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721.
区域物流中心(城市)空间体系及驱动机理研究 总被引:3,自引:0,他引:3
物流中心城市空间体系是指在一定地域范围内以物流枢纽城市为核心,以具有经济优势和物流组织条件的边缘城市为支持而构成的空间有机体。本文以安徽省为例证,建立物流巾心(城市)模糊区间层次(IGJAHP)综合评判模型,测算安徽省17个城市的物流发展水平,评判物流中心(城市)的等级;探讨物流中心(城市)的功能及发展模式;在此基础上,引用“轴-辐(hub—and—spokes)”空间理论,构筑以芜湖-合肥为双核心,以蚌埠、阜阳、安庆等为支持的区域物流中心HS空间格局;最后,从商流中心、交通网络、内外部经济效益以及物流技术等诸方面,探讨物流中心(城市)空间体系演进的驱动机理,以期推动安徽省区域物流的发展。 相似文献
723.
文章利用海洋台站观测资料,对3类再分析资料的气温、海表温度数据在江苏海域进行比较分析。结果表明:总体而言,气温、海表温度的再分析数据与观测数据均具有很高的一致性,且海表温度再分析数据与观测数据的一致性高于气温再分析数据;在3种再分析资料中,ERA5的可靠性优于JRA-55和NCEP;在离岸较远的外磕脚测点,再分析数据与观测数据的一致性高于另2个测点;在台风影响期间,吕四测点、外磕脚测点的再分析数据与观测数据更为接近,在更近岸的连云港测点,再分析数据与观测数据的差异更大;在冷空气造成的气温下降期间,再分析数据与观测数据的差异较小,但在气温缓步回升期间,吕四测点、外磕脚测点的再分析数据明显高于观测数据;在冷空气影响过程中,再分析数据反映的海表温度下降幅度明显低于观测数据。本研究可为再分析资料在江苏海域的适用性和可信度提供评估依据。 相似文献
724.
以青藏高原查拉坪地区一处热融湖塘(40 m×50 m,最大深度为1 m)为研究对象,由实测数据对比分析了热融湖塘与天然地表相同深度的温度变化特征.结果表明:与天然地表相比,热融湖塘融化时间长,冻结时间短,且存在接近4℃的水温变化;受太阳辐射及热对流的影响,垂向水温梯度仅在水表从4℃降温及冻结阶段较大,其余时段接近0;湖底年均温度比相同深度的天然地表高约6.4℃,湖底下部存在约14 m深随时间发展的融区,土体吸热增大,放热减小;热融湖塘2.5~3.0 m土体的年内热交换为19592.0 k J/m2,约是天然地表的230倍,其中吸热量及放热量分别为后者的1.4倍及8.7%.湖塘下部的融化夹层是深层冻土的主要热源,湖塘对下部土体放热的抑制作用是湖塘对土体产生热影响的主要原因. 相似文献
725.
Structural architecture of Neoproterozoic rifting depression groups in the Tarim Basin and their formation dynamics 总被引:1,自引:0,他引:1
Bizhu HE Cunli JIAO Taizhu HUANG Xingui ZHOU Zhihui CAI Zicheng CAO Zhongzheng JIANG Junwen CUI Zhuoyin YU Weiwei CHEN Ruohan LIU Xiaorui YUN Guangming HAO 《中国科学:地球科学(英文版)》2019,(3):529-549
The Tarim Basin is the largest, oil-bearing, superimposed basin in the northwest of China. The evolution and tectonic properties of the initial Tarim Basin have been hotly disputed and remain enigmatic. The Neoproterozoic basin is covered by a vast desert and a huge-thickness of sedimentary strata, has experienced multiple tectonic movements, had a low signal to noise ratios(SNRs) of deep seismic reflection data, all of which have posed critical obstacles to research. We analysed four field outcrops, 18 wells distributed throughout the basin, 27 reprocessed seismic reflection profiles with higher SNRs across the basin and many ancillary local 2D and 3D profiles and aeromagnetic data. We found about 20 normal fault-controlled rifting depressions of the Cryogenian and Ediacaran scattered throughout the basin, which developed on the Precambrian metamorphic and crystalline basement. The structural framework is clearly different from that of the overlying Phanerozoic. The rifting depressions consist of mainly half grabens, symmetrical troughs and horst-grabens. From the northeast to southwest of the basin,they are divided into three rifting depression groups with the WNW, ENE, and NW-trends that are mainly controlled by normal faults. The maximum thicknesses of the strata are up to 4100 m. From the Cryogenian to Ediacaran, most of the main inherited faults to active and eventually ceased at the end of the Ediacaran or Early Cambrian, while subsidence centres appeared and migrated eastward along the faults. They revealed that the different parts of the Tarim continental block were in NNE-SSWoriented and NNW-SSE-oriented extensional paleo-stress fields(relative to the present) during the Neoproterozoic, and were accompanied by clockwise shearing. According to the analysis of the activities of syn-sedimentary faults, filling sediments,magmatic events, and coordination with aeromagnetic anomalies, the tectonic properties of the fault depressions are different and are primarily continental rifts or intra-continental fault-controlled basins. The rifting phases mainly occurred from 0.8–0.61 Ga.The formation of the rifting depression was associated with the initial opening of the South Altun-West Kunlun Ocean and the South Tianshan Ocean, which were located at the northern and southern margins of the Tarim Block, respectively, in response to the break-up of the Supercontinent Rodinia and the initial opening of the Proto-Tethys Ocean. 相似文献
726.
Little is known regarding characteristics and evolution of radiolarian fossils in the early Cambrian due to its rarity and poor preservation. Here we report a new radiolarian fauna from the Cambrian Shuijingtuo Formation corresponding to the Chiungchussuan Stage(Cambrian Series 2) in western Hubei, China. It contains over 300 radiolarian tests and these fossils belong to 4 morphotypes, including Paraantygopora porosa gen.et sp. nov., Braunosphaera sinensis gen.et sp. nov., Tetrasphaera? sp. and incertae spherical radiolarians. In taxonomy, Spumellaria predominates in the fauna and comprises 92% of the total. In shell structure, about 73% of all specimens are similar to the early Ordovician radiolarian fossils, with the shell walls characterized by perforated plate structures. The spherical radiolarians with latticed shells constitute another feature of the early Cambrian radiolarian fauna. The radiolarian fauna reported here contains many fossil specimens and covers different taxonomical taxa. These specimens usually consist of distinctive concentric multi-layers with complex structure. These characteristics indicate that Radiolaria had already thrived during the Cambrian Chiungchussuan Stage(Series 2, Stage 3), which may have occurred synchronously with the explosion and prosperity of macrobiota recorded in the strata deposited in shallower water condition. 相似文献
727.
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729.
五里湖作为太湖富营养化最严重的区域,内源污染和生态退化成为困扰五里湖最主要的两个问题.生态清淤工程的特点是对所要疏浚污染底泥污泥厚度通过采样分析后精确测定,并且在施工过程中的控制精度也高于一般的工程疏浚.所以生态清淤既可以清除五里湖的内源污染,又能为其生态恢复创造条件.本文通过对五里湖生态疏浚对生态系统的影响,疏浚区底泥、水质质量的改善的效果以及对原位培养生物的抗氧化系统组分变化等多个方面进行分析评价,发现,五里湖生态疏浚区底泥中磷含量下降了30%,左右,重金属含量升高的地质积累指数小于1级.疏浚后半年内水体中总磷和溶解磷含量比疏浚前下降10%-25%左右,叶绿素a含量下降40%,左右,其它水质理化参数保持正常.作为生物标志物原位培养生物的抗氧化系统组分在疏浚前后变化较小所以认为,五里湖疏浚达到了一定的效果,并且控制了对生态的压力,为下一步生态修复创造了条件. 相似文献
730.