吉林省金星金矿床特征及成因探讨

该矿床位于辉南—桦甸—和龙金(银)成矿带的东段,产于太古界三道沟组中,矿体受北西向韧性剪切带内次级断裂控制,成因类型为变质热液韧性剪切带型(蚀变糜棱岩型)。     

Penglai Zircon Megacrysts: A Potential New Working Reference Material for Microbeam Determination of Hf–O Isotopes and U–Pb Age

We introduce a potential new working reference material – natural zircon megacrysts from an Early Pliocene alkaline basalt (from Penglai, northern Hainan Island, southern China) – for the microbeam determination of O and Hf isotopes, and U–Pb age dating. The Penglai zircon megacrysts were found to be fairly homogeneous in Hf and O isotopes based on large numbers of measurements by LA-multiple collector (MC)-ICP-MS and SIMS, respectively. Precise determinations of O isotopes by isotope ratio mass spectrometry (IRMS) and Hf isotopes by solution MC-ICP-MS were in good agreement with the statistical mean of microbeam measurements. The mean δ¹⁸O value of 5.31 ± 0.10‰ (2s) by IRMS and the mean ¹⁷⁶Hf/¹⁷⁷Hf value of 0.282906 ± 0.0000010 (2s) by solution MC-ICP-MS are the best reference values for the Penglai zircons. SIMS and isotope dilution-TIMS measurements yielded consistent ²⁰⁶Pb/²³⁸U ages within analytical uncertainties, and the preferred ²⁰⁶Pb/²³⁸U age was found to be 4.4 ± 0.1 Ma (95% confidence interval). The young age and variably high common Pb content make the Penglai zircons unsuitable as a primary U–Pb age reference material for calibration of unknown samples by microbeam analysis; however, they can be used as a secondary working reference material for quality control of U–Pb age determination for young (particularly < 10 Ma) zircon samples.     

X-ray Spectromicroscopy of Mineral Intergrowths in the Santa Catharina Meteorite

This work describes the application of microfocus X-ray absorption spectroscopy (XAS) and X-ray photo-emission electron microscopy (XPEEM) to the study of the complex mineralogical intergrowths within the Santa Catharina meteorite. The Santa Catharina meteorite of this study (BM52283 from the meteorite collection of the Natural History Museum, London, UK) primarily comprises a taenite bulk host phase (Fe:Ni ratio = 70.9 ± 0.8%:29.1 ± 0.8%) with a set of oxide-bearing cloudy zone textured regions (Fe:Ni:O ratio = 40.4 ± 0.3%:49.0 ± 0.7%:10.6 ± 0.8% at the core and Fe:Ni:O ratio = 34.4 ± 1.5%:42.7 ± 0.6%:22.9 ± 1.8% towards the rims) and numerous schreibersite (Fe:Ni:P ratio = 38.6 ± 1.6%:38.4 ± 0.9%:23.0 ± 0.5%) inclusions. Between the schreibersite and the taenite are rims up to 50 μm across of Ni-rich kamacite (Fe:Ni ratio = 93.4 ± 0.4%:6.6 ± 0.5%). No chemical zoning or spatial variations in the Fe and Ni speciation was observed within either the schreibersite or the kamacite phases. The oxide-bearing cloudy zone textured regions mostly comprise metallic Fe–Ni alloy, predominantly tetrataenite. Within the oxide phases, the Fe is predominantly, but not entirely, tetrahedrally co-ordinated Fe³⁺ and the Ni is octahedrally co-ordinated Ni²⁺. Structural analysis supports the suggestion that non-stoichiometric Fe₂NiO₄ trevorite is the oxide phase. The trevorite:tetrataenite ratio increases at the edges of the oxide-bearing cloudy zone textured regions indicating increased oxidation at the edges of these zones. The spatial resolution of the XPEEM achieved was between 110 and 150 nm, which precluded the study of either the previously reported ∼ 10 nm precipitates of tetrataenite within the bulk taenite or any antitaenite.     

Isobar Attenuation Using Anion–Gas Reactions for Accelerator Mass Spectrometry and Application to 36Cl

Preliminary tests of a prototype radio-frequency quadrupole (RFQ) collision cell system, known as an isobar separator for anions (ISA), for the removal of isobaric interferences for accelerator mass spectrometry (AMS) and for studies of anion–gas interactions are reported. The ISA decelerated a mass-analysed beam of anions from an energy (∼ 20 keV) typically generated by an AMS ion source to < 10 eV. RFQs and electrostatic lenses then guided the ions through the collision cell where ion-gas collisions reduced both the energy and energy spread of the ion beam (cooled the ions) and ion-gas reactions attenuated most of the unwanted isobars. The anions were then re-accelerated to their original energy for injection into the rest of the AMS system. With the ISA installed on a full 3 MV AMS system, attenuations of ³²S^-, ¹²C₃^- and ³⁹K^- by six, seven and greater than ten orders of magnitude, respectively were achieved using 0.7–1 Pa NO₂ gas in the collision cell, while maintaining approximately 10–30% of the chlorine anion transmission. A further measurement of a ³⁶Cl/Cl = 4.1 × 10^-11 RM is also described. The results suggest that the ³⁶Cl/Cl lower detection limit of the current system was 10^-14–10^-15 for samples that could be prepared with S/Cl ratios below 10 μg g^-1.     

New Approach to Geochemical Measurement: Estimation of Measurement Uncertainty from Sampling,rather than an Assumption of Representative Sampling

It is argued that the current division between field sampling and chemical analysis is counterproductive in terms of ensuring that geochemical measurement results are fit for their intended purpose. An integrated approach to the whole measurement process has many advantages including no dependence on the two assumptions that either the samples are necessarily representative if taken with a correct protocol, or that the measurement results can be assumed to be true values of chemical concentration. The measurement results then require values of measurement uncertainty, including that from sampling as well as from chemical analysis. This enables the user of the measurement results, rather than the producer, to judge their fitness for a specific purpose. Case studies are used to illustrate the practicality and benefits of this new approach, including the use of measurement results with optimal, but relatively high, levels of uncertainty to make reliable decisions. This contrasts with the traditional assumption that pursuit of the lowest possible measurement uncertainty is the best approach.     

Perturbed Robe’s circular restricted three-body problem under an Oblate Primary

This paper examines the existence and linear stability of equilibrium points in the perturbed Robe’s circular restricted three-body problem under the assumption that the hydrostatic equilibrium figure of the first primary is an oblate spheroid. The problem is perturbed in the sense that small perturbations are given to the Coriolis and centrifugal forces are being considered. Results of the analysis found two axial equilibrium points on the line joining the centre of both primaries. It is further observed that under certain conditions, points on the circle within the first primary are also equilibrium points. And a special case where the density of the fluid and that of the infinitesimal mass are equal (D = 0) is discussed. The linear stability of this configuration is examined; it is observed that the first axial point is unstable while the second one is conditionally stable and the circular points are unstable.     

文人主导下的群体性办刊模式——20世纪40年代港版《文艺生活》的办刊模式及其省思

在20世纪40年代后期香港特殊的时空环境中,国内流亡文人与其所办刊物的生存方式是一个耐人寻味的话题。司马文森之于港版《文艺生活》月刊的办刊策略适时调整为文人主导下的群体性办刊模式,主要表现为出版资金的群体性支持,发行上的群众性和杂志稿源的群众性。这种独特的办刊模式不仅丰富了人们对20世纪40年代文学期刊办刊模式的认识,有助于人们更加深入地了解四十年代现代文学(尤其是华南现代文学)和现代作家的历史境遇和现代命运,而且对于当下一些文学杂志以及其他刊物的办刊策略和市场运作等方面具有后瞻性的意义和价值。     

基于UGC文本挖掘的城市旅游客流网络结构研究——以西安市为例

旅游流是旅游地理学研究的一项重要命题,理解游客的空间流动特征对城市旅游的发展有重要意义。通过对穷游网UGC文本数据的挖掘,依托图论理论构建了一种可以同时保留旅游客流的有向性与加权性的流网络结构描述方法,并对西安市区域层面与节点层面的旅游客流网络结构进行研究。结果表明:(1)城市旅游的客流存在明显的网络结构特征,客流网络结构主要由区域(节点)的中心程度决定;(2)城市旅游客流结构与旅游主体功能分区高度耦合;(3)区域(节点)主体功能的时空属性也是影响旅游客流结构的一个重要因素;(4)通过对区域(节点)净外向程度的分析,可以得到其旅游“集”“散”功能的偏重,可为具体区域的旅游发展提供借鉴与启示。     

城市公园游憩行为的性别差异——以广州人民公园为例

以广州市人民公园为研究对象,通过实地踏勘和问卷调查,利用统计与观察分析方法解剖城市公园游憩行为的性别差异特征。在游憩者的行为和社会特征方面,两性之间存在明显差异;女性的公园游憩行为与其社会分工特别是家庭责任紧密联系;女性因对安全性的要求高而趋向视线开敞的集体区域活动,男性因要求独立性而趋向在有视线遮挡的区域活动,且男性同性恋活动区域对女性形成了一定的活动抑制;女性对出行距离较为敏感,而男性独自出行游憩的比例更高;女性对城市游憩空间的需求趋于稳定、有规律,也凸显了公园对女性日常生活的重要性。基于公平性与人性化原则提出相应的城市公园规划设计对策,特别应对公共设施进行细致而灵活的设计,以适应使用者的性别差异性;并应按照步行尺度进行游憩场所的规划布局,以保障女性就近游憩的需求。     

民生福祉导向下的中国中部地区低碳发展竞争力评价——基于AHP-TOPSIS模型的实证

在碳约束下提升区域竞争力是中部地区低碳发展获取竞争优势的关键所在。区域低碳发展竞争力是一个地区在碳约束下持续提高碳排放绩效、不断促进地区经济繁荣和提升居民福祉的能力。基于AHP-TOPSIS组合评价法对中国中部六省低碳发展竞争力进行评价。湖南省综合竞争力最强,江西省次之,山西省最弱,湖北省次弱,河南、安徽两省居中。中部六省低碳发展竞争力的驱动模式具有较大差异:山西省低碳发展竞争力主要由产出竞争力驱动,江西省由基础竞争力和效率竞争力驱动,安徽省主要由效率竞争力驱动,湖北省由潜力竞争力和产出竞争力驱动,河南省主要由基础竞争力和效率竞争力驱动,湖南省低碳发展各子竞争力之间相对均衡发展。