孟加拉扇沉积作用与古气候研究进展   总被引：1，自引：0，他引：1  

李景瑞  刘升发  吴建政  冯秀丽  孙兴全  曹鹏  王宇童  石学法 《海洋科学》2016,40(6):139-157

"气候-构造-沉积"耦合问题是全球变化研究的重要内容,孟加拉深海扇作为世界第一大浊积扇,沉积物主要来自喜马拉雅山及青藏高原的侵蚀物质,且处于亚洲两大季风区之一的印度季风区,是研究三者相互关系的天然实验室。通过总结该区前人研究成果,对孟加拉扇沉积作用与古气候研究现状进行了综述,提出了该区尚存争议的主要科学问题并展望了今后的研究方向。研究认为,除来自喜马拉雅山和青藏高原的物质外,孟加拉扇还受到印度、东南亚大陆等源区的影响,另外还有少量生物沉积和火山来源物质等。孟加拉扇沉积物以细粒物质为主,扇体表面遍布浊流通道。浊流和等深流是孟加拉扇主要的沉积动力机制。目前对孟加拉扇扇体沉积模式及其在青藏高原隆升、孟加拉扇"源-汇"过程、"气候-构造-沉积"耦合研究中的作用仍存在不同见解,尚需更加深入的研究。  相似文献   

Petrogenesis of the crater-facies Tokapal kimberlite pipe,Indravati Basin,Central India     

N.V. Chalapathi Rao  ;B. Lehmann  ;B.K. Panwar  ;Alok Kumar  ;D. Mainkar 《地学前缘(英文版)》2014,5(6):781-790

New geochemical data of the crater-facies Tokapal kimberlite system sandwiched between the lower and upper stratigraphic horizons of the Mesoproterozoic lndravati Basin a：：e presented. The kimberlite has been subjected to extensive and pervasive low-temperature alteration. Spinel is the only primary phase identifiable, while olivine macrocrysts and juvenile lapilli are largely pseudomorphed （talc-serpentine- carbonate alteration）. However, with the exception of the alkalies, major element oxides display systematic fractionation trends; likewise, HFSE patterns are well correlated and allow petrogenetic interpretation. Various crustal contamination indices such as （SiO2 ＋ AI：：O3 ~ Na20）]（MgO ~ K20） and Si] Mg are close to those of uncontaminated kimberlites. Similar La]Yb （＇79-109） of the Tokapal samples with those from the kimberlites of Wajrakarur （73-145） and Narayanpet （72-156）, Eastern Dharwar craton, southern India implies a similarity in their genesis. In the discriminant plots involving HFSE the Tokapal samples display strong affinities to Group 1I kimberlites from southern Africa and central India as well as to ＇transitional kimberlites＇ from the Eastern Dharwar craton, southern India, and those from the Prieska and Kuruman provinces of southern Africa. There is a striking ~;imilarity in the depleted-mantle （TOM） Nd model ages of the Tokapal kimberlite system, Bastar craton, th~ kimberlites from NKF and WKE Eastern Dharwar craton, and the Majhgawan diatreme, Bundelkhand craton, with the emplacement age of some of the lamproites from within and around the Palaeo~Mesoproterozoic Cuddapah basin, southern India. These similar ages imply a major tectonomagmatic event, possibly related to the break- up of the supercontinent of Columbia, at 1.3-1.5 Ga across the l：hree cratons. The ＇transitional＇ geochemical features displayed by many of the Mesoproterozoic po~：assic-ultrapotassic rocks, across these Indian cratons are inferred to be memories of the metasomatisi  相似文献   

印度震动反馈导航鞋问世，告别地图去旅行     

《中国测绘》2014,(3):86-86

据《每日邮报》网站报道．印度班加罗尔的两名工程学学生研发出一款名为Lechal智能导航鞋。只要穿上它．即便来到完全陌生的城市．也能被导航到目的地。  相似文献   

The morphotectonics and its evolutionary dynamics of the central Southwest Indian Ridge (49° to 51°E)   总被引：1，自引：1，他引：0  

LIANG Yuyang  LI Jiabiao  LI Shoujun  RUAN Aiguo  NI Jianyu  YU Zhiteng  ZHU Lei 《海洋学报(英文版)》2013,32(12):87-95

The morphotectonic features and their evolution of the central Southwest Indian Ridge （SWIR） are dis- cussed on the base of the high-resolution flfll-coverage bathyraetric data on the ridge between 49°-51°E. A comparative analysis of the topographic features of the axial and flank area indicates that the axial topogra- phy is alternated by the ridge and trough with en echelon pattern and evolved under a spatial-temporal mi- gration especially in 49°-50.17°E. It is probably due to the undulation at the top of the mantle asthenosphere, which is propagating with the mantle flow. From 50.17° to 50.7°E, is a topographical high terrain with a crust much thicker than the global average of the oceanic crust thickness. Its origin should be independent of the spreading mechanism of ultra-slow spreading ridges. The large numbers of volcanoes in this area indicate robust magmatic activity and may be related to the Crozet hot spot according to RMBA （residual mantle Bouguer anomaly）. The different geomorphological feature between the north and south flanks of the ridge indicates an asymmetric spreading, and leading to the development of the OCC （oceanic core complex）. The tectonic activity of the south frank is stronger than the north and is favorable to develop the OCC. The first found active hydrothermal vent in the SWIR at 37°47＇S, 49°39＇E is thought to be associated with the detach- ment fault related to the OCC.  相似文献   

Component characteristics of organic matter in hydrothermal barnacle shells from Southwest Indian Ridge     

HUANG Xin  ZENG Zhigang  CHEN Shuai  YIN Xuebo  WANG Xiaoyuan  ZHAO Huijing  YANG Baoju  RONG Kunbo  MA Yao 《海洋学报(英文版)》2013,32(12):60-67

In 2008-2009, hydrothermal barnacle and sediment samples were collected from the Southwest Indian Ridge during a survey of the China Ocean Mineral Resources R＆D Association （COMRA）. Samples were ana- lyzed by gas chromatography-mass spectrometer （GC-MS）, revealing the main organic constituents of hy- drothermal barnacle and sediment to be fatty acids and alkylbenzenes. N-alkanes which possessed obvious even carbon advantage were also detected in hydrothermal sediment. The high concentrations of aromatic compounds might be the result of macromolecular thermal alteration. Microorganism in the submarine hydrothermal ecosystem, especially those related to sulfur metabolism, might be the source of the high con- centrations of fatty acids detected in these samples. In high temperature and high pressure hydrothermal environments, n-alkanes which possessed obvious even carbon advantage might originate from thermal alteration of carboxylic acids and other lipid compounds.  相似文献   

体积排阻高效液相色谱-电感耦合等离子体质谱法同时测定印度芥菜(Brassica Juncea)中镉铜锌形态   总被引：2，自引：1，他引：1  

杨红霞  刘崴  李冰  魏巍  张惠娟  陈登云 《岩矿测试》2010,29(1):9-13

建立了体积排阻高效液相色谱-电感耦合等离子体质谱法同时测定印度芥菜中镉、铜、锌形态分析方法。为了防止巯基化合物氧化反应的发生,样品采取液氮保护并在-70℃保存,样品分析全流程采取氮吹防氧化措施。在镉、铜、锌胁迫下,诱导产生植物螯合肽(PCs)。在叶片和根部均检测到3种元素的4种形态,植物螯合肽(PC)3-Cd(Cu,Zn)、植物螯合肽(PC)2-Cd(Cu,Zn)、谷胱甘肽(GSH)-Cd(Cu,Zn)、半胱胺酸(Cys)-Cd(Cu,Zn)及其在植物体内的分布规律。结合植物不同部位Cd、Cu、Zn分布规律初步推断,Cd、Cu、Zn在与GSH及Cys的结合上存在竞争。  相似文献   

大陆动力学研究提出新认识青藏高原隆升: 印度/亚洲板块五阶段碰撞推进     

本刊编辑部 《地球学报》2010,31(6):832-832

在2010年9月召开的中法青藏高原动力学国际研讨会上,中国地质科学院地质研究所研究员、中国科学院院士许志琴等展示了青藏高原大陆动力学研究最新成果:印度/亚洲板块碰撞大地构造格架及碰撞五阶段论,引起国内外青藏科学家的关注和反响。  相似文献   

正在变弱的印度季风和ENSO相关关系          下载免费PDF全文

K.Krishna Kumar  Balaji Rajagopalan  Mark A.Cane  赵连伟 《气象与环境学报》2000,17(1):51-54

对 140a历史资料的分析表明 :ELNino 南方涛动 (ENSO)与印度夏季风的反相关关系 (暖ENSO事件产生弱季风 )在近 10a来已经破坏了。有 2种可能原因。首先 ,与ENSO事件相关的瓦克环流向东南移可能导致了印度地区下沉气流减弱 ,因而有利于加强季风。另外 ,冬春季欧亚大陆地面温度升高———这是中纬度大陆变暖趋势的一部分 ,可能有利于加强陆地—海洋热力梯度 ,因而导致强季风的爆发。这就增加了这样一种可能性 :即近 1 0a来欧亚大陆变暖有助于维持正常水平的季风降水 ,尽管在这期间发生了强ENSO事件  相似文献   

2000年6月4日印度尼西亚苏门答腊7.3级地震概述     

张春艳  张洪由 《国际地震动态》2000,(9):18-20

据《新华社》、《美联社》、《路透社》等多家新闻媒体报道 ,2 0 0 0年 6月 4日午夜 ,印度尼西亚苏门答腊岛西南部海域连续发生两次强烈地震 ,造成了惨重的人员伤亡和财产损失。1　地震参数1.1　发震时间主震发生在当地时间 2 0 0 0年 6月 4日 2 3时 2 8分 ;北京时间 6月 5日零时 2 8分 ;格林尼治时间 6月 4日 16时 2 8分。地震持续了数分钟 ,约 11分钟后 ,又发生了一次 6级 (美国地质调查局测定为 6.7级 )强余震。此后余震不断 ,仅震后 2天就记录到 2 0 0多次余震 ,进一步加剧了灾区的人员伤亡和财产损失及人们的恐慌心理。据有关地质专家…  相似文献   

我国西部地震群体活动特征研究   总被引：1，自引：1，他引：0  

赵振才  陈兵 《地震》2000,20(1):80-84

在对我国西部本世纪第五个地震活跃幕以来地震群体活动时空强演变规律回顾的基础上,研究了近１～２年中强地震的分布特点,结合大地形变的演变状况,对本区地震活动进行了研究,并认为本区处于本活跃幕末的翘尾活动阶段。  相似文献