Stellar Abundance and Galactic Chemical Evolution through LAMOST Spectroscopic Survey

A project of a spectroscopic survey of Galactic structure and evolution with a Large sky Area Multi-Object fiber Spectroscopic Telescope (LAMOST) is presented. The spectroscopic survey consists of two observational modes for various targets in our Galaxy. One is a major survey of the Milky Way aimed at a systematic study of the stellar abundance and Galactic chemical evolution through low resolution (R=1000-2000) spectroscopy. Another is a follow-up observation with medium resolution (R = 10000) spectrographs aimed at detailed studies of the selected stars with different chemical composition, kinematics and dynamics.     

A New Eusauropod Dinosaur from the Lower Cretaceous of Guangxi Province, Southern China

<正>A new sauropod dinosaur,Liubangosaurus hei gen.et sp.nov.,is erected based on a specimen represented by five articulated middle-caudal dorsal vertebrae,which was discovered in the Lower Cretaceous Napai Formation of Guangxi Province,southern China.This new taxon is diagnosed by a unique combination of derived features:prezygapophysis closely contacts with parapophysis,with the prdl and prpl absent;presence of cavity on the dorsal surface of the diapophysis;neural spine very low,with its distal end level with that of diapophysis;distal end of the neural spine strongly expanded laterally to form a platform;marked fossa formed between the infradiapophyseal lamina and the parapophysis;broad,flat area of featureless bone on lateral surface of neural arch;vertically directed infradiapophyseal lamina expands or bifurcates ventrally to form a inverted "Y";highly positioned parapophyses large and tear-drop in shape.The discovery of this new taxon increases the diversity of sauropods in China during the Early Cretaceous.     

小秦岭地区金矿化与花岗岩浆活动的关系──流体标型特征提供的依据

对小秦岭地区与金矿化有关的主要地质体中流体包裹体叠加组合标型特征和有关地质体Sr、H、O同位素组成的标型性研究证明,小秦岭地区中生代中温热液金矿化流体与中生代花岗岩浆分界出的热液之间没有直接联系,成矿流体更可能是一种演化的大气降水。花岗岩浆活动对金矿化的贡献主要表现为提供了一组局部热源,间接地影响了金矿化的形成。     

桐柏-大别地区中温热液金矿床成矿流体性质与沉淀机理

通过对桐柏－大别地区１０个中温热液金矿床（点）的流体包裹体研究，确定成矿流体属于低盐度（６ｗｔ％ＮａＣｌ），富ＣＯ２（１０ｍｏｌ％）的ＮａＣｌ－ＣＯ２－Ｈ２Ｏ体系。这种以演化的大气降水为主的流体在４～１０ｋｍ深度范围内，由于压力由静岩压力状态的向静水压力状态的空而发生的复杂三阶段不混溶过程中沉淀，在该过程的中晚期出现金矿化。压力状态的突变是柏桐－大别造山带在中生代碰撞造山晚期，由挤压体制向伸展体制     

麻粒岩中流体研究提供的成因信息

本文从流体的成分和性质(流体组成,a_(H2O),f_(O2)与C-O-H流体系统相关系)及有关的四种麻粒岩形成机制模式方面概括了麻粒岩中流体研究近年来取得的主要成果。这些成果极大地促进了麻粒岩问题研究的深入进行,但同时又向人们提出了一系列新的需要解决的问题,文中简要地指出了主要的五个问题。