Petrogenesis and Geodynamic Implications of Early Cretaceous (~130 Ma) Magmatism in the Baingoin Batholith, Central Tibet: Products of Subducting Slab Rollback

The Baingoin batholith is one of the largest granitic plutons in the North Lhasa terrane. Its petrogenesis and tectonic setting have been studied for decades, but remain controversial. Here we report data on geochronology, geochemistry and isotopes of Early Cretaceous granitoids within the Baingoin batholith, which provide more evidence to uncover its petrogenesis and regional geodynamic processes. The Early Cretaceous magmatism yields ages of 134.4–132.0 Ma and can be divided into I-type, S-type and highly fractionated granites. The I- and S-type granites exhibit medium SiO2, high K2O/Na2O with negative εNd(t) and εHf(t) values, whereas, the albite granites have very high SiO2 (79.04%–80.40%), very low K2O/N2O, negative εNd(t) and a large variation in εHf(t). Our new data indicate that these granitoids are derived from unbalanced melting in a heterogeneous source area. The granodiorites involved had a hybrid origin from partial melting of basalt-derived and Al-rich rocks in the crust, the porphyritic monzogranites being derived from partial melting of pelitic rocks. The albite granites crystallized from residual melt separated from K-rich magma within the ‘mush’ process and underwent fractionation of K-feldspar. We believe that the Early Cretaceous magmatism formed in an extensional setting produced by the initial and continuous rollback of a northward-subducting slab of the NTO.     

北斗卫星导航系统精密定轨技术研究现状

北斗系统开通运行以来,无论是系统建设还是精密定轨技术均获得了长足发展。文中简要介绍了北斗系统目前的建设情况,总结梳理了北斗卫星精密定轨技术发展现状。在此基础上,分析论述了北斗系统精密定轨中亟待解决的主要问题。     

Labour mobility in the public sector: the impact of job opportunities

This paper investigates the mobility of highly skilled labour, using doctors in public hospitals in Denmark as an example. From the perspective of regional development, the concentration of human capital is one of the contributors to regional growth and consequently to inequality between places, being associated most often with differences in economic growth between regions. The decentralisation of highly skilled public jobs to even out the concentration of human capital could be one way to stimulate growth outside city regions. However, such initiatives are somewhat dependent upon the cooperation of the highly skilled public employees, whose preferences have been little studied thus far. Based on data from a survey of 1600 publicly employed doctors, PLUM regression modelling was applied to test the relative significance of four professional preferences influencing choice of workplace. It was found that professional preferences have different influences on doctors’ choices, depending on their place of residence measured in terms of a location’s population density. The paper concludes that opportunities in employment depend on one’s stage in life and can serve to explain choices and mobility among highly skilled public employees.     

东准噶尔喀拉萨依高分异A 型花岗岩岩石成因及其地质意义

喀拉萨依岩体位于东准噶尔卡拉麦里碱性花岗岩带西端,由钾长花岗岩和二长花岗岩组成。LA-ICP-MS锆石U-Pb年龄为307.7±3.2Ma~309.6±2.0Ma,岩石高硅（SiO2平均含量为77.25%）、富碱（K2O+Na2O=7.50%~9.23%）、低铝（A/CNK=0.922~1.084）,贫钙、镁;富集Rb、K、Th等大离子亲石元素及Zr、Hf等高场强元素和稀土元素,亏损Ba、Sr、Eu。10000Ga/Al值变化于7.00~10.35之间,总体上具碱性A型花岗岩的特征,是该岩带东侧老鸦泉—黄羊山A型花岗岩岩基经高程度分异演化的产物,并非前人认为的S型花岗岩。岩体具正εNd（t）值（3.5~6.0）和年轻的Nd模式年龄（TDM2=520~630Ma）,Pb同位素投点位于造山带演化线附近,同位素数据显示岩浆来源于新生造山带下部的年轻地壳。从本次1∶5万区调成果看,卡拉麦里洋盆在晚泥盆世之前已经闭合,从晚泥盆世开始转入碰撞后的拉张环境,在晚石炭世早期进入板内裂谷发展阶段,因此喀拉萨依岩体应是该区板内裂谷阶段而非前人所说的后碰撞阶段的产物。     

Metamorphism and deformation of mafic and felsic rocks in a magma transfer zone,Stewart Island,New Zealand

In the mingled mafic/felsic Halfmoon Pluton at The Neck, Stewart Island (part of the Median Batholith of New Zealand) some hornblende gabbros and diorites retain magmatic structures, whereas others show evidence of major changes in grain and inclusion shapes, and still others are amphibolite‐facies granofelses with few or no igneous relicts. These mafic to intermediate magmas crystallized in felsic magma relatively quickly, with the result that most deformation occurred at subsolidus conditions. It is suggested that mafic‐intermediate rocks with predominantly igneous microstructures spent less time in the magmatic system. The metamorphism of the mafic rocks appears to be ‘autometamorphic’, in the sense that elevated temperatures were maintained by magmatic heat during subsolidus cooling. Elevated temperatures were maintained because of repeated sheet injection and subconcordant dyke injection of hot basaltic and composite mafic‐felsic magmas, into a dominantly transtensional, km‐scale, outboard‐migrating, magmatic shear zone that operated semi‐continuously for between c. 140 and c. 130 Ma. Complete cooling occurred only when the system evolved to transpressional and the locus of magmatism migrated inboard (southward) between c. 130 and c. 120 Ma, associated with solid‐state mylonitic deformation. Intermingled granitic rocks escaped metamorphism, because they remained magmatic to lower temperatures, and experienced shorter and lower‐temperature subsolidus cooling intervals. However, the felsic rocks underwent relatively high‐temperature solid‐state deformation, as indicated by myrmekite replacing K‐feldspar and chess‐board subgrain patterns in quartz; locally they developed felsic mylonites. The felsic rocks were deformed in the solid state because of their high proportion of relatively weak minerals (quartz and biotite), whereas the mafic rocks mostly escaped subsolidus deformation, except in local high‐strain zones of hornblende‐plagioclase schist, because of their high proportion of relatively strong minerals (hornblende and plagioclase). We suggest that such contrasting microstructural features are diagnostic of long‐lived syntectonic magma transfer zones, and contrast with the more typical complex, batholith‐scale magma chambers of magmatic arcs.     

高被引华人科学家知识网络的空间结构及影响因素

知识网络的空间结构特征与影响因素是经济地理学探讨的热点议题之一,以往研究侧重于产业案例的分析,主要关注国家和城市层面的知识网络,而对科学家等个人层面的网络研究较为缺乏。以2014—2015年全球高被引科学家为原始数据,筛选出高被引华人科学家,并基于Web of Science数据库,检索高被引华人科学家之间合著论文的数据构建知识网络,借助社会网络分析方法对高被引华人科学家知识网络的空间结构进行分析;并运用负二项回归模型,从地理邻近性、社会邻近性、制度邻近性3个维度,探讨高被引华人科学家知识网络的影响机制。研究发现：① 高被引华人科学家知识网络存在核心-边缘结构特征,且具有小世界网络的网络特征;② 此知识网络呈现“小集聚大分散”的空间结构特征,地理邻近性作用明显;③ 高被引华人科学家知识网络形成过程中会受到科学家自身科研能力等因素的影响,地理距离和科学家之间的联系呈现负相关关系,地理邻近性的影响仍然存在,社会邻近性和制度邻近性均对知识网络的形成有促进作用。     

Precise integration method without inverse matrix calculation for structural dynamic equations

The precise integration method proposed for linear time-invariant homogeneous dynamic systems can provide accurate numerical results that approach an exact solution at integration points. However, difficulties arise when the algorithm is used for non-homogeneous dynamic systems due to the inverse matrix calculation required. In this paper, the structural dynamic equalibrium equations are converted into a special form, the inverse matrix calculation is replaced by the Crout decomposition method to solve the dynamic equilibrium equations, and the precise integration method without the inverse matrix calculation is obtained. The new algorithm enhances the present precise integration method by improving both the computational accuracy and efficiency. Two numerical examples are given to demonstrate the validity and efficiency of the proposed algorithm.     

逐步添加法制备单链环状DNA的影响因素探究

单链环状DNA在纳米技术、分子生物学和医药学等领域具有广泛的应用前景,但难以大量制备一直是制约其研究和应用的难题之一。本文针对一种高效大量制备单链环状DNA的方法-逐步添加法,系统地探究了逐步添加法中各主要条件对制备单链环状DNA的影响,确定了逐步添加法中的主要关键条件为:T4DNA连接酶Buffer浓度、单链DNA浓度、添加间隔时间、温度和Splint GC含量。以72nt的核酸链为例,使用逐步添加法将单链环状DNA的制备得率提高至99%,产量与常用的一步法相比提高至4.9倍。本研究为高效、大量制备单链环状DNA提供了指导,为以单链环状DNA为基础的研究奠定了基础。     

珠三角快速城镇化地区国土调查典型试点探索与实证——面向第三次全国国土调查

选择东莞市4个镇（街）作为珠三角典型高度城镇化地区和第三次全国国土调查试点,针对试点内容设置、试点典型性选择、试点方法、成果和质量控制等全过程进行了总体策划和设计。从调查底图层面提出了数据源精选类别,形成了3套数据组合配置思路。从调查技术层面阐述了内业分析判读、外业调查核实和内业录入整理的3个关键方法实施路径。通过试点：形成了丰富的专题报告、专题报表、专题图和专题库等实验成果,以土地利用现状调查为例分析了各试点区历经快速城镇化后的土地利用差异性和空间格局特征,提出了在涉密基础数据使用、不一致图斑举证、细碎图斑处理、地类认定标准、多源数据空间不套合和标识码核心关联等7个问题环节的具体先验经验和未来需要深入探索提升的方向。试点成果可作为试点区土地精细化管理之用,试点经验可供快速城镇化地区参考之用。     

利用高支链类异戊二烯(HBIs)重建极地海冰的研究进展

海冰的准确重建对反演气候和环境变化具有重要意义。近期研究表明,有机指标高支链类异戊二烯(HBIs)具有重建极地海冰状况的潜质,海洋沉积物中具有海冰特异性的单烯HBI(IP_(25))和双烯HBI(IPSO_(25))指标已分别成为研究北极和南极海冰变化的有力工具。本文综述了IP_(25)、IPSO_(25)的提出和验证,分析了影响HBIs生成、迁移和埋藏的诸多因素,总结了为实现精细化区分海冰状况和定量化重建海冰密集度而提出的新指标的发展及应用,并就目前存在的问题和未来研究方向进行了探讨和展望。