自然铜 中华文明的另一种图腾     

刘许生 《湖南地质》2009,(8):82-84

行走在八月，感受铜的季节变幻。八月是铜的季节，因为此时，它显示出价格的最高峰。“亚洲铜，亚洲铜，击鼓之后，我们把在黑暗中跳舞的心脏叫做月亮，这月亮主要由你构成。”在海子的眼里，亚洲铜是民族的图腾，是祖辈们最后的栖息地。这些古老的铜，见证了人类多少兴表，它是与我们祖辈最早亲近的金属之一，成为时间的沙漏。而自然铜，地球上含铜量最纯粹、最高的晶体，却在亿万年“养在深闺人未识”。  相似文献   

大西洋与欧洲沿海的海洋战略角逐     

桑红 《海洋世界》2008,(4):70-75

大西洋位于欧洲、非洲、美洲和南极洲之间,是世界第二大洋。大西洋有多条国际航线,连接欧洲、美洲、非洲的沿岸国家,货运量居各大洋第一位。从地缘政治角度看,大西洋具有极其重要的战略意义,是世界战略资源及国际重要水上通道最密集的地区,美国、西欧和亚洲国家所需的大部分石油,都必须经过大西洋。世界许多重要的海上战略通道都在大西洋,成为西方大国争夺最激烈的地区。“因此,大西洋成为了许多国家高度重视的超级战略大洋。”  相似文献   

第三十届亚洲遥感会议（30ACRS）通知     

吴洁 《地球信息科学学报》2009,(4):460-460

第三十届亚洲遥感会议（30ACRS）将于2009年10月18-23日在北京会议中心召开。亚洲遥感会议是亚洲遥感界发起并推动遥感科学技术发展与交流的盛会,至今已经举办了29届。2009年是亚洲遥感会议三十周年庆典,届时欢迎您的参与!大会组织机构组织单位：亚洲遥感委员会（AARS）中国遥感委员会（CNCRS）主办单位：中国科学院遥感应用研究所中国科学院对地观测与数字地球科学中心国土资源部航空物探遥感中心会议主题———迈向空间时代的亚洲大会欢迎遥感及相关研究领域的专家学者、企业家、学生代表与会,  相似文献   

Critical Approach to Methods of Glacier Reconstruction in High Asia and Discussion of the Probability of a Qinghai-Xizang （Tibetan） Inland Ice     

Matthias Kuhle 《山地科学学报》2007,4(2):91-124

This overview discusses old and new results as to the controversy on the past glacier extension in High Asia, which has been debated for 35 years now. This paper makes an attempt to come closer to a solution. H.v. Wissmann's interpretation (1959) of a small-scale glaciation contrasts with M. Kuhle's reconstruction (1974) of a large-scale glaciation with a 2.4 million km2 extended Qinghai-Xizang (Tibetan) inland glaciation and a Himalaya-Karakorum icestream network. Both opinions find support but also contradiction in the International and Chinese literature (Academia Sinica). The solution of this question is of supraregional importance because of the subtropical position of the concerned areas. In case of large albedo-intensive ice surfaces, a global cooling would be the energetical consequence and, furthermore, a breakdown of the summer monsoon. The current and interglacial heat-low above the very effective heating panel of the Qinghai-Xizang (Tibetan) Plateau exceeding 4000 m, which gives rise to this monsoon circulation, would be replaced by the cold-high of an inland ice. In addition, the plate-tectonically created Pleistocene history of the uplift of High Asia — should the occasion arise up to beyond the snowline (ELA) —would attain a paleoclimatically great, perhaps global importance. In case of a heavy superimposed ice load, the question would come up as to the glacio-isostatic interruption of this primary uplift. The production of the loesses sedimentated in NE-China and their very probable glacial genesis as well as an eustatic lowering of the sea-level by 5 to 7 m in the maximum case of glaciation are immediately tied up with the question of glaciation we want to discuss. Not the least, the problems of biotopes of the sanctuary-centres of flora and fauna, i.e., interglacial re-settlement, are also dependent on it. On the basis of this Quaternary- geomorphological-glaciological connection, future contributions are requested on the past glaciation, the current and glacial permafrost table and periglacial development, the history of uplift, and the development of Ice Age lakes and loess, but also on the development of vegetation and fauna in High Asia.  相似文献   

Information for contributors on Global Geology     

世界地质学 杂志投稿者  亚洲东北 中国吉林大学 《东北亚地学研究》2007,10(1):F0003-F0003

The journal of Global Geology （English Edition ） is sponsored by the International Cen- ter of Geoscience Research and Education in Northeast Asia, Jilin University of China. The former name of the journal was the Journal of International GeoscientiJic Research in Northeast Asia which was started in 1998 and served the scientists and teachers in geosciences in the world, particularly for the scientists from the six countries of the NE Asia including China,  相似文献   

1：500万国际亚洲地质图第三次工作会议在杭州召开     

倪瑛 《浙江国土资源》2007,(11):13

第一份由中国地质学家主持编制的国际亚洲地质图第三次工作会议9月10日至14日在杭州召开,来自法、俄、朝、韩、日等18个国家的33名外国地质学家和60余名中国地质学家参加了这次会议。会议由中国地质科学院地质研究所与浙江省国土资源厅承办。"1:500万国际亚洲地质图"是由联合国教科文组织支持,世界地质图委员会于2004年批准的项目,2005年正式启动,预计2010年完成。由世界地质图会员会南亚和东亚分会、中东分会、北欧亚分会、海底  相似文献   

A coupled model study on the intensification of the Asian summer monsoon in IPCC SRES Scenarios   总被引：1，自引：0，他引：1  

Min WEI 《大气科学进展》2005,22(6):798-806

The Asian summer monsoon is an important part of the climate system. Investigating the response of the Asian summer monsoon to changing concentrations of greenhouse gases and aerosols will be meaningful to understand and predict climate variability and climate change not only in Asia but also globally. In order to diagnose the impacts of future anthropogenic emissions on monsoon climates, a coupled general circulation model of the atmosphere and the ocean has been used at the Max-Planck-Institute for Meteorology. In addition to carbon dioxide, the major well mixed greenhouse gases such as methane, nitrous oxide, several chlorofluorocarbons, and CFC substitute gases are prescribed as a function of time. The sulfur cycle is simulated interactively, and both the direct aerosol effect and the indirect cloud albedo effect are considered. Furthermore, changes in tropospheric ozone have been pre-calculated with a chemical transport model and prescribed as a function of time and space in the climate simulations. Concentrations of greenhouse gases and anthropogenic emissions of sulfur dioxide are prescribed according to observations （1860-1990） and projected into the future （1990-2100） according to the Scenarios A2 and B2 in Special Report on Emissions Scenarios （SRES, Nakcenovic et al., 2000） developed by the Intergovernmental Panel on Climate Change （IPCC）. It is found that the Indian summer monsoon is enhanced in the scenarios in terms of both mean precipitation and interannual variability. An increase in precipitation is simulated for northern China but a decrease for the southern part. Furthermore, the simulated future increase in monsoon variability seems to be linked to enhanced ENSO variability towards the end of the scenario integrations.  相似文献   

Climate change signal analysis for Northeast Asian surface temperature     

Jeong-Hyeong LEE  Byungsoo KIM  Keon-Tae SOHN  Won-Tae KOWN  Seung-Ki MIN 《大气科学进展》2005,22(2):159-171

Climate change detection, attribution, and prediction were studied for the surface temperature in the Northeast Asian region using NCEP/NCAR reanalysis data and three coupled-model simulations from ECHAM4/OPYC3, HadCM3, and CCCma GCMs (Canadian Centre for Climate Modeling and Analysis general circulation model). The Bayesian fingerprint approach was used to perform the detection and attribution test for the anthropogenic climate change signal associated with changes in anthropogenic carbon dioxide (CO2) and sulfate aerosol (SO42-) concentrations for the Northeast Asian temperature. It was shown that there was a weak anthropogenic climate change signal in the Northeast Asian temperature change. The relative contribution of CO2 and SO42- effects to total temperature change in Northeast Asia was quantified from ECHAM4/OPYC3 and CCCma GCM simulations using analysis of variance. For the observed temperature change for the period of 1959-1998, the CO2 effect contributed 10%-21% of the total variance and the di  相似文献   

云南大学亚洲国际河流中心     

《地理学报》2005,60(3):526-527

云南大学亚洲国际河流中心是基于20世纪80年代以来,国家自然科学基金、国家社科基金、国家科技部和云南省科技厅等长期资助国际河流研究的基础上于2000年10月在云南大学成立的。它是我国第一个也是目前唯一一个聚焦国际河流的学术机构。中心主要针对中国及亚洲大陆国际河流为主  相似文献   

阴山及邻区三叠纪富碱侵入岩的成因意义   总被引：5，自引：1，他引：4  

汤艳杰  张宏福  英基丰 《岩石学报》2014,30(7):2031-2040

富碱侵入岩主要包括碱性岩和碱性花岗岩以及碱长花岗岩,其全碱含量(K2O+Na2O)一般8%。碱性岩主要包括正长岩、霞石正长岩、辉石正长岩、霓霞正长岩、闪石正长岩等,在岩石化学上相对贫硅富铝高碱。碱性花岗岩是指含碱性角闪石、碱性辉石的花岗岩,相对富硅贫铝高碱。在各类侵入岩中,富碱侵入岩所占比例很小,其出露面积约占各类侵入岩出露总面积的2%。但是,富碱侵入岩却有重要的矿产和地质意义。富碱侵入岩的研究不仅对于揭示岩石圈地幔的组成特征、壳幔相互作用及其地球动力学背景具有重要的意义,而且,能为有关岩石圈演化、找矿勘查和资源评价工作提供科学依据。根据对现有资料的总结,燕辽-阴山地区目前已发现很多三叠纪的富碱侵入岩体,它们西起内蒙古包头市,东到吉林省的中部,向东一直延伸到朝鲜的北部,大体分布于北纬40°~42°之间(宽度约100km),构成一条近EW向、长达1500km的碱性岩带。阴山及邻区的三叠纪富碱侵入岩分布在包头、凉城、四子王旗、察哈尔右后旗和察哈尔右中旗地区,东边与之相邻的碱性侵入岩主要分布在天镇、阳原和矾山,它们形成于268~190Ma,其中凉城和包头富碱侵入岩的形成年龄较小(197~190Ma)。这些杂岩体的岩石学和地球化学组成变化较大,其SiO2含量变化可从35%到70%。相比之下,四子王旗和察哈尔地区的正长岩具有较高的SiO2和Al2O3含量,较低的TiO2、Fe2O3和MgO,这可能反映了它们是地幔源区物质较高程度部分熔融的产物,而且经历了相对较大程度的辉石、橄榄岩和角闪石的分离结晶作用。绝大多数正长岩具有很低的MgO含量,落在了板片熔融实验(1~4GPa)所产生的熔体范围之内,部分样品具有相对较高的MgO含量和Mg#,落在了来源于大洋板片熔融所产生的埃达克岩范围内,说明这些岩石的形成可能与再循环的俯冲板片熔融有关。这些侵入岩普遍富集轻稀土元素和大离子亲石元素(如Ba,K和Sr)富集、亏损高场强元素(Nb、Ta、Ti)、Th、U和P,其εNd(t)和(87Sr/86Sr)i值的变化范围分别为-17~-3和0.7054~0.7092。多数数据点落在了大洋沉积物的范围内,显示出II型富集地幔参与的特征,即这些正长岩的原始岩浆主要来源于富集的岩石圈地幔。四子王旗正长岩具有最低的εNd(t)值(-17),表明下地壳物质的贡献较大,这与其钾长石的Pb同位素组成特征相一致。现有的Pb同位素数据也表明在研究区富碱侵入岩的岩浆形成过程中有大洋物质的参与。从εNd(t)值与侵入岩形成年龄的相关性变化可以看出,随着形成年龄的减小,下地壳物质的贡献在增加。总之,上述特征表明它们主要来源于富集的岩石圈地幔,并有不同程度的下地壳物质的参与。该富集地幔的形成与古亚洲洋的俯冲作用有关。由于富碱侵入岩通常形成于拉张的构造背景下,因此研究区富碱侵入岩的形成标志着古亚洲洋的闭合以及华北-蒙古陆块碰撞的结束。这些俯冲和碰撞事件造成了华北北缘岩石圈地幔组成和性质的明显改变。该区富碱侵入岩的岩浆活动时空分布规律及其动力学背景尚需精确的年代学和详细的地球化学研究来进一步制约。  相似文献