北半球阻塞高压的维持Ⅱ:瞬变扰动强迫和平均流位涡平流的形成

着重探讨大西洋阻高和东亚阻高个例中瞬变扰动位涡（涡度）输送强迫和太平洋阻高中平均流位涡平流的形成机理。结果表明，扰动在阻高西南部西风分流区因形变而产生的扰动拟能向更小尺度串级过程，并不是扰动位涡输送强迫形成的必要机理。扰－流相互作用在阻高西（北）部非分流气流中也十分显著。数值试验表明，这一相互作用也可能是扰动强迫作用形成的机理。而青藏高原和附近海陆对比的强迫作用则可能是太平洋阻高中平均流的位涡平流形成的重要因素。对比分析表明，阻高维持机制的地域性差别可能与其上游（如青藏高原地区、落基山脉）地形和热源强迫作用不同有关。     

攀西地区重力均衡异常的研究

研究表明,康滇地轴及其东部地区属均衡补偿平衡区,西部属强烈上升的异常区。上升的原动力为板块碰撞的构造力与均衡调整力的综合。     

On the genesis of dabaoshan polymetallic deposit in Guangdong Province,China

The Dabaoshan deposit is a polymetallic deposit containing Mo, W, Cu, Pb and Zn. There is much controversy about the genesis of the deposit. In the early 1960s, it was considered as a meso-hypothermal deposit resulting from interstratified replacement. Recently, some other genetic models have been put forward, e.g. the strata-bound deposit model. Studies of the contents of characteristic elements in pyrite and sphalerite, the compositions of sulfur and lead isotopes, zoning of primary halos, homogenization temperatures of fluid inclusions in minerals from the deposit and element abundances in the strata led to a conclusion that the deposit is of post-magmatic hydrothermal origin.     

Geochemical characteristics of gossans related to siderite deposits in carbonate strata,western guizhou

Zonal distribution can be noticed in the gossans resulting from the weathering of siderite in carbonate strata, and this can be accounted for by zoning of subsurface waters. Since siderite is more insoluble than its hostrock, gossans are generally developed in the same place as siderite is exposed. Systematic variations in chemistry are recognizable from the ore body upwards to the surface. The gossans are high in Fe and Mn, but impoverished in S, P, Pb, Zn, Be, Cd, and Ag. This may serve as an indicator of distinguishing siderite gossans from sulphide ones in this region.     

Stable isotope characteristics and origin of ore-forming fluids in copper-gold-polymetallic deposits within strike-slip pull-apart basin of Weishan-Yongping continental collision orogenic belt, Yunnan Province, China

More than 140 middle-small sized deposits or minerals are present in the Weishan-Yongping ore concentration area which is located in the southern part of a typical Lanping strike-slip and pull-apart basin. It has plenty of mineral resources derived from the collision between the Indian and Asian plates. The ore-forming fluid system in the Weishan-Yongping ore concentration area can be divided into two subsystems, namely, the Zijinshan subsystem and Gonglang arc subsystem. The ore-forming fluids of Cu, Co deposits in the Gonglang arc fluid subsystem have δD values between −83.8‰ and −69‰, δ¹⁸O values between 4.17‰ and 10.45‰, and δ¹³C values between −13.6‰ and 3.7‰, suggesting that the ore-forming fluids of Cu, Co deposits were derived mainly from magmatic water and partly from formation water. The ore-forming fluids of Au, Pb, Zn, Fe deposits in the Zijinshan subsystem have δD values between −117.4‰ and −76‰, δ¹⁸O values between 5.32‰ and 9.56‰, and Δ¹³C values between −10.07‰ and −1.5‰. The ore-forming fluids of Sb deposits have δD values between −95‰ and −78‰, δ¹⁸O values between 4.5‰ and 32.3‰, and Δ¹³C values between −26.4‰ and −1.9‰. Hence, the ore-forming fluids of the Zijinshan subsystem must have been derived mainly from formation water and partly from magmatic water. Affected by the collision between the Indian and Asian plates, ore-forming fluids in Weishan-Yongping basin migrated considerably from southwest to northeast. At first, the Gonglang arc subsystem with high temperature and high salinity was formed. With the development of the ore-forming fluids, the Zijinshan subsystem with lower temperature and lower salinity was subsequently formed. Translated from Mineral Deposits, 2006, 25(1): 60–70 [译自: 矿床地质]     

特大地震对震源邻区的增(减)震作用的研究

通过研究中国大陆1910年以来8级以上特大地震和国外几组典型特大地震对震源邻近区域的影响,发现特大地震往往发生在断裂带上,一组或一次特大地震可能使发震断裂部分破裂,而未破裂断裂的构造应力可能增大,又成为大震的空段,该空段短时间内可能会发生大震(起到增震作用);反之,发震断裂完全破裂或没有大震空段,震源邻近区域构造应力可能减小,短时间可能不会发生大震(起到减震作用)。依据这一结果,可对特大地震发生后震源邻近区域的后续大震作短、中期预测。     

影响我国主要粮食作物产量的气象因子研究

通过收集前人主要粮食作物气象产量预报的研究成果，将所得到的资料按作物进行分类，并进行归一化处理，使用系统聚类分析方法，以预报方程中的影响因子为指标，分区找出各区主要粮食作物产量的主、次要影响因子和影响时期，为大范围作物产量预报提供了科学依据。     

地面中—β尺度强锋区激发的特大暴雨过程分析

受0012号台风（派比安）外围影响，2000年8月30日02时至31日08时，在江苏省东北部发生了一次具有局域性、突发性、高强度、超历史、灾情重等特征的特大暴雨，分析研究发现，在台风外围第二象限，江苏东北部地面存在中-β尺度的能量锋区，此能量锋区是构成产生、维持特大暴雨的中-β尺度的天气系统。利用锋生函数对此能量锋区的发生发展进行诊断，结果表明，锋生函数的变形项起了决定性作用，辐合项也有较明显的贡献，非绝热加热在锋生初期有作用，但对锋区的维持，其贡献并不明显，进一步用二维中尺度方程对锋区进行数值模拟，结果显示，在能量锋附近驱动产生了涡旋，在涡旋上升支，将高能区的暖湿空气向上输送而成云致雨，在涡旋下沉支，通过下沉气流使雨迅速下落，同时拖曳冷空气使地面降温，使得锋区维持和加强，致使雨强增幅，综合分析表明，中-β尺度能量锋区形成以后，通过锋区附近的中-β尺度的辐合线，中低压，中高压以及锋区附近驱动的扰动涡旋等中-β尺度的天气系统间的相互作用，导致了这次江苏省东北部高强度的特大暴雨。     

湘中锡矿山式锑矿成矿地质条件分析

湘中锡矿山式锑矿形成于晚白垩-古新世,空间上与岩脉关系密切,各锑矿床、矿化点都伴有或附近发育有煌斑岩及中-酸性岩脉群,在锑矿成矿同期地质事件中,还有周缘一些中-新生代红色盆地的形成及基性火山岩喷发,据之,提出湘中锡矿山式锑矿成矿与燕山晚期拉张构造-岩浆活化作用有关.锑矿床(点)基本上都产出于两组或两组以上断裂的交汇点附近,3组断裂的交汇部位对应于最主要的锑矿床(点).矿体具体受断裂交汇部位附近的次级短轴背斜轴部、倾伏背斜的倾伏端及其翼部被纵向陡倾角断裂构造所切穿的部位控制,是断裂导矿与背斜构造圈闭的体现.岩性组合控矿表现为易于硅化蚀变交代的砂质碳酸盐岩与隔挡层泥质岩所构成的岩性圈闭.根据包裹体均-温度和盐度测定成果,推算成矿压力为(200～300)×10⁵Pa,成矿深度约为1 km.     

大气季节内振荡：其全球同步性及其与ENSO的关系

利用美国国家环境预报中心和大气研究中心的大气再分析资料，分析研究了大气季节内振荡的年际变化及其与ＥＮＳＯ的关系。揭示了全球不同纬度带之间存在着的大气季节内振荡年际变化的同步性，以及大气季节内振荡与海温和大气向外长波辐射之关系的复杂性。我们还发现大气季节内振荡与Ｎｉｎｏ３指数的关系存在年代际尺度的变化，即，这种关系有时强时弱的现象。