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今年《地质论评》已出版50卷。我国超过50卷的学术刊物是很少的,《地质论评》刊出50卷是个值得庆贺的时刻。《地质论评》1936年创刊,1951年出到第16卷时,与“Bulletin of Geological Society of China”《中国地质学会会志》(英文、法文、德文)合并为中文版的《地质学报》。随着地质工作的蓬勃发展和国际交流日益频繁。中国地质学会事理会会议决定恢复《地质论评》,     

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冰川冻上第17卷（1995）

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《中国可持续发展总纲》第3卷 《中国能源与可持续发展》

<正>2007年2月由科学出版社出版的宏篇巨著《中国可持续发展总纲》丛书分国家卷(共20卷,1350万字)和区域卷(共31卷),由路甬祥院士任总主编,牛文元教授任执行总主编。国家卷涵盖了中国人口、资源、     

水科学进展第14卷(2003年)单位索引

北京大学　·激光测速粒子对复杂流动的响应研究———Ⅰ颗粒非恒定运动数学模型及其数值方法 (第 14卷　第 1期　 2 0 0 3年 1月 )　·激光测速粒子对复杂流动的响应研究———Ⅱ典型流场中粒子跟随性的数值分析 (第 14卷　第 1期　 2 0 0 3年 1月 )　·中国水系的盒维数及其关系 (第 14卷　第 6期　 2 0 0 3年 11月 )　·湖泊富营养化模型的研究现状与发展趋势 (第 14卷　第 6期　 2 0 0 3年 11月 )北京师范大学　·国际河流的水权及其有效利用和保护研究 (第 14卷　第 1期　 2 0 0 3年 1月 )　·吉林省水资源可持续利用研究 (第 14卷　第…     

水科学进展第18卷（2007年）作者索引

曹勇陈吉余·长江口南汇东滩近岸淡水资源的成因探讨(第18卷第3期2007年5月)曹云黄志刚郑华欧阳志云·柑桔园林下穿透雨的分布特征(第18卷第6期2007年11月)曹建廷秦大河罗勇赵建世·长江源区1956-2000年径流量变化分析(第18卷第1期2007年1月)陈建韩小波丁登山金洪钧·工业废水和城市综合污水的环境风险管理(第18卷第4期2007年7月)陈权李震王磊·机载雷达和辐射计数据反演植被覆盖区土壤水分的初步研究(第18卷第5期2007年9月)陈吉余·河流健康的定义与内涵(第18卷第1期2007年1月)陈锦年王宏娜吕心艳·南海区域海气热通量的变化特征分析(第18…     

湖南地质(第20卷总索引)

第期1溆浦陆相红盆地质特征及其演化探讨 (Discussion on the Geological Characteristics and the Evolution… of Xupu Red Basin of Continental Facies) …………李福顺(1)湘西南震旦纪长安期沉积相变与构造环境分析 (Analyzing the Facies Change of Sedimentary Facies and the Structural Environment in the Chang-an Stage of Sinian Period in South-Western Hunan………………)柏道远(5)湘南地区表生氧化锰矿地球化学行为及成矿机理研究(Research for the Geochemical Behaviors and the Genesis Mechanism of Hypog…     

水科学进展 第15卷（2004年） 单位索引

安徽建筑工程学院　·拟序结构下空泡近壁区运动规律研究 (第 15卷　第 3期　 2 0 0 4年 5月 )安徽省环境保护局　·酸雨研究进展与问题探讨 (第 15卷　第 4期　 2 0 0 4年 7月 )安徽省环境保护科学研究所　·枯水研究进展 (第 15卷　第 2期　 2 0 0 4年 3月 )澳大利亚墨尔本大     

印度盐岭寒武纪动物群 金氏著

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Rapid erosion of the coast of Sagar island, West Bengal - India

The coastal zone of the Sagar island has been studied. The island has been subjected to erosion by natural processes and to a little extent by anthropogenic activities over a long period. Major landforms identified in the coastal area of the Sagar island are the mud flats/salt marshes, sandy beaches/dunes and mangroves. The foreshore sediments are characterized by silty, slightly sandy mud, slightly silty sand and silty sand. Samples 500 m inland from high waterline are silty slightly sandy mud, and by clayey slightly sandy mud. The extent of coastline changes are made by comparing the topographic maps of 1967 and satellite imageries of 1996, 1998 and 1999. Between 1967 and 1999 about 29.8 km² of the island has been eroded and the accreted area is only 6.03 km². Between 1996 and 1998 the area underwent erosion of 13.64 km² while accretion was 0.48 km². From 1998 to 1999, 3.26 km² additional area was eroded with meager accretion. Erosion from 1997 to 1999 was estimated at 0.74 km² /year; however, from 1996 to 1999, the erosion rate was calculated as 5.47 km²/year. The areas severely affected by erosion are the northeastern, southwestern and southeastern faces of the island. As a consequence of coastal erosion, the mud flats/salt marshes, sandy beaches/dunes and mangroves have been eroded considerably. Deposition is experienced mainly on the western and southern part of the island. The island is built primarily by silt and clay, which can more easily be eroded by the waves, tides and cyclonic activities than a sandy coast. Historic sea level rises accompanied by land subsidence lead to differing rates of erosion at several pockets, thus periodically establishing new erosion planes.     

Sri Lanka - India Intraplate Tectonics - Precambrian to Present

The tectonic history of Sri Lanka - India can be traced from the Precambrian to the present. On the basis of the geological record, plate tectonic processes have operated for example, the Highland Group of Sri Lanka may have represented a Precambrian plate tectonic suture. Tectonic models of these Precambrian events may be presented by spreading, collision, subduction, shearing or in situ jostling. The recent tectonic history of Sri Lanka and India relates to the evolution of the Indian Ocean since at least the Cretaceous. Although Sri Lanka is considered to be a part of the larger Indo - Australian plate, it may have had a local independent history as a block within the larger crustal unit of India. There is evidence that the separation of Sri Lanka from India was in part controlled by Precambrian structures and a history of translational, rotational and vertical adjustments to the Indian Ocean developmental plate tectonic stresses still operating.     

Chloritoid from low-grade schists. Singhbhum,Eastern India

Chloritoid-sericite schists from the chlorite zone of the regionally metamorphosed Singhbhum anticlinorium in Eastern India are described with regard to the formation of chloritoid during prograde metamorphism — the main stage of its crystallisation was coeval with the movement. The movements accompanying metamorphism have had a marked effect on the lattice orientation of this mineral, so that its crystallographic axis is roughly parallel to the regional fold axis. In one case chloritoid appears to be in stable association with hematite, i.e. it persists beyond the magnetite-hematite equilibrium, which is probably a local effect due to a slight rise in oxygen partial pressure in the last stages of metamorphism. The occurrence of phengitic mica in these schists is suggestive of high total pressures and high water pressures.