广南洒拉冲-东瓜湾金矿地质

洒拉冲-东瓜湾金矿属于微细粒浸染型金矿及火山熔岩型金矿。金矿化受地层、构造、基性火成岩的控制。多期基性火成岩侵入,为金矿化的形成提供了热源和物源。     

西双版纳勐海勐满热泉型金矿

勐满金矿赋存在澜沧群浅变质岩系和侏罗系红层中,金富集对围岩岩性无明显选择,具低温热液蚀变特征,属热泉、变质热液成因。     

临沧坝兔花岗岩破碎带石英脉型含银铅矿

矿床为双脉并行,产于两条与花岗岩破碎带相关的含银铅矿化带内。建立三个矿物生成阶段及与矿化有关的二个矿物组合,铅锌成矿应在岩浆期后中一低温热液阶段,硅化破碎花岗岩是主要赋矿岩石。     

云南沧源芒哈铅锌银矿成因及预测

沧源芒哈铅锌银多金属矿床是澜沧江南段火山岩成矿带乃至三江地区较重要的一种新类型,矿体产于花岗斑岩脉的外接触带,岩体和矿体同受北西走向的构造破碎带控制。     

2型糖尿病、非酒精性脂肪肝与血清胆碱酯酶的关系探讨

目的 探讨2型糖尿病（T2DM）、非酒精性脂肪肝（NAFLD）与血清胆碱酯酶（S-CHE）的关系。方法 随机选取221例T2DM患者,将患者分为T2DM合并NAFLD、未合并NAFLD两组。并随机选取同一时期体检的工人及退休人员206例,分为单纯NAFLD和正常对照组。所有被检者进行餐前和餐后2h血糖、糖化血红蛋白（HbA1c）、肝肾功能、血脂、S-CHE的检测以及肝胆胰脾B超检查;对T2DM患者进行空腹C肽和餐后C肽的测定,并计算胰岛素抵抗指数（HOMA2-IR）、胰岛素敏感度指数（HOMA2-%S）、胰岛β细胞功能（HOMA2-%B）。结果 DM合并NAFLD和单纯NAFLD组的S-CHE水平明显高于T2DM未合并NAFLD组和正常对照组（P均<0.01）;随着T2DM病程的延长,S-CHE、ALT、GGT、TG、TC、空腹C肽、餐后C肽的水平逐渐下降,年龄逐渐增高（P<0.05或P<0.01）;将T2DM患者分为A（S-CHE<8900IU/L）、B（S-CHE≥8900IU/L）两组,B组患者的BMI、脂肪肝百分比、ALT、AST、GGT、TG、TC、LDL-C、HOMA2-IR高于A组,HOMA2-%S低于A组（P<0.05或P<0.01）;Pearson偏相关分析显示,校正年龄、性别、病程、HbA1c、FBG、收缩压、舒张压后,S-CHE与HOMA2-IR、BMI、TG、TC、LDL-C、ALT、GGT水平呈正相关,与HOMA2-%S呈负相关（P<0.05或P<0.01）;多元线性回归分析显示,S-CHE与TC、HOMA2-IR、ALT水平呈正相关（R²=0.281,P均<0.01）。结论 S-CHE的水平在NAFLD患者明显增高,而未合并NAFLD的T2DM患者S-CHE的水平并无增高,S-CHE水平升高主要与脂肪肝、胰岛素抵抗及血脂紊乱相关,常规检测S-CHE可以反映T2DM患者胰岛素抵抗的情况以及早期预测NAFLD的发生。     

Origin of crude oils from oilfields in the Zagros Fold Belt,southern Iraq: Relation to organic matter input and paleoenvironmental conditions

Crude oil samples from Cretaceous and Tertiary reservoir sections in the Zagros Fold Belt oil fields, southern Iraq were investigated using non-biomarker and biomarker parameters. The results of this study have been used to assess source of organic matter, and the genetic link between oils and their potential source rocks in the basin. The oils are characterized by high sulphur and trace metal (Ni, V) contents and relatively low API gravity values (17.4–22.7° API). This indicates that these oils are heavy and generated from a marine source rock containing Type II-S kerogen. This is supported by their biomarker distributions of normal alkanes, regular isoprenoids, terpanes and steranes and the bulk carbon isotope compositions of their saturated and aromatic hydrocarbons. The oils are characterized by low Pr/Ph ratios (<1), high values of the C₃₅ homohopane index and C₃₁-22R/C₃₀ hopane ratios, relatively high C₂₇ sterane concentrations, and the predominance of C₂₉-norhopane. These biomarkers suggest that the oils were generated predominantly from a marine carbonate source rock, deposited under reducing conditions and containing plankton/algal and microorganisms source input. The presence of gammacerane also suggests water column stratification during source rock deposition.The biomarker characteristics of the oils are consistent with those of the Middle Jurassic Sargelu carbonate as the effective source rock in the basin. Biomarker maturity data indicate that the oils were generated from early maturity source rocks.     

绿春大马尖山铜砷矿矿床成因

矿体赋存于下志留统变质砂板岩及侵入其中的石英斑岩中,与燕山晚期构造运动及岩浆活动有关。水平及垂直分带明显。属低温热液硫化物充填—交代型铜砷矿。     

Type II bursts in Meter and Decameter – Hectometer Wavelength Ranges and Their Relation to Flares and CMEs

Statistical analysis of the relationship between type II radio bursts appearing in the metric (m) and decameter-to-hectometer (DH) wavelength ranges is presented. The associated X-ray flares and coronal mass ejections (CMEs) are also reported. The sample is divided into two classes using the frequency-drift plots: Class I, representing those events where DH-type-II bursts are not continuation of m-type-II bursts and Class II, where the DH-type-II bursts are extensions of m-type-II bursts. Our study consists of three steps: i) comparison of characteristics of the Class I and II events; ii) correlation of m-type-II and DH-type-II burst characteristics with X-ray flare properties and iii) correlation of m-type-II and DH-type-II burst characteristics with CME properties. We have found no clear correlation between properties of m-type-II bursts and DH-type-II bursts. For example, there is no correlation between drift rates of m-type-II bursts and DH-type-II bursts. Similarly there is no correlation between their starting frequencies. In Class I events we found correlations between X-ray flare characteristics and properties of m-type-II bursts and there is no correlation between flare parameters and DH-type-II bursts. On the other hand, the correlation between CME parameters and m-type-II bursts is very weak, but it is good for CME parameters and DH-type-II bursts. These results indicate that Class I m-type-II bursts are related to the energy releases in flares, whereas DH-type-II bursts tend to be related to CMEs. On the contrary, for Class II events in the case of m-type-II and DH-type-II bursts we have found no clear correlation between both flare and CMEs.     

康古尔塔格碰撞带中酸性侵入岩成因类型

从地球化学特征入手对康古尔塔格碰撞带中酸性侵入岩的成因类型和构造环境进行了探讨。认为该带花岗岩类岩石以第Ⅰ组和第Ⅱ组为主，第Ⅲ组为辅。此外，尚有部分第Ⅳ组碱性玄武岩。     

兰坪金顶铅锌矿——陆相SEDEX型矿床

矿床形成于兰坪-云龙古新世湖盆东部,沘江同生断层西侧的次级坳陷。容矿岩系为古新统云龙组中、上段。中段为重力滑塌岩块及角砾岩相-构造活动型冲积扇相沉积;上段为河口砂坝相沉积。矿床两层结构明显:上部是化学沉积成矿系统;下部是补给成矿系统。两系统的矿体形态、矿石类型、结构构造、矿化及蚀变强弱均有显著差异。矿床显示SEDEX型(Sedimentary Exhalation喷气沉积的缩写)矿床特征。成矿物质系深源,硫来自硫酸盐经分解而产生的还原硫,成矿介质属混合水。矿床在有利的聚矿次级坳陷、导矿同生断层、有利矿化沉积岩相、上下屏蔽层圈闭及外来岩系掩埋等条件下耦合形成。属陆相SEDEX型铅锌矿床。