浙西北前震旦纪火山岩的Nd、Sr同位素地球化学

在浙西北双溪坞群和上墅组火山岩系获得较可靠的Sm－Nd同位素年龄的基础上，本文进一步做了Nd、Sr同位素地球化学研究。∈Nd（T）和∈Sr（T）示踪判别了该区前震旦纪火山岩浆源区特征及其物质来源。同时，Nd同位素模式年龄为该区存在更古老基底提供了重要的地质年代信息。     

马超营断裂带地质及地球化学特征

根据对马超营断裂带系统进行的地质—地球化学剖面研究，探讨了该带断裂构造活动及其元素地球化学迁移富集规律与构造地球化学分异之间的关系；分析了蚀变、矿化与成矿的关系，认为早期面型蚀变伴有成矿元素的活化和迁移，但无矿化富集，后期带状蚀变伴有金的富集成矿且以硅化、绢云母化为主要标志。从而，为马超营断裂带这一重要的以金为主成矿带的进一步工作、研究，提供了地球化学方面的依据。     

Discovery of A-type Granite Zone and Its Geodynamic Significance in the Western Kunlun Mts., China

l. IntroductionGranite distributes widely in western KunlunMts. Many researches have been conducted byscientists (Wang Yuzhen et.al., l987; Zhang Yuquanet.al., l989, Fang Xilian et.al., I990, Jiang Chunfaet.al., 1992; Pan Yusheng, l992, Xu Ronghua et.al.,l 994; Jing Daogui et.al., l996, Zhang Yuquan et.al.,l998). But all of the researches have been donealong Sino-Pakistan road and Xinjiang-Tibet roadt"ith fOcus on isotopic dating of the intrusion andconducted a few on origin and tect…     

EXPERIMENTAL GEOCHEMISTRY STUDY ON GOLD IN WATER-ROCK REACTION UNDER THERMAL FLUID SYSTEM AT MESO-LOW TEMPERATURE

Based on the knowing geochemical characteristics of wall rock in the Mobin gold deposit and composition of fluid inclusion in ore,water-rock experiments were carried out,important achievements are acquired as following: Gold is mainly derived from the ore-bearing wall rock,i,e.,a series of epimetamorphic clastic gritstone,sandy slate,and tuffaceous slate in the Wuqiang Banxi Formation,Wuqiangxi Group.In thermal system with middle-low temperature chlorine gold may be derived form stable complex ions,so it is quite important in gold metallogenic process.Sulphur and chlorine perform as the major negative ions throughout the gold activation and migration movement.The concentration of sulphur and chlorine ions,pH value and temperature are of deciding significance for gold activation,migration and precipitation.     

No-association of proportions

This note has three purposes: to briefly review the role of neutrality as a criterion of no-association of proportions; to compare neutrality with a criterion proposed by Snow in this journal; to describe a simple test of neutrality in the median.     

Dissolved chromium in the St. Lawrence estuary

A study of dissolved chromium in the St. Lawrence estuary and Gulf of St. Lawrence has been carried out. A chromium concentration of 0·7 μg l^?1 was found in the St. Lawrence River. In the turbidity maximum of the upper estuary, chromium is removed from solution onto fine-grained resuspended sediments and internally produced organic-rich floccules. A simple flux calculation shows that these processes remove ～50% of the total dissolved chromium input of the river. At salinities greater than 5‰ dissolved chromium mixes conservatively.     

玲珑金矿田岩石地球化学测量及其找矿效果

根据玲珑金矿田１∶２０００岩石地球化学测量结果,结合本区地质构造条件,初步总结了该矿田岩石地球化学特征。获取的岩石地球化学异常经过验证,施工的３５个钻孔有２７个见矿,４３条验证探槽中有４条发现工业矿体。该方法在发现隐伏的矿化蚀变带、寻找矿体（矿化体）、确定矿体剥蚀程度及指导钻探施工等方面均有明显效果。     

吉林东部延吉地区中生代火山岩地球化学特征

吉林东部延吉地区大面积出露的中生代火山岩,根据岩性特征可分为三个火山喷发旋回。各旋回火山岩均属ＳｉＯ２过饱和的中基性—中酸性岩类。从第一旋回至第三旋回岩石碱度变化较大,岩浆分异明显,特别是第三旋回分异作用明显高于第一、二旋回。火山岩中金、铜微量元素的平均含量普遍高于同类岩石的克拉克值几倍至几十倍,而且随着岩浆分异程度的升高,其平均含量有明显升高的趋势,为本区金、铜矿床的形成提供了物质来源。     

Applied hydrodynamic wave-resistance computation by Fourier transform

An applied Fourier transform computation for the hydrodynamic wave-resistance coefficient is shown, oriented to potential flows with a free surface and infinity depth. The presence of a ship-like body is simulated by its equivalent pressure disturbance imposed on the un-perturbed free surface, where a linearized free surface condition is used. The wave-resistance coefficient is obtained from the wave-height downstream. Two examples with closed solutions are considered: a submerged dipole, as a test-case, and a parabolic pressure distribution of compact support. In the three dimensional case, a dispersion relation is included which is a key resource for an inexpensive computation of the wave pattern far downstream like fifteen ship-lengths.     

藏东吉塘地区早古生代花岗岩锆石U-Pb年龄、Hf同位素及其对原特提斯洋演化的启示

以前对藏东吉塘地区的早古生代岩浆事件鲜有报道,在吉塘地区的浪拉山新发现了中—晚奥陶世花岗岩。采用LA-ICP-MS锆石U-Pb测年,获得该花岗岩的206Pb/238U年龄加权平均值为455±2.0 Ma（WSWD=1.15,n=26）,属于中—晚奥陶世。岩石地球化学特征表明,该花岗岩具有高SiO2（78.72%~79.48%）、富钾（K2O/Na2O=5.55~10.20）,低MgO（0.10%~0.25%）的特征,铝饱和指数A/CNK为1.08~1.26,岩石属于高钾钙碱性强过铝S型花岗岩。岩石稀土元素总体表现为轻稀土元素富集、重稀土元素亏损的特征,具强烈负Eu异常,δEu值为0.35~0.39;在原始地幔标准化微量元素蛛网图上,明显富集Rb、Th、Nd、Pb等元素,亏损Ba、Nb、Sr、P、Ti等元素。结合区域地质资料分析,该岩体是由原特提斯洋俯冲消减引起古老地壳物质部分熔融形成的,是原特提斯洋俯冲消减的岩浆事件响应;说明在中—晚奥陶世吉塘地区存在原特提斯洋的俯冲消减作用。