Babu (SW China)‐Cao Bang (NE Vietnam) Ophiolite Complex: Implications for Tectonic Evolution between South China and the Indochina Block     

MA Tianshou  WANG Lixing  GE Guangfu  DAI Chunzheng  YU Hao 《《地质学报》英文版》2019,93(Z2):34-36

The convergence process between South China and the Indochina Block is still controversial. A large number of igneous rocks scattered along the current China‐Vietnam border provide a good opportunity to investigate the tectonic evolution. Babu ophiolites, cropping out in the southeastern Yunnan province (SW China), consist primarily of metaperidotite, serpentinite, pillow basalt (metabasalt), gabbro, metadiabase. Most of them are fault contacted and strongly sheared, especially between metaperidotite/serpentinite and metabasalt. U‐Pb zircon analyses yield an Early Permian formation age of ～278 Ma. Basalts and metagabbros show light rare earth elements (LREEs)‐depleted and heavy rare earth elements (HREEs)‐flat REE patterns, and large ion lithophile elements (LILEs)‐depleted primitive‐normalized spider diagrams without Nb‐Ta anomalies, which is similar to N‐MORB. Metaperidotites have low initial ¹⁸⁷Os/¹⁸⁸Os (0.122‐0.126) and γOs values, and indicate that they were derived from a depleted mantle source. Relative low (⁸⁷Sr/⁸⁶Sr)i and high εNd(t) values of basalts and metagabbros also support their DMM origin. The petrological, geochemical and isotope characteristics suggest that Babu ophiolites were N‐MORB‐type and represent remnants of an Early Permian oceanic crust. Mafic‐ultramafic rocks exposed in Cao Bang area (NE Vietnam) have recently been considered as dismembered Paleotethyan ophiolites instead of were genetically linked to the Emeishan Large Igneous Province. U‐Pb zircon analyses suggest an Early‐Middle Permian age (274 ±18 Ma) for the formation of ultramafic rocks. Both whole rock geochemistry and Cr‐spinel mineral chemistry show MORB‐like characteristics. Field observations suggest that Babu and Cao Bang ophiolite complex structurally overlie Middle‐Triassic deposits, and form a tectonic mélange zone. It developed from the subduction of a Paleotethyan subsidiary ocean basin between the South China and Indochina blocks until their collision..  相似文献   

南祁连党河南山中段科克巴斯陶玄武岩年代学、地球化学特征及其地质意义     

王磊  李向民  胡兆国  杨超  郭令芬  闫海忠  葛瑞臣  计波 《大地构造与成矿学》2019,43(5):1069-1077

与柴北缘和北祁连相比,南祁连研究程度偏低,对其各个阶段的构造演化缺少精确时限。对分布于南祁连党河南山中段的科克巴斯陶玄武岩进行了岩石地球化学及锆石U-Pb年代学研究,定年结果显示,该玄武岩成岩年龄为713±4.6Ma,为新元古代震旦纪。岩石地球化学分析表明,科克巴斯陶玄武岩SiO2含量为45.08%~49.81%,MgO为4.37%~6.67%,Na2O为2.95%~3.71%,K2O为0.28%~1.92%,TiO2为1.40%~2.01%,与拉斑玄武岩平均值相似。Nb/Y-SiO2图解显示科克巴斯陶玄武岩属亚碱性系列拉斑玄武岩。其ΣREE为(75.47~124.00)×10^-6,LREE/HREE为4.2~6.19。(La/Yb)N为3.67~6.18,(La/Sm)N为1.83~2.64,球粒陨石标准化稀土元素配分曲线图呈轻稀土明显富集的右倾型。原始地幔标准化微量元素蛛网图上,岩石以富集Sr、K、Rb、Ba为特征。岩石地球化学特征显示科克巴斯陶玄武岩岩浆为具OIB性质的地幔源区,其形成于板内洋岛构造环境。结合区域地层对比及锆石测年成果,将原划定的志留系巴龙贡嘎尔组进行了重新解体,由南至北,分别为志留系巴龙贡嘎尔组变砂岩段、新元古界震旦系天峻组火山岩段和中新元古界拐杖山组片岩段。  相似文献   

页岩岩屑高精度波速测量的仪器与方法     

索彧  葛洪魁  王小琼  孟范宝  刘峻嵘 《岩土力学》2018,39(1):385-392

压裂改造是页岩气开发的关键技术,岩石的脆性评价是储层可改造性的重要参数之一。实验室中通常利用岩芯柱进行波速测量,获得杨氏模量和泊松比以评价页岩的脆性系数。但规则的页岩岩芯很难获得。为此,利用非规则的页岩岩屑,设计并提出了一套基于脉冲回声法的岩屑高精度波速测量的仪器和方法。分析了影响岩屑波速测量精度的主要因素,引入了新针式高频声波探头和新数字信号分析方法,利用脉冲回声法,通过提高采样率和信噪比、使用自相关的方法来提高精度,形成了一套页岩岩屑高精度波速测量的仪器与方法。同时试验结果也与规则岩芯测量结果进行了对比,证实了此仪器与方法的可靠性。  相似文献   

西太平洋暖池混合层热力异常与我国东部夏季降水的关系   总被引：5，自引：5，他引：0  

张良瑜  王黎娟  韩世茹  葛静 《热带气象学报》2015,31(3):355-363

利用1981—2012年GODAS(Global Ocean Data Assimilation System)月平均次表层海温资料、混合层深度资料、NCEP/NCAR再分析资料及中国756个站的逐日降水资料,分析西太平洋暖池混合层热力异常与中国东部夏季降水的关系及可能的影响途径。结果表明,前期5月是西太平洋暖池(125~150 °E,0~18 °N)混合层热力异常影响我国东部夏季降水的关键期。在前期5月西太平洋暖池异常偏暖(冷)年,长江中下游流域的夏季降水偏少(多),黄河中下游流域夏季降水偏多(少)。1991—2012年,5月的西太平洋暖池热力异常呈现明显的变化趋势,由异常偏冷期向偏暖期转变。机制分析表明,由于前期5月西太平洋暖池热力异常,引起夏季菲律宾附近及其以东洋面和印度半岛中北部上空的对流活动、西太平洋副热带高压(简称副高)和南亚高压位置及强度的异常,进而影响水汽输送及上升运动,最终导致我国东部夏季降水的异常分布。   相似文献   

Design of the HUV based on the airplane's principles     

WANG Qiang  GE Tong  WU Chao  YAN Hui 《海洋工程》2012,30(2)

结合固定翼飞机与潜器设计原理设计了一种密度大于水的潜器——重水潜器,它利用机翼升力平衡剩余重量,外形就像固定翼飞机.由理论分析可知在有效载荷和航行速度相同的情况下重水潜器较常规潜器的体积有明显减小,而以中高速航行时重水潜器阻力优势明显.根据固定翼飞机与潜器设计原理相结合的设计方法制作的重水潜器样机进行水池试航时顺利完成直航、水平回转、爬升、下潜等规定动作,并表现出良好的稳定性和操纵性,从而证明了该设计方法的可实现性.  相似文献   

南海 18°N 断面 上的体积和热盐输运   总被引：2，自引：0，他引：2  

葛黎丽  程旭华  齐义泉  王东晓 《热带海洋学报》2012,31(1):10-17

以2005—2008年4年中南海北部开放航次所获得的水文观测资料为基础,结合卫星高度计遥感资料,采用动力计算方法计算南海18°N断面的经向地转流,并与声学多普勒流速剖面仪(Acoustic Doppler Current Profilers,ADCP)走航观测资料进行对比,进而计算出通过南海18°N断面1000m以浅的各站位以及断面上总的经向地转体积、热、盐输运量。结果表明,2005—2008年南海北部开放航次期间18°N断面上的经向地转流呈相间带状分布,各站位经向地转流流速垂向分布和ADCP观测的大体一致。从卫星高度计获得的海面高度场可知,经向地转流流向的空间变化与海洋中尺度涡旋的活动密切相关。2005—2007年航次期间南海18°N断面上1000m以浅总的经向地转体积、热、盐输运均为南向输运,其3年的平均输运量分别为11.8Sv(1Sv=106m3.s 1)、0.38PW、418.8Gg.s 1;其年际间差别较大,经向地转体积、热、盐输运量均为2005年最大,2006年次之,2007年最小。2008年110°—117°E之间1000m以浅总的海水地转体积、热、盐输运量分别为7.3Sv、0.22PW、259.4Gg.s 1。  相似文献   

利用ADS40相机快速生成正射影像图的方法研究     

王明海  耿迅  张军  戈一鸣 《海洋测绘》2012,(3):56-58

介绍了ADS40相机快速生成正射影像图的方法,即利用高精度POS设备能直接定向测图的特点,省去空三T序,利用POS解算出的外方位元素和自动提取的DEM进行正射影像纠正,结合实际生产项目对成图精度进行了分析。试验结果表明,ADS40相机应用于航测生产可大幅度缩短成图周期,利用本文的生产方法可以满足正射影像图精度要求,并节省大量时问,适用于应急测绘保障。  相似文献   

不同地区毛蚶群体的形态差异的比较研究   总被引：1，自引：0，他引：1  

宋菲菲  王其翔  刘名  盖姗姗  刘洪军  唐学玺 《中国海洋大学学报(自然科学版)》2012,(11):40-45

运用多变量形态度量学分析方法,采用13个形态性状,对山东省4个地区:青岛红岛、威海乳山、东营河口、东营广饶,以及辽宁省葫芦岛和海南省三亚6个不同地区的毛蚶(Scapharca subcrenata)群体间的形态差异进行了比较研究。聚类分析和主成分分析结果表明:河口群体和广饶群体形态最为接近,海南群体的趋异程度最大。主成分分析建立了3个主成分—壳质量、楯面长、前端到腹缘,其贡献率分别为:31.25%,24.46%,12.39%,积累贡献率为68.10%。判别分析结果显示,6个毛蚶群体的形态差异显著(P<0.01)。建立了6个毛蚶群体的判别函数,其判别准确率P1为82.76%～98.63%,P2为80.00%～100%,综合判别率为91.7%。研究结果为毛蚶的地理群体识别、遗传特征研究、种质资源保护与恢复提供重要的依据。  相似文献   

夏季江苏近海水文化学要素特征及其对沿岸水东北向扩展的指示   总被引：3，自引：0，他引：3  

韦钦胜  葛人峰  李艳  范士亮  傅明珠 《海洋学报》2012,34(5):197-204

  相似文献   

Spatial and temporal variations of sedimented organic matter in Xiaohai Lagoon, Hainan Island   总被引：1，自引：1，他引：0  

LIU Xingjian  GE Chendong 《海洋学报(英文版)》2012,31(3):74-86

The characteristics of grain-size,total organic carbon(TOC) and total nitrogen(TN) contents,TOC/TN ratios,stable carbon isotope(δ13C) and 210 Pb dating were measured in six sediment cores from the Xiaohai Lagoon.The results show distinct spatial and temporal variations in sedimentation patterns.The sediments are dominated by clayey silt,sandy silt and by silty sand in the southern,middle lagoon and the northern lagoon,respectively.TOC and TN contents decline from south to north.Sedimentation rates,determined by 210 Pb dating,tend to decrease from south to middle.However,the determination of sedimentation rate in the north is difficult.These spatial variations are related to the variations in sediment sources and hydrodynamic conditions in the Xiaohai Lagoon.The variations of organic matter signatures can be divided into two stages in the cores from the southern and middle lagoon.Before 1988,the organic matter signatures are relatively stable.The contribution of terrestrial organic carbon sources varies between 60% and 85%.After 1988,the organic matter signatures demonstrate significant variations.TOC and TN contents increase rapidly,TOC/TN ratios decrease,δ13C values shift to higher and the contribution of terrestrial organic carbon sources decreases to 40%-50%.The contributions of phytoplankton organic matter have increased in the sediment since 1988.Increasing aquaculture activities have had a significant impact on organic matter signatures since 1988.The sedimentation rates have increased rapidly in the southern and middle lagoon since 1988 due to the anthropogenic activities which include aquaculture,mining and deforestation.These activities have caused eutrophication and increased siltation in the southern and middle lagoon.  相似文献