SPATIAL VARIATION OF Zn GEOCHEMICAL FRACTIONS IN THE SURFACE SEDIMENTS OF THE STRAITS OF MALACCA: NATURAL OR ANTHROPOGENIC?

1INTRODUCTION Studiesonheavymetalcontaminationinsedi mentshavealwaysbeenfocusedonthecoastalandin tertidalareas(Sivalingam,etal.,1980;Ismail,1993;Ismail,etal.,1993;IsmailandRosniza,1997;Yap,etal.,2002a,2002b).Theheavymet alconcentrationsfoundinthesediments…     

Spatial distribution and behavior of dissolved selenium speciation in the South China Sea and Malacca Straits during spring inter-monsoon period

Selenium(Se) has been recognized as a key trace element that is associated with growth of primary producers in oceans. During March and May 2018, surface water(67 samples) was collected and measured by HG-ICP-MS to investigate the distribution and behavior of selenite [Se(IV)], selenate [Se(VI)] and dissolved organic selenides(DOSe) concentrations in the Zhujiang River Estuary(ZRE), South China Sea(SCS) and Malacca Straits(MS). It showed that Se(IV)(0.14–3.44 nmol/L) was the dominant chemical species in the ZRE, related to intensive manufacture in the watershed; while the major species shifted to DOSe(0.05–0.79 nmol/L) in the MS, associated with the wide coverage of peatland and intensive agriculture activities in the Malaysian Peninsula. The SCS was identified as the northern and southern sections(NSCS and SSCS) based on the variations of surface circulation.The insignificant variation of Se(IV) in the NSCS and SSCS was obtained in March, potentially resulting from the high chemical activity and related preferential assimilation by phytoplankton communities. Contrastively, the lower DOSe concentrations in the SSCS likely resulted from higher primary production and utilization during March. During May, the concentration of Se(IV) remained low in the NSCS and SSCS, while DOSe concentrations increased notably in the SSCS, likely due to the impact of terrestrial inputs from surface current reversal and subsequent accumulation. On a global scale, DOSe is the dominant Se species in tropical oceans, while Se(IV) and Se(VI) are major fractions in high-latitude oceans, resulting from changes in predominated phytoplankton and related biological assimilation.     

闽粤沿海地震形势的初步分析

本文从地震学和地震地质学角度出发，讨论海峡７．３级地震对东南沿海地震带活动性的影响。着重分析了海峡７．３级震前的背景空区及其震后演变过程，并采用各种方法对闽粤沿海地区进行了时空扫描分析，提取异常指标。预测该地区未来地震活动的趋势，对缩小未来可能发生破坏性地震的时间、地点、强度范围具有一定的意义。     

Least-Squares Estimation of Bottom Topography Using Horizontal Velocity Measurements in the Tsushima/Korea Straits

Several bathymetric data sets are compared and assessed with constraints of an ocean current model and velocity observations. The root-mean-square (rms) differences among the data sets reach 20 m in the shallow Tsushima/Korea Straits. The numerical experiments to simulate the Tsushima Warm Current are performed using four different topography data sets. The JTOPO1 data (MIRC, 2003) give the smallest rms difference to long-term horizontal velocity observations. Several least-squares combinations of the topography data sets are then sought to minimize the rms difference between the observed and modeled barotropic velocities. Most of the data sets reveal a large bias of 30–60 m at the Western Channel compared to independent sounding depths     

台湾海峡及其两岸的地球动力学环境

本文根据断层的力学性质、活动习性、褶皱、断陷盆地、平原、海湾的形成机理,火山活动、水系分布格局,震源机制解、地壳形变场、ＧＰＳ观测成果和ＥＤＭ（光电测距）资料等,对比研究了台湾海峡及其两岸现今的地球动力学环境。结果表明：台湾海峡处在北西方向引张的应力环境;台湾地区受到来自太平洋菲律宾海板块向北西方向的挤压和因台湾海峡下降而产生的向南东方向的挤压;福建沿海则受到印度板块向北向东的挤压和太平洋菲律宾海板块向北西方向的挤压以及台湾海峡下降而产生的向北西方向的挤压。     

The source rupture feature of the southern Taiwan Straits earthquake of September 16, 1994 ( M S7.3) & the analysis of earthquake circumstance in southeastern coast of China

According to the source mechanism of the main shock and the distribution feature of the aftershocks occurring in the southern Taiwan Straits on Sept. 16, 1994, in this paper the authors analysed the source rupture feature of the major earthquake, demonstrated that this seismic sequence possessed the characteristics of a large intraplate earthquake. And according to the seismotectonic background and the historical seismicity in the area, the authors clarified the active characteristics of the seismically active belts along northwestern direction and analysed preliminarily the earthquake circumstance in the southeastern coast of China.     

台湾海峡两岸地缘经济整合的 驱动机制与途径

基于对地缘经济整合的理论思考和内、外部驱动机制的分析，论证了海峡两岸地缘经济一体化是中国在全球经济区域化进程中的一项重要战略选择的观点。通过海峡两岸经济整合的内部基础、特别是近年来台湾经济发展对大陆依赖性的解剖，反映了海峡两岸经济一体化的雏形。采取现状与前景预测相结合的方式，探讨了两岸经济在世界经济体系中的整体竞争优势和地位，从而确定了经济整合的目标和战略重点。并着眼“海峡两岸经济整合促进统一大业实现”的立论，提出了若干政策层面的建议：立足两岸互补条件和各自的竞争潜力、加强经济合作；构筑垂直与水平分工并重的产业分工体系；建立两岸新的区域合作框架和经济合作运行模式。     

海峡西岸城市群旅游经济网络演化的动力机制与因果组合配置

以海峡西岸城市群为例,通过修正引力模型构建旅游经济网络,依托“增长极”理论,运用QAP和地理探测器分析方法,探讨旅游经济网络驱动因素,并运用fsQCA方法探讨其因果组合配置策略。结果如下：(1)海峡西岸城市群旅游经济网络空间结构呈东部沿海地区网络相对密集、中西部网络稀疏特征。(2)地区经济水平、对外开放程度是其核心驱动因素;各影响因子对促进旅游经济空间发展的影响强度均较高。(3)地理探测器分析结果显示,各影响因素在旅游经济网络系统中处相对优势地位,旅游经济空间发展核心驱动因素明显,其中,以地区GDP、对外开放程度最为突出,这也体现为旅游需求不断提升以及旅游供给向高质量方向发展的趋势。研究最终识别出两种因果组合配置方案。本研究有助于实现区域旅游经济空间发展优化及管理。