山东莱州金城金矿床构造-流体成矿特征

This paper studied the metallotectonics, altered rocks, altered minerals and fluid inclusions. The conclusions are: (1)The gold deposits in Jiaodong district were formed quickly uplifted tectonic setting which was induced by the Mantle doming in Mesozoic era. (2)Both Jiaojia-type and Linglong-type gold mineralizations were formed in the same tectonic-fluid system. (3) The Ar-Ar age of the earlier stage of the gold mineralization is 114～116Ma. (4)The development of the plaiting ore-control tectonic system underwent four stagesrcounterclockwise ductile compresso-shearing, clockwise brittle tenso-shearing and counterclockwise brittle compresso-shearing and brittle normal faulting after mineralization. (5)The mineralization has five stages: quartz and k-feldspar stage, quartz and ferro-carbonate and pyrite stage, quartz and chalcopyrite stage, pyrite and sericite and quartz stage and carbonate stage, and they make up four ore-types: red ore, vein ore, mottled ore and grey ore. (6) The features of mineralizations and ore-forming fluids in different stages are different. But the ore-forming fluids are rich in Si, Fe, P_2O_5, H_2O, CO_2, SO_4~(2-), K~+, Na~+, Ca~(2+) and Cl~- in general and their salinities are from 4 to 18 NaClwt%. (7) The ore-forming fluids came mainly from the Mantle in early stage, then mainly from magma, and mainly from meteoric water in the last stage. (8) Au in the ore-forming fluid was mainly carried in the form of complex of Au and S. (9)The temperature of ore-forming fluid is from 350℃ to 120℃and its pressure is from 20MPa to 38MPa. (10)The gold vein composed by quartz, ferro-carbonate, chalcopyrite and pyrite (vein ore) was filled in the tensional fracture in the top of the magma dome. The disseminated ore bodies composed by pyrite, sericite and quartz (grey ore) was metasomatized in the shearing fault which developed along the contact zone between Linglong intrusive body and Jiaodong Group, which is placed in the flank top of magma dome. In the joint and fracture induced by the shearing fault which developed along the contact zone between Linglong intrusive body and Jiaodong Group, veiniet and stockwork ore (red ore) and veinlet-disseminated ore (mottled ore) composed by quartz and pyrite was formed. (ll)Fluid boiling maybe one of the form of the ore-forming substances precipitation.

新疆萨瓦亚尔顿（穆龙套型）金矿床物质来源与成矿机制

萨瓦亚尔顿金矿床是我国90年代金矿地质工作者在新疆西南天山地区寻找穆龙套型金矿床的一个突破。本文通过对新疆萨瓦亚尔顿金矿床的矿石矿物组成、稀土元素地球化学、同位素地球化学以及流体包裹体特征等方面的研究，探讨了萨瓦亚尔顿金矿床地质地球化学特征、金的赋存状态及成矿流体特征、成矿流体来源，提出了该矿床的成矿机制，取得如下认识：1．流体包裹体岩相学研究表明，萨瓦亚尔顿金矿床的流体包裹体主要为V＋L相和富CO_2相包裹体，前者为NaCl-H_2O体系，后者主要有L_(CO2)、L_(CO2)+L、V_(CO2)+L、V_(CO2)＋L_(CO2)＋L相包裹体；并发现极少量含子晶流体包裹体。2．通过流体包裹体显微测温学研究，表明金矿床的均一温度成矿早阶段为270～320 ℃，成矿主阶段为170～250 ℃，成矿晚阶段为110-250 ℃，呈逐渐降低的趋势，低温成矿作用明显。3．单个流体包裹体的激光拉曼分析表明，流体包裹体中除含有CO2之外，还含有一定量的N_2和CH_4。4.成矿物质来源的复杂性。萨瓦亚尔顿金矿床矿石中微量元素组成、稀土配分模式大都反映了成矿金属物质主要来自赋矿地层本身。金属硫化物的6345：-3.4‰～+2.6‰，西南天山地区下古生界地层中广泛存在各类火山岩可能是该矿床的主要硫源，部分可能有深部物质的参与。矿石中主要脉石矿物石英和菱铁矿 中包裹体水的氢氧同位素组成为δD = -72％～-62‰，δ~(18)O ＝ -11.6‰～＋5.4‰。成矿流体主要为大气降水补给的地下卤水，并有少量岩浆水的混合。5．Ar-Ar同位素地球化学研究表明，萨瓦亚尔顿金矿床的主要成矿时代为印支晚期，210 Ma。6. 对矿石中的流体包裹体进行了温度、压力、成分、pH、含盐度等的分要的，并系统的进行了矿床形成时的物理化学条件的理论计算，基中包括EH、PH、f_(O_2)、f_(S_2)等及金在矿液运移中的搬运形式。指出减压过程或伴生沸腾的减压过程，是矿床形成过程中矿质卸载的基本机制，此外，酸蚀变过程（如绢云母化等）中由于H~+的消耗促进了溶液中pH值的升高；含高炭质的围岩，降低了矿液的氧逸度以及含矿热液与地表下渗冷水的混合等诸多因素，则是矿订形成的辅助机制。

Prediction of soil adsorption coefficients from retention parameters on three reversed-phase liquid chromatographic columns

Reversed-phase high-performance liquid chromatographic (RP-HPLC) retention parameters, which are determined by the intermolecular interactions in retention process, can be considered as the chemical molecular descriptors in linear free energy relationships (LFERs). On the basis of the characterization and comparison of octadecyl-bonded silica gel (ODS), cyano-bonded silica gel (CN), and phenyl-bonded silica gel (Ph) columns with linear solvation energy relationships (LSERs), a new multiple linear regression model using RP-HPLC retention parameters on ODS and CN columns as variables for estimation of soil adsorption coefficients was developed. It was tested on a set of reference substances from various chemical classes. The results showed that the multicolumn method was more promising than a single-column method was for the estimation of soil adsorption coefficients. The accuracy of the suggested model is identical with that of LSERs.