云南元江地区铜矿GIS预测时的找矿有利度和空间相关性分析

以云南元江地区铜矿ＧＩＳ预测为例,介绍了线型异常和面型异常的找矿有利度分析方法,并给出断裂、物化探异常和地层找矿有利度分析的结果．给出了计算空间相关性的公式,并研究了不同元素化探异常的空间相关性．研究了相关元素的组合异常,论证了在矿产资源预测中应用组合异常的必要性．     

Culm Plants from Northern Kuangtung

正 In February 1943 some valuable specimens of plant fossils were collected by the members of the Geological Survey of Kuangtung and Kuangsi from a coal series in     

胶莱盆地蛇窝泊地区白垩纪林寺山组沉积时代与物源特征:来自碎屑锆石U-Pb测年与稀土元素组成的新证据

林寺山组是胶莱盆地莱阳群底部重要的地层单元之一.准确限定其沉积时代与物源性质对于客观重建华北陆块东部晚中生代大地构造格局以及周缘造山带/前寒武纪变质基底晚中生代的折返过程具有重要的制约作用.以莱阳盆地蛇窝泊地区莱阳群林寺山组细砾岩为研究对象,对其开展了野外地质调查、岩相学观察、锆石U-Pb测年与锆石稀土元素分析等综合研...     

再论塔里木板块的归属问题

长期以来，对塔里木板块属于华北板块？扬子板块？还是一个独立的板块？一直存在争议。本文根据塔里木板前寒武纪基底的性质，古生代沉积建造序列，生物古地理区系的面貌和古地磁资料认为：（１）塔里木是属于前寒武纪陆壳基底的独立板块，与周边板块之间的存在不同规模的洋盆；（２）早古生代时，塔里木位于南半球，更接近于扬子板块，而远离华北板块（３）在古生代一中生代时，塔里木板块与周边坡板块先后碰撞，直到三叠纪末，塔里     

哀牢山-红河左旋走滑剪切带中新世抬升的时间序列

在哀牢山-红河剪切带的元阳到者龙的6个不同地点,对18个变质岩样品进行系统分析钾长石的~(40)Ar-~(39)Ar年龄。发现用MDD模式得到的18条冷却曲线(温度范围在400-150℃之间)均存在一次(或两次)快速冷却过程(冷却速度>100°C/Ma),这种快速冷却(抬升)过程不仅反映了该剪切带在大约25-17Ma时,韧性走滑作用结束和正断作用的开始,而且它的起始时间还有自东南向西北逐渐变新的趋势。利用6个不同地点快速冷却(抬升)的起始时间与相对距离作图时,得到了较好的线性函数关系(斜率为34mm/a)     

空间分析技术与地理信息系统的结合*

空间分析和地理信息系统是两种有效的空间信息分析和处理技术,二者的结合一方面可以大大拓展GIS的空间分析功能,另一方面也可使得迅速发展的空间分析得到GIS的有力支持,文中对此进行了探讨,并分析了二者结合的途径。     

Ecological compensation for desertification control: A review

Desertification control is a crucial way to enhancing the ecological conditions of arid and semi-arid regions, and maintaining sustainable development globally. Designing and improving an ecological compensation mechanism for desertification control has great significance related to achieving balance amongst the needs of different economic subjects and the assurance of a sustained and stable supply of desert ecosystem services. In this paper, (1) the theoretical bases of ecological compensation for desertification control were re-analyzed; (2) the research status and challenges of three important topics related to ecological compensation for desertification control were systemically discussed, including compensation standards, ecosystem service supply-consumption process and multi-scale effects, and resource- environment basis and policy orientation; (3) a research framework of ecological compensation for desertification control based on the process of desert ecosystem service supply–flow–consumption was proposed; (4) and finally, seven priority research issues were discussed, which aimed to support ecological compensation policy-making and ecological engineering implementation for desertification control.     

中国区域水汽输送异常与长江流域旱涝的关系

The characteristics of water vapor transport (WVT) over China and its relationship with precipitation anomalies in the Yangtze River Basin (YRB) are analyzed by using the upper-air station data in China and ECMWF reanalysis data in summer from 1981 to 2002. The results indicate that the first mode of the vertically integrated WVT is significant whose spatial distribution presents water vapor convergence or divergence in the YRB. When the Western Pacific Subtropical High (WPSH) is strong and shifts southward and westward, the Indian Monsoon Low Pressure (IMLP) is weak, and the northern part of China stands behind the middle and high latitude trough, a large amount of water vapor from the Bay of Bengal (BOB), the South China Sea (SCS) and the western Pacific forms a strong and steady southwest WVT band and meets the strong cold water vapor from northern China in the YRB, thus it is likely to cause flood in the YRB. When WPSH is weak and shifts northward and eastward, IMLP is strong, and there is nearly straight west wind over the middle and high latitude, it is unfavorable for oceanic vapor extending to China and no steady and strong southwest WVT exists in the region south of the YRB. Meanwhile, the cold air from northern China is weak and can hardly be transported to the YRB. This brings on no obvious water vapor convergence, and then less precipitation in the YRB. Foundation: International Technology Cooperation Project of the Ministry of Science and Technology of China, No. 2007DFB20210; Application Technology Research and Development Project of Sichuan Province, No. 2008NG0009; Basic Research Foundation of Institute of Chengdu Plateau, China Meteorological Administration, No.BROP2000802 Author: Jiang Xingwen (1983–), specialized in the study of climate diagnosis.     

海岸沙丘成因的讨论

本文以中国和西非二个典型沙丘海岸为例,说明海滨沙丘是海陆相互作用下形成的,特别是在冰期极地气候条件下,低海面时形成广大的岸外沙质浅滩,极地气旋风暴作用,促进海岸沙丘的形成发育。     

雅鲁藏布江曲水-泽当段风沙活动动力条件分析与风沙灾害防治建议

雅鲁藏布江河流宽谷区是青藏高原风沙活动最为强烈地区之一.本文选择雅鲁藏布江曲水-泽当段为研究区,分析该地区1981-2010年以来的风动力条件变化特征.结果表明:1981年以来年平均风速明显降低,月平均风速2-4月最大.受河流-山地复合系统的影响,风向复杂且具有明显的空间差异性,贡嘎以西风和东风为主,泽当包括西风、南风...