 42.9%.Conclusions: In our study, primary sites were associated with clinical characteristics and outcomes. Compared with EN-DLBCL, N-DLBCL had better prognosis. | Yuankai Shi Ying Han Jianliang Yang Peng Liu Xiaohui He Changgong Zhang Shengyu Zhou Liqiang Zhou Yan Qin Yongwen Song Yueping Liu Shulian Wang Jing Jin Lin Gui Yan Sun | 2019 | Chinese Journal of Cancer Research2019，31，1： | 19 |
| 10 | SHRIMP zircon U-Pb ages and tectonic implications for Indosinian granitoids of southern Zhuguangshan granitic composite, South China显示文摘The large southern Zhuguangshan granitic batholith composite consists of granites with ages varying from the Caledonian through Indosinian to Yanshanian. Based on K-Ar dating data, the ages of the major parts of this composite were previously regarded as Yanshanian. In this study, the SHRIMP zircon U-Pb dating method has been adopted for six plutons, Ledong, Longhuashan, Dawozi, Zhaidi, Baiyun and Jiangnan, in the southern Zhuguangshan composite, in which the four plutons other than Baiyun and Jiangnan were previously regarded as Yanshanian granites. Magmatic zircons from these six plutons, dated by this study, have yielded ages of 239±5 Ma (MSWD = 2.5), 239±5 Ma (MSWD = 2.5), 239±2 Ma (MSWD = 1.7), 239±4 Ma (MSWD = 3.2), 231±2 Ma (MSWD = 0.81) and 231±3 Ma (MSWD = 1.8), respectively. The results indicate that these plutons were formed by early Indosinian magmatism. Geochemical characteristics suggest that these granites were formed in an extensional tectonic environment. Therefore, the Indosinian period granites in the southern Zhuguangshan composite were formed by partial melting of the Paleo-Mesoproterozoic crustal components during the collapse of thickened lithosphere after the collision between the South China and Indosinian plates. | DENG Ping REN JiShun LING HongFei SHEN WeiZhou SUN LiQiang ZHU Ba TAN ZhengZhong | 2012 | Chinese Science Bulletin2012，57，13： | 19 |
| 11 | Encapsulating segment-like antimony nanorod in hollow carbon tube as long-lifespan,high-rate anodes for rechargeable K-ion batteries显示文摘K-ion battery (KIB) is a new-type energy storage device that possesses potential advantages of low-cost and abundant resource of potassium.To develop advanced electrode materials for accommodating the large size and high activity of potassium ion is of great interests.Herein,a segment-like antimony (Sb) nanorod encapsulated in hollow carbon tube electrode material (Sb@HCT) was prepared.Beneficial from the virtue of abundant nitrogen doping in carbon tube,one-dimensional and hollow structure advantages,Sb@HCT exhibits excellent potassium storage properties:in the case of potassium bis(fluorosulfonyl)imide (KFSI) electrolyte,Sb@HCT displays a reversible capacity of up to 453.4 mAh·g^-1 at a current density of 0.5 A·g^-1 and good rate performance (a capacity of 211.5 mAh·g^-1 could be achieved at an ultrahigh rate of 5 A·g^-1).Additionally,Sb@HCT demonstrates excellent long-cycle stability at a current density of 2 A·g^-1 over 120 cycles.Meanwhile,electrolyte optimization is an effective strategy for greatly improving electrochemical performance.Through ex-situ characterizations,we disclosed the potassiation of Sb anode is quite reversible and undergoes multistep processes,combining solid solution reaction and two-phase reaction. | Wen Luo Feng Li Weiran Zhang Kang Han Jean-Jacques Gaumet Hans-Eckhardt Schaefer Liqiang Mai | 2019 | Nano Research2019，12，5： | 18 |
| 12 | Shear Alteration, Mass Transfer and Gold Mineralization: An Example from Jiaodong Ore Deposit Concentrating Area, Shandong, China显示文摘Taking the gold ore deposit concentrating area of Jiaodong area in Shandong, China for an example, based on geological analysis, and applying Gresens’ equation, Grant’s isocon diagram and O’hara microelement calculation method, a thorough study on shear alteration, mass transfer and gold mineralization was carried out. The authors also made mathematic simulation and geochemical analysis. The work reveals temporal spatial changing regularities of temperature field and velocity field of fluids, and also reveals fluid transport chemical reaction coupling metallogenic dynamics of the Jiaojia gold ore concentrating area. During shear alteration process of the Jiaodong gold ore concentrating area, all kinds of components transferred with different amounts, fluid rock ratio was rather high and volume strain was of dilation type. Fast flow of ore forming fluid favors the occurrence of mixed fluid. Shear fractured zones are places where there was strong transportation reaction coupling mineralization. Ore bodies were located in dilation space of shear structure where there was the greatest fluid flux. After the emplacement of the rock body, a convex heat field was formed around the rock body. It is one of the main metallogenic forces. The major reason for mineralization is the mobilization, migration and enrichment of ore forming elements induced by shear compressive extensional tectonism. Inclusion gold dominant low grade ores were formed in the early ore forming stage, while high grade ores, which contained fissure gold and polymetallic veinlets, were formed in late ore forming stage. | Deng Jun Zhai Yusheng Wang Jianping Faculty of Earth Sciences and Mineral Resources, China University of Geosciences, Beijing 100083, China Yang Liqiang Institute of Geophysics, Chinese Academy of Sciences, Beijing 100101, China Fang Yun Faculty of | 2000 | Journal of Earth Science2000，19，3： | 18 |
| 13 | Real-time and reliability analysis of time-triggered CAN-bus显示文摘Real-time performance and reliability are two most important issues in applications of time-triggered controller area network (CAN) bus systems at present. A scheduling matrix of time-triggered CAN-bus system is established using average-loading algorithm. Periodic messages are guaranteed to transmit without delay by distributing independent transmission windows within the system matrix. Considering the traditional CAN-bus transmission mechanism and the time-triggered feature, an algorithm is improved to calculate the worst-case delay of event-triggered messages in time-triggered CAN-bus systems. The failure probability is calculated for event-triggered messages whose worst-case delay exceeds their deadlines. Different levels of redundant structures of CAN-bus circuits are analyzed and the maintenance management is proposed to improve the system reliability. Finally, the reliabilities of different structures are calculated and the influences of maintenance on the system reliability are analyzed. | Xia Jiqiang Zhang Chuansen Bai Ronggang Xue Liqiang | 2013 | Chinese Journal of Aeronautics2013，26，1： | 17 |
| 14 | Quasi-real-time simulation of rotating drum using discrete element method with parallel GPU computing显示文摘Real-time simulation of industrial equipment is a huge challenge nowadays. The high performance and fine-grained parallel computing provided by graphics processing units (GPUs) bring us closer to our goals. In this article, an industrial-scale rotating drum is simulated using simplified discrete element method (DEM) without consideration of the tangential components of contact force and particle rotation. A single GPU is used first to simulate a small model system with about 8000 particles in realtime, and the simulation is then scaled up to industrial scale using more than 200 GPUs in a 1D domain-decomposition parallelization mode. The overall speed is about 1/11 of the real-time. Optimization of the communication part of the parallel GPU codes can speed up the simulation further, indicating that such real-time simulations have not only methodological but also industrial implications in the near future. | Ji Xu Huabiao Oi Xiaojian Fang Liqiang Lu Wei Ge Xiaowei Wang Ming xu Feiguo Chen xianfeng He Jinghai Li | 2011 | Particuology2011，9，4： | 16 |
| 15 | An experimental study on variation of thermal fields during the deformation of a compressive en echelon fault set显示文摘温度变化在变丑期间一在在一件岩石样品的军队飞机差错集合压缩被表面测量系统 th 测量多点的铂电阻温度计和一个红外线的 theirnal 图象系统。二个系统获得的大小与对方一致,显示在 then-nd 领域的时间空间的变化和应力和紧张的变化之间的一种关系。在岩石样品的改变的 sfructurd 位置,温度升起是不同的,暗示在这些位置的不同压力分布。在实验,样品的 defoirmation 过程包括了三个阶段:有弹性的变丑,粘住滑倒,和 nipture。Grrespondingly,温度的变化过程也有三个阶段,其各个有它的 oq 温度升起侧面。并且热放射领域显示出一个类似的过程。这些现象意味着在变丑的 sJl 阶段升起的温度的主导的机制是不同的。试验性的结果 prode 由使用卫星的数据的当前的差错活动的学习的一个物理基础红外线的图象。 | LIU Peixun MA Jin LIU Liqiang MA Shengli CHEN Guoqiang | 2007 | Progress in Natural Science:Materials International2007，17，3： | 14 |
| 16 | Observation of mega-dune evaporation after various rain events in the hinterland of Badain Jaran Desert, China显示文摘The formation mechanisms of the mega-dunes and lakes in the hinterland of Badain Jaran Desert,China,is the focus of extensive academic research in the field of geoscience,and an often debated topic is whether atmospheric precipitation on the mega-dune can infiltrate to recharge groundwater.In the present study,the probability distribution functions and the return period analysis of extreme daily precipitation based on long-term precipitation records for the southern margin of Badain Jaran Desert and 2-year observation of hinterland precipitation were used to classify precipitation in the desert region.The data of automatic weather station and eddy covariance system in the desert hinterland were used to analyze evaporation on the mega-dune surface after various rain events.The results showed that the rain events in the desert could be divided into three categories.The first is conventional precipitation(CP),which is below 5 mm,accounting for roughly 90%of all rain events in the desert.The second and third categories are ordinary annual maximum(OAM)and extreme precipitation(EP),in which precipitation is roughly 20 mm and more than 40 mm,respectively.The atmospheric precipitation of CP and OAM evaporated from the megadune surface in 1–3 days and 3–4 weeks,respectively.Following an EP event,the mega-dune evaporation was negatively influenced by the upper dry sand layer,and a lengthy period was required for its complete removal.The accumulative evaporation and accumulative precipitation of all three types of rain events indicated that local atmospheric precipitation had no significant contribution to recharging the groundwater system in the hinterland of Badain Jaran Desert.This research will benefit comprehensive elucidation of the formation mechanism of lakes in the hinterland of Badain Jaran Desert. | Ning Ma Naiang Wang Liqiang Zhao Zhenyu Zhang Chunyu Dong Shiping Shen | 2014 | Chinese Science Bulletin2014，59，2： | 14 |
| 17 | World-class Xincheng gold deposit: An example from the giant Jiaodong gold province显示文摘The Jiaodong gold deposits are currently the most important gold resources(with Au reserves of>4000 t) in China,and the leading gold-producing country globally(with Au production of ~428 t in2013).Jiaodong is also considered as perhaps the only world-class to giant gold accumulation on the planet where relatively young gold ores(ca.130-120 Ma) were deposited in rocks that are 2 Ga older.The Xincheng world-class high-grade gold deposit,with a proven reserve of >200 t gold,is one of the largest deposits in the giant gold province of the Jiaodong Peninsula.It is located in the northwestern part of the jiaobei Uplift,and hosted by ca.132-123 Ma Xincheng quartz monzonites and monzogranites.Ore zones are structurally controlled by the NE-trending and NW-dipping Jiaojia Fault and subsidiary faults,and are mainly restricted to the footwall of the fault.The dominant disseminated- and stockworkstyle ores are associated with strong sericitization,silicification,sulfidation and K-feldspathization,and minor carbonate wallrock alteration halos.The four mineralization stages are pyrite-quartz-sericite(stage 1),quartz-pyrite(stage 2),quartz-polysulfide(stage 3) and quartz-carbonate(stage 4).Gold occurs dominantly as electrum,with lesser amounts of sulfide-hosted native gold and rare native silver and argentite,normally associated with pyrite,chalcopyrite,galena and sphalerite:the latter with proven resources of about 105 t Ag,713 t Cu,and 5100 t S.There are three types of ore-related fluid inclusions:type 1 aqueous-carbonate(H_2O-CO_2),type 2aqueous(liquid H_2O+vapor H_2O),and type 3 CO_2(liquid CO_2 and vapor CO_2) inclusions.Homogenization temperatures range from 221 to 304℃ for type 1 inclusions,with salinities of 2.4-13.3 wt.%NaCl eq.,and bulk densities of 0.858-1.022 g/cm^3.The δ^(34)S_(CDT) values of hydrothermal sulfides are 4.3-10.6‰and δ^(18)O values of hydrothermal quartz have a median value of 13.0‰.δD values of fluid inclusions in hydrothermal quartz have a median value of-75‰.Calculated δ^(18)Owater has a median value of 5.2‰.The timing of gold mineralization at the Xincheng gold deposit is younger than 123±1 Ma,and likely between 120.9 and 119.9 Ma.A minerals system genetic model for the probable epizonal orogenic Xincheng deposit suggests an initial medium temperature,CO_2-rich,and low salinity H_2O-CO_2 deeply sourced metamorphic ore fluid associated with dehydration and decarbonization of subducting Paleo-Pacific lithosphere.The Jiaojia Fault constrained the migration of ore-forming fluids and metals at the brittle-ductile transition.Fluid immiscibility,caused by episodic pressure drops,led to significant high-grade gold deposition in the giant Xincheng gold deposit. | Liqiang Yang Jun Deng Ruipeng Guo Lin'nan Guo Zhongliang Wang Binghan Chen XudongWang | 2016 | Geoscience Frontiers2016，7，3： | 14 |
| 18 | The Kiloton Class Jiaojia Gold Deposit in Eastern Shandong Province and Its Genesis显示文摘当以前建议了,在东方山东省的 Jiaojia 区域的最近的深勘探结果显示 Jiaojia 矿石域几单个金沉积物创作了实际上是极端大的金沉积物。这沉积物盖住 ∼40 km 2, 的一个区域并且由 Jiaojia 差错和它的第二等的差错显示出结构的控制。金 orebodies 通常沿着一样的矿化作用改变带,和主要 orebodies 发生与对方一起交叉或展出平行或重叠的分布。这沉积物的储备被估计是 1,黄金的 200t,是超过 1000t 黄金的第一金沉积物在中国保留。没有。在页岩深的 Sizhuang 矿石块的 I-1 orebody 使金储备保持比 350 t 大,否则 29% 总数保留列在后面由没有。我在有超过 150t 黄金的 Matang-Jiaojia 矿石块的 orebody 保留。这存款主要在 Jiaojia 差错的矿脉基卒下盘发生,并且在矿化作用,改变和结构介绍 zoned 模式。强烈使矿物化的地区强烈同意改变了并且构造地断裂了地区。这些 orebodies 显示象 strataform 一样, veinlike 或透镜的形状,并且通常显示出外面拧并且重现的特征,分叉并且收敛,膨胀并且缩小。orebodies 通常与剧降变化从沿着差错罢工变化的职务并且在轻轻的地点发生对陡峭轻轻。主要 orebodies 与控制矿石的差错的主要飞机平行,并且趋于从表面轻轻到深。orebodies 主要跳入到西南,与跳入 45 °-60° 的角度。控制矿石的差错的主要飞机附近的 Orebodies 比那些有更多的金资源离开主要差错地区。orebodies 的观点深度通常比沿着它的罢工方向的长度大;orebodies 变得厚,金等级从浅区域变得低到深区域。形成矿石的液体是 H 2O 公司 2-NaCl±CH4 类型与对低咸度中等温度、中等。硫同位素的价值(δ34 S 为金矿石的 CDT ) 在 11.08 ‰ 之间变化并且 12.58 ‰ ,显示混合了硫来源;氢同位素的价值(δD 从 -83.68‰ 的 V 降雪 ) 范围到 -116.95‰并且氧同位素的价值(δ18 O 在 12.04 ‰ 之间的 V 降雪 ) 范围并且 16.28 ‰ 。氢和氧同位素建议形成矿石的液体从主要岩浆发源,并且在迟了的阶段期间与大量大气的水混合。东方山东省金存款与让 mantle-crust-mixed 采购原料的 magmatic 活动被联系,并且也与热水的黄金扔的 orgenic 和 epithermal 分享一些类似。因为东方山东省黄金与与另外的金牌不同的唯一的 metallogenic 特征和形成背景扔,沉积物录入世界,我们把它称为 Jiaojia 类型金存款。千吨班 Jiaojia 金存款与液体活动,延期和分队有关源于岩浆的热 upwelling。在到在东方山东省的早白垩纪的迟了的舞台的中间的强壮的 magmatic 活动为金 depsoits 导致活跃液体,和提供的丰富的形成矿石的材料。而且,源于外壳的扩展的许多 extensional 结构为放的 orebody 提供了赞成空间。 | SONG Mingchun DENG Jun YI Pihou YANG Liqiang CUI Shuxue XU Junxiang ZHOU Mingling HUANG Tailing SONG Guozheng SONG Yingxin | 2014 | Acta Geologica Sinica(English Edition)2014，88，3： | 14 |
| 19 | Theoretical and experimental study on relationship between stress-strain and temperature variation显示文摘Principle on temperature response to the stress-strain variation is fundamental to the relationship between thermal radiation variation and stress-strain field. Current research indicates that temperature has a sensitive response to rock deformation under the condition of normal temperature background. However, the basic physical relationship between deformation and temperature variation is not clear and need to be investigated further. In this paper, principle on temperature response to stress-strain variation is studied in detail, based on thermodynamics, elastic strain theory, and experiments on both ideal material and rock. In the stage of elastic deformation, results indicate that: 1) temperature increment is positively correlated with volume strain variation. Temperature rises with hydrostatic pressure increase. In other words, temperature rises when the specimen is under the compressive state whereas temperature drops under the tensile state. 2) Pure shear deformation does not contribute to tempera- ture variation. Namely, shape change of specimen does not produce temperature variation. However, there exist the relative tensile area and the compressive one in the specimen under the state of pure shear. Temperature drops within the relative tensile area while temperature rises within the compressive areas during the process of loading. | CHEN ShunYun LIU LiQiang LIU PeiXun MA Jin CHEN GuoQiang | 2009 | Science China Earth Sciences2009，52，11： | 13 |
| 20 | Reconstruction of Ore-controlling Structures Resulting from Magmatic Intrusion into the Tongling Ore Cluster Area during the Yanshanian Epoch显示文摘摘要:Tongling 矿石簇区域经历了集中的压缩并且联系了在 Indosinian-Yanshanian 时代期间砍,它形成了一个箱子在 caprock 的控制矿石的褶层和差错系统。在 Yanshanian 时代的 magmatic 侵入导致了多相的液体的多级式的 unmixing,导致多层、宽范围、多种形式的式样描绘的矿化作用。在 Tongling 区域的 magmatic 侵入不仅供应了必要形成矿石的材料,而且重建控制矿石的结构根据下列五条阶层边界的趋势表面模拟:志留纪泥盆纪,泥盆纪含碳,含碳二叠,中间二叠上面二叠、二叠三叠纪。这模拟的结果证明那在那里存在在上面的部分和那些在的阶层之间的重要差别更低。而上面的趋势表面是 synform,更低的趋势表面是 antiform。另外,趋势迭加邻近的床边界出现(例如,志留纪泥盆纪边界在泥盆纪含碳的边界之上迭加) 证明更低的趋势表面总是上面穿透那。而且,不同迭加的趋势表面的穿透的部分的位置和取向是类似的并且根据地区性的 E-W-trending magmatic-metallogenic 带的分发显示出 E-W-trending 带的分发。基于阶层,结构的变丑机制,和地现象的机械性质的全面分析,看起来, stratal 趋势表面的特殊特征由于 magmatic 侵入源于 jacking 进一个 E-W-trending 地下室差错以前控制的 caprock。因此,主要控制矿石的结构,在地区性的水平压缩期间形成了,被形成矿石的岩浆的垂直 jacking 功能在 Yanshanian 时代期间重建,这被推出。在形成矿石的过程期间,岩浆的本地垂直 jacking,结合了地区性的水平压缩,在液体水管网络优化了广泛的环境并且加速了多相的液体的 unmixing 后面的 magmatic 炮兵阵地。Jacking 也加强了垂直、侧面的指导液体的结构,供应为多层的炮兵阵地和多相的液体的广阔运输的更合适的物理条件。 | DENG Jun WANG Qingfei YANG Liqiang GAO Bangfei HUANG Dinghua LIU Yah XU Hao JIANG Shaoqing | 2007 | Acta Geologica Sinica(English Edition)2007，81，2： | 13 |
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