Carboniferous eclogite and garnet–omphacite granulite from northeastern Hainan Island,South China: Implications for the evolution of the eastern Palaeo‐Tethys

High‐P (HP) eclogite and associated garnet–omphacite granulite have recently been discovered in the Mulantou area, northeastern Hainan Island, South China. These rocks consist mainly of garnet, omphacite, hornblende, quartz and rutile/ilmenite, with or without zoisite and plagioclase. Textural relationships, mineral compositions and thermobarometric calculations demonstrate that the eclogite and garnet–omphacite granulite share the same three‐stage metamorphic evolution, with prograde, peak and retrograde P?T conditions of 620–680°C and 8.7–11.1 kbar, 820–860°C and 17.0–18.2 kbar, and 700–730°C and 7.1–8.5 kbar respectively. Sensitive high‐resolution ion microprobe U–Pb zircon dating, coupled with the identification of mineral inclusions in zircon, reveals the formation of mafic protoliths before 355 Ma, prograde metamorphism at c. 340–330 Ma, peak to retrograde metamorphism at c. 310–300 Ma, and subsequent pegmatite intrusion at 295 Ma. Trace element geochemistry shows that most of the rocks have a MORB affinity, with initial ε_Nd values of +2.4 to +6.7. As with similar transitional eclogite–HP granulite facies rocks in the thickened root in the European Variscan orogen, the occurrence of relatively high P?T metamorphic rocks of oceanic origin in northeastern Hainan Island suggests Carboniferous oceanic subduction leading to collision of the Hainan continental block, or at least part of it, with the South China Block in the eastern Palaeo‐Tethyan tectonic domain.     

自适应高程分级的城区DSM晕渲方法

在对传统的分层设色晕渲理论应用于城区DSM的可视化技术进行充分研究的基础上,提出了一种基于高程直方图的自适应高程分级方法。该方法通过高程直方图研究城区地形、地物的高程分布及变化特征,自适应建立高程带分级模型。实验表明,提出的晕渲图制作方法兼顾了地貌形态和地物特征的表达,成果色彩过渡自然,层次清晰,地形、地物区分明显,有较强的艺术性和实用价值。     

青海省祁漫塔格地区1∶5万水系沉积物测量衬值异常圈定实例

青海省祁漫塔格地区位于柴达木盆地西南缘,是青海省重要的铁多金属成矿基地之一。利用88442个野外采样点1∶5万水系沉积物测量数据,采用Geo Expl软件圈定了该地区的衬值异常。衬值是指各元素0.5 km×0.5 km网格化数据与其园域搜索半径5km、移动步长0.5km移动平均值的比值。选用自定义累频"90、95、98、100"确定了异常的外、中、内带。通过常规方法和衬值圈定的异常的对比,表明衬值异常能够削弱不同地质背景差异,使异常形态更为规整,浓集中心更为明显,并且可能发现新异常。     

大兴安岭北段东坡中北部小莫尔可地区 中生代火山岩成因及其地质意义

大兴安岭地区是一个经历了古亚洲洋、蒙古-鄂霍茨克洋闭合和环太平洋构造体系叠加复合构造区,以其发育规模巨大、结构复杂的陆相火山岩带和花岗岩带以及有色、贵金属矿床备受国内外地质学家广泛关注和研究(Wu, et al.,2006;白令安,2013;Sun J G,2013;Xu,et al.,2013;苟军,2013)。目前,虽然该区在中生代陆相火山岩的成因、形成的构造背景已取得了较大进展;但是,由于大兴安岭地区火山作用复杂,自然地理、交通条件较差,尚有大面积空白区未开展过系统的1：50000区域地质矿产调查和科研工作;近期我们课题组在开展大兴安岭东坡花岗岩带北部1：50000小鄂尔贝尔汗（M51E012016）和小莫尔可（M51E011016）幅区域地质矿产调查过程中,将地质矿产调查与科研相结合,对侵入喷发在花岗岩岩体之间陆相火山岩进行了岩石地层厘定和岩相学、元素地球化学、年代学以及Hf同位素研究,以期为整体揭示大兴安岭火山岩的源区性质及其演化规律提供科学依据,并从成矿元素地球化学角度来约束成矿物质来源,并结合区域成矿作用探讨区域找矿意义。     

The impact of boreal autumn SST anomalies over the South Pacific on boreal winter precipitation over East Asia

The possible mechanism behind the variability in the dipole pattern of boreal winter precipitation over East Asia is analyzed in this study. The results show that the SST anomalies(SSTAs) over the South Pacific Ocean(SPO) in boreal autumn are closely related to the variability in the dipole pattern of boreal winter precipitation over East Asia. The physical link between the boreal autumn SPO SSTAs and the boreal winter East Asian precipitation dipole pattern is shown to mainly be the seasonal persistence of the SPO SSTAs themselves. The seasonal persistence of the SPO SSTAs can memorize and transport the signal of the boreal autumn SSTAs to the following winter, and then stimulates a meridional teleconnection pattern from the SH to the NH, resulting in a meridional dipole pattern of atmospheric circulation over East Asia in boreal winter. As a major influencing factor, this dipole pattern of the atmospheric circulation can finally lead to the anomalous precipitation dipole pattern over East Asia in boreal winter. These observed physical processes are further confirmed in this study through numerical simulation. The evidence from this study, showing the impact of the SPO SSTAs in boreal autumn,not only deepens our understanding of the variability in East Asian boreal winter precipitation, but also provides a potentially useful predictor for precipitation in the region.     

2015年汛期气候预测先兆信号的综合分析

文章全面回顾了发布2015年汛期预测时考虑的先兆信号及其应用情况。2015年春夏季厄尔尼诺事件进一步发展,并由中部型向东部型转变,热带印度洋为一致偏暖模态发展;冬、春季北大西洋三极子为正位相;冬、春季北极海冰较常年略偏少,南极海冰偏多;冬季欧亚积雪增量略少,青藏高原积雪略多但气温偏高。通过诊断分析,认为2015年汛期预测的主导外强迫信号是太平洋厄尔尼诺事件和印度洋海温一致偏暖模态。同时参考动力气候模式的预测,在4月初的预报中,重点考虑了厄尔尼诺事件的强度和空间型变化对东亚夏季风环流的影响,有利于东亚夏季风偏弱,西太平洋副热带高压偏强偏西,季风季节内进程偏晚,我国降水呈南多北少型。在5月底的订正预报中,进一步考虑热带印度洋偏暖模态对副热带高压偏强偏西偏南的影响,以及南半球越赤道气流强度偏弱特征及对夏季风季节进程和强度的影响。经过综合分析,准确地预测了2015年东亚夏季风偏弱、我国夏季降水南多北少的布局,以及季节内主要气候事件的演变。最后对汛期气候预测存在的不足进行了初步分析和讨论。