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排序方式: 共有9188条查询结果,搜索用时 171 毫秒
921.
922.
923.
924.
农坪金(铜)矿床受控于东西向断裂构造带,产于英云闪长(斑)岩蚀变岩中,与闪长玢岩密切相关。矿床成因类型为次火山热液含金慢变岩型。矿床类型特殊,外围找矿潜力较大,对珲春地区金、铜找矿具有指导意义。 相似文献
925.
地球表层是地球各层圈相互作用并进行物质,能量和信息交换的重要场所,它为人类提供了生存的空间和资源。由于天然和人为的作用,地球表层环境遭受的破坏日益严重,威胁着人类的生存和发展。加强地球表层系统的研究,有计划地编制地球表层系统系列地质图件,是地质工作服务于经济建设和社会发展的一项重要任务。 相似文献
926.
北京地区重磁数据计算机图像处理及地质效果 总被引:2,自引:1,他引:1
介绍了对北京地区重力和磁力数据进行计算机图像处理的技术及流程,解译了重磁数据图像处理结果,分析了重磁数据计算机图像处理的地质效果,得到了一些对北京地区成矿预测有益的新认识 相似文献
927.
The Quaternary geological environment supplied mankind with a habitat and rich natural resources such as forest, meadow,
water, etc. Mankind has developed to modern civilization through a very long history. During the last 100 years the area of
desertification has been expanding, natural resources have been consumed, and eco-environments plundered. Mankind felled forests,
cultivated grassland, and increased farmland because of unceasing increasing population and the need for materials. In a period
of 50–100 years, mankind's destruction could change good meadow into desert. The following examples are evidence: Shangdu
grassland in Inner Mongolia and the west grassland of Jilin Province have been changing into desert rapidly. Two concepts
of destructive power (D) and bearing capacity (B) can be used to describe this process. When D<B, the ecosystem keeps good circulation, D=B, eco-balance reaches critical state, and D>B, ecosystem loses balance, the environment is destroyed and developed toward desert. The law of destructive power increasing
with time accords with logistic curves and can be expressed by a logistic model. Destructive power (D) increases with decrease of bearing capacity (B);D and B represent a reciprocal relation. With a logistic model the developing process of desertification can be studied and the developing
rate and strength of change can be forecasted.
Received: 20 July 1998 · Accepted: 1 December 1998 相似文献
928.
试论中国古大陆中-新元古代汇聚与裂解的地质记录 总被引:1,自引:0,他引:1
自1990年新元古Rodinia超大陆提出后,现已发展成地学研究热点之一。在全球新元古代超大陆旋回的汇聚与裂解机制影响下,中国古大陆也随之变化。中元古代末一新元古代初的汇聚和新元古代晚期的裂解是最重要的两次地质事件。塔里木、华北、华南古陆都有它的地质记录。晋宁事件应是中元古代晚期-新元古代早期,北秦岭地块与中秦岭地块俯冲一碰撞造山作用和新元古代时期Rodinia超大陆形成的主要地质事件;华南的武陵运动,使华夏古陆与扬子地块发生碰撞形成统一的“华南古陆”。在塔里木古陆与哈萨克斯坦一伊犁古陆之间的那拉提南缘碰撞带,甘肃北山南带柳园及青海柴达木盆地北部边缘的榴辉岩一花岗岩带的发现都是最新的研究成果。 相似文献
929.
通过对地勘单位资金短缺,资产质量低下等现状剖析,提出加强资金、资产管理,降低资金成本和费用支出的设想和具体办法,向管理要效益,使地勘经济健康发展。 相似文献
930.
Contributions of groundwater conditions to soil and water salinization 总被引:23,自引:2,他引:21
Salinization is the process whereby the concentration of dissolved salts in water and soil is increased due to natural or
human-induced processes. Water is lost through one or any combination of four main mechanisms: evaporation, evapotranspiration,
hydrolysis, and leakage between aquifers. Salinity increases from catchment divides to the valley floors and in the direction
of groundwater flow. Salinization is explained by two main chemical models developed by the authors: weathering and deposition.
These models are in agreement with the weathering and depositional geological processes that have formed soils and overburden
in the catchments. Five soil-change processes in arid and semi-arid climates are associated with waterlogging and water. In
all represented cases, groundwater is the main geological agent for transmitting, accumulating, and discharging salt. At a
small catchment scale in South and Western Australia, water is lost through evapotranspiration and hydrolysis. Saline groundwater
flows along the beds of the streams and is accumulated in paleochannels, which act as a salt repository, and finally discharges
in lakes, where most of the saline groundwater is concentrated. In the hummocky terrains of the Northern Great Plains Region,
Canada and USA, the localized recharge and discharge scenarios cause salinization to occur mainly in depressions, in conjunction
with the formation of saline soils and seepages. On a regional scale within closed basins, this process can create playas
or saline lakes. In the continental aquifers of the rift basins of Sudan, salinity increases along the groundwater flow path
and forms a saline zone at the distal end. The saline zone in each rift forms a closed ridge, which coincides with the closed
trough of the groundwater-level map. The saline body or bodies were formed by evaporation coupled with alkaline-earth carbonate
precipitation and dissolution of capillary salts.
Received, May 1998 · Revised, July 1998 · Accepted, September 1998 相似文献