全文获取类型
收费全文 | 6405篇 |
免费 | 1133篇 |
国内免费 | 1231篇 |
专业分类
测绘学 | 408篇 |
大气科学 | 338篇 |
地球物理 | 507篇 |
地质学 | 4430篇 |
海洋学 | 1016篇 |
天文学 | 14篇 |
综合类 | 600篇 |
自然地理 | 1456篇 |
出版年
2024年 | 18篇 |
2023年 | 93篇 |
2022年 | 215篇 |
2021年 | 280篇 |
2020年 | 235篇 |
2019年 | 302篇 |
2018年 | 227篇 |
2017年 | 234篇 |
2016年 | 268篇 |
2015年 | 270篇 |
2014年 | 326篇 |
2013年 | 323篇 |
2012年 | 322篇 |
2011年 | 379篇 |
2010年 | 339篇 |
2009年 | 364篇 |
2008年 | 357篇 |
2007年 | 396篇 |
2006年 | 434篇 |
2005年 | 386篇 |
2004年 | 403篇 |
2003年 | 335篇 |
2002年 | 322篇 |
2001年 | 300篇 |
2000年 | 267篇 |
1999年 | 236篇 |
1998年 | 213篇 |
1997年 | 159篇 |
1996年 | 170篇 |
1995年 | 124篇 |
1994年 | 104篇 |
1993年 | 91篇 |
1992年 | 61篇 |
1991年 | 65篇 |
1990年 | 42篇 |
1989年 | 27篇 |
1988年 | 21篇 |
1987年 | 12篇 |
1986年 | 13篇 |
1985年 | 10篇 |
1984年 | 7篇 |
1983年 | 6篇 |
1982年 | 9篇 |
1981年 | 2篇 |
1979年 | 1篇 |
1978年 | 1篇 |
排序方式: 共有8769条查询结果,搜索用时 46 毫秒
131.
柱撑粘土矿物层间域的性质及其环境意义 总被引:10,自引:3,他引:10
柱撑粘土矿物是近年来胺国内外矿物学广泛关注的矿物材料之一。柱撑粘土矿物层间域是一个特殊的化学反应场所。本系统评述了氮氧化物、重金属离子、阴离子、肥料养分及有机污染物等环境污染物在柱撑粘土矿物层间域中的催化还原、吸附、脱附、控释及光催化反应机理,着重阐述了柱撑粘土矿物的层间域性质,讨论了它们的环境化学行为对环境的影响和意义。 相似文献
132.
133.
The Trypali carbonate unit (Upper Triassic), which crops out mainly in central‐western Crete, occurs between the parautochthonous series (Plattenkalk or Talea Ori‐Ida series, e.g. metamorphic Ionian series) and the Tripolis nappe (comprising the Tripolis carbonate series and including a basal Phyllite–Quartzite unit). It consists of interbedded dolomitic layers, represented principally by algally laminated peloidal mudstones, foraminiferal, peloidal and ooidal grainstones, as well as by fine‐grained detrital carbonate layers, in which coarse baroque dolomite crystals and dolomite nodules are dispersed. Baroque dolomite is present as pseudomorphs after evaporite crystals (nodules and rosettes), which grew penecontemporaneously by displacement and/or replacement of the host sediments (sabkha diagenesis). However, portions of the evaporites show evidence of resedimentation. Pre‐existing evaporites predominantly consisted of skeletal halite crystals that formed from fragmentation of pyramidal‐shaped hoppers, as well as of anhydrite nodules and rosettes (salt crusts). All microfacies are characteristic of peritidal depositional environments, such as sabkhas, tidal flats, shallow hypersaline lagoons, tidal bars and/or tidal channels. Along most horizons, the Trypali unit is strongly brecciated. These breccias are of solution‐collapse origin, forming after the removal of evaporite beds. Evaporite‐related diagenetic fabrics show that there was extensive dissolution and replacement of pre‐existing evaporites, which resulted in solution‐collapse of the carbonate beds. Evaporite replacement fabrics, including calcitized and silicified evaporite crystals, are present in cements in the carbonate breccias. Brecciation was a multistage process; it started in the Triassic, but was most active in the Tertiary, in association with uplift and ground‐water flow (telogenetic alteration). During late diagenesis, in zones of intense evaporite leaching and brecciation, solution‐collapse breccias were transformed to rauhwackes. The Trypali carbonate breccias (Trypali unit) are lithologically and texturally similar to the Triassic solution‐collapse breccias of the Ionian zone (continental Greece). The evaporites probably represent a major diapiric injection along the base of the parautochthonous series (metamorphic Ionian series) and also along the overthrust surface separating the parautochthonous series from the Tripolis nappe (Phyllite–Quartzite and Tripolis series). The injected evaporites were subsequently transformed into solution‐collapse breccias. 相似文献
134.
The Dead Sea, the Holocene terminal lake of the Jordan River catchment, has fluctuated during its history in response to climatic change. Biblical records, calibrated by radiocarbon-dated geological and archaeological evidence, reinforce and add detail to the chronology of the lake-level fluctuations. There are three historically documented phases of the Dead Sea in the Biblical record: low lake levels ca. 2000–1500 B.C.E. (before common era); high lake levels ca. 1500–1200 B.C.E.; and low lake levels between ca. 1000 and 700 B.C.E. The Biblical evidence indicates that during the dry periods the southern basin of the Dead Sea was completely dry, a fact that was not clear from the geological and archaeological data alone. 相似文献
135.
136.
The salinized sandy lands are the important reclaimable reserve wastelands in thesouth area of the Xinjiang Uygur Autonomous Region of China. But it is necessary that the eco-logical environment of the area is not destroyed by action of oasis development. The main factor tohinder oasis development is land salinization. Rational oasis establishment rebuilds wastelandswith lower productivity and utilization efficiency for the growth of agriculture, forestry, and stock raising. The results of surveying sub-soil environment of Aimugaike. Awati oasis in Hotian County ofthe Xinjiang Uygur Autonomous Region show that the underground water and soil environment arenot deteriorated under the rational management and administration, which could be coordinatedfor obtaining economic and environmental benefit. During the oasis establishment period from1997 to 1999, the plowland area has reached 166.7 hm2, and the seed cotton yield per unit areahas reached 2250 kg @ hm-2, the area of timber forest and active sand break forest has reached 20hm2, the area of fruit trees is 71.5 hm2; and the soil moisture has decreased from 22.07% to18.12%. In the first year of oasis establishment, the soil type has changed salt soil into light saltsoil, in the second year the soil has been out of salt harm; and the content of soil organic matter intopsoil has increased obviously. 相似文献
137.
Florias Mees 《地球表面变化过程与地形》2002,27(7):719-735
In a region along the western margin of the Kalahari in eastern Namibia and western Botswana, many pan basins have mainly calcareous deposits along part of their margins. These are typically lined by low vertical scarps. In Namibia, these pans are mainly located in dry river beds. The petrographical study of these deposits demonstrates that they consist of lacustrine sediments that have to a varying extent been affected by early‐diagenetic processes and by the formation of late‐diagenetic features. The original composition of the deposits ranges from highly calcareous sediments, typically with ostracod, diatom and charophyte remains, to entirely non‐calcareous diatomites. The deposits generally show an upward increase in total carbonate content, which is mainly a synsedimentary feature. The early‐diagenetic processes that affected the deposits include the formation of orthic siliceous nodules. At a later stage, secondary calcite enrichment occurred, leaving only the silica‐impregnated sections unaffected. This enrichment partly accounts for the upward increase in total carbonate content in some profiles and often resulted in the development of a highly calcareous surface horizon. Sepiolite and amorphous silica that are part of the groundmass of the deposits may also partly have formed at this stage. Late‐diagenetic features include various forms of secondary calcite and silica. This study of pan basins in eastern central Namibia indicates that a lacustrine rather than purely pedogenic origin should also be considered for calcareous deposits that commonly occur along pan margins in other parts of southern Africa. Copyright © 2002 John Wiley & Sons, Ltd. 相似文献
138.
139.
东北地区生态环境保育与绿色社区建设 总被引:12,自引:6,他引:12
20世纪以来,东北地区资源环境发生了巨大的变化,为全球范围内具有有短时限人地关系高强度作用特征的典型地区之一。区域资源过量消耗、生态环境趋于恶化,可持续发展面临威胁,保育生态环境成为一项十分迫切的任务。建设“绿色社区”,是生态保育的有效措施和重要内容,也是生态建设的一项基础工程,建立绿色社区的目标的营造绿色文化、保育绿色生态和发展绿色经济,建立绿色社区的基本任务是发展生态经济,保育生态环境,解决农村生态环境退化,促进城市可持续发展。提出了绿色社区建设的实施方案。 相似文献
140.
西北五省(区)生态环境综合分区及其建设对策 总被引:17,自引:2,他引:17
本文以图像遥感解译为主 ,结合野外实际考察 ,并通过抽样验证完成。在对生态环境界定和赋予内涵的基础上 ,根据区划目的、原则和所选取的指标体系 ,从生态环境分类入手 ,经过从上向下续分和由下向上合并的反复磨合过程、专家集成模拟 ,对西北五省(区 )生态环境做了全面的综合分区研究 ,并针对所存在的生态环境问题 ,提出生态环境保护和建设的对策 ,为西北五省 (区 )实施西部大开发生态环境监测、治理、建设和规划提供科学依据。 相似文献