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881.
882.
Liangyuan Feng Ruoling Li Yawen Zhang Yixian Wang Zhixin Qian Zhenghua Zhao 《中国地球化学学报》1983,2(2):153-169
Rare-earth elements in samples of geological interest were separated from other elements and concentrated onto ion-exchange membrane through ion-exchange procedures. The membrane was then used to determine the REE by X-ray fluorescence spectrography. In comparison with the traditional “thick-specimen” approach, the requirement of sample (REE oxides) in this method was reduced from 10 to 1 mg. Variable-internal-standard-quantification method was adopted to determine the relative concentrations of REE collected on the membrane. The area density of the sample was controlled at about 0.0003 g/cm2, so that the matrix effect could be eliminated to a satisfactory extent. Interference calibration between the spectro-lines and the background determination was also improved, with the detection limit reaching 2.5×10?6g. 相似文献
883.
诸暨璜山金矿是除治岭头以外浙江省第二金矿,它的找矿模式为"三高两低一复合"的找矿模式,即高金晕、高极化率、高磁场跳跃、低电阻率、低电位和北东断裂与北东东断裂复合处是成矿最有利部位.在其附近仍有类似成矿部位,有望扩大远景. 相似文献
884.
王赫 《中国气象科学研究院年报》2005,(1):45-46
中国气象科学研究院博士后科研工作站2003年1月正式挂牌并开始招收博士后研究人员,2005年4月被批准为正式招收博士后研究人员单位。2005年,我院首批招收的博士后研究人员已有4人按规定完成了在站期间的各项科研任务,并做出了创新性成果,顺利出站。2005年底在站博士后研究人员11人。我院招收的博士后研究人员,总体素质较高。2005年有2名博士后研究人员分别获得了国家自然科学基金青年基金项目和国家自然科学基金面上项目。 相似文献
885.
油气储运系统钢结构设备地震火灾效应研究 总被引:3,自引:0,他引:3
预防和减轻油气储运系统地震火灾危险性是防震减灾中的重要课题。本文论述了油气储运系统的地震火灾特征及防火要求,对钢结构的防火涂料在遭到破坏和平时情况下的抗火性能进行了对比分析,并应用有限元法对油气储运系统中典型钢结构设备在地震火灾荷载作用下的抗火性能进行了数值模拟。研究结果表明,防火涂料遭到强地震荷载破坏后,钢结构的抗火性能大大降低。 相似文献
886.
我国非点源污染研究进展与发展趋势 总被引:14,自引:0,他引:14
非点源污染是我国重要的污染源。本文简要介绍了非点源污染模型,我国非点源污染的研究现状,分析了我国非点源污染研究存在的问题及未来研究发展趋势。 相似文献
887.
888.
Wang Xiuxi Li Jijun Song Chunhui Zhang Jun Zhao Zhijun Gao Junping Pan Meihui 《Frontiers of Earth Science》2007,1(3):304-308
The Cenozoic sedimentation in the Tianshui basin, which is located at the junction of the liupanshan and West Qinling, northeast
margin of the Tibetan plateau, provides a record for the regional tectonism and exhumation history of the surrounding mountains.
Thermochronologic study on the detrital apatite grains from sandstones at Yaodian, near Tianshui, has revealed two rapid tectonic
uplift-exhumation events of the source area, which happened at 23.7 and 14.1 Ma, respectively. The fast exhumation (0.34 mm/a)
at 23.7 Ma, which recorded the tectonic uplift of West Qinling, led to the formation of the Neogene Tianshui basin and initiated
the reception of alluvial deposits. This event is most likely in response to the synchronous tectonism of the Tibetan plateau.
The source region experienced another rapid exhumation (1.05 mm/a) at 14.1 Ma, when the Tianshui basin began to depress broadly
and fluvial-lacustrine sediments dominated the Late Miocene.
Translated from Acta Sedimentologica Sinica, 2006, 24(6): 783–789 [译自: 沉积学报] 相似文献
889.
The No. 6 Coal-bed from the Heidaigou Mine, Jungar Coalfield, Inner Mongolia is a super-large Ga deposit. The dominant carrier of Ga is boehmite in coal. The study of coal facies may provide genetic enrichment information of Ga and its carrier (boehmite) in the Ga deposit. On the basis of study on coal petrology and mineralogy, it was found that the No. 6 Coal-bed from the Heidaigou Mine of Jungar was enriched in inertinites and the microlitho-types were dominated by clarodurite. The maceral morphological features and association indicate that the coal-bed was formed in a dry sedimentary environment or in a periodic dry sedimentary environment caused by the alternating variations of groundwater level. The optimum conditions for the enrichment of Ga and its particular carrier (boehmite) were dominated by four transitional conditions: (1) the upper delta plain which was the transitional zone between alluvial and lower delta plains, (2) the transitional zone between the dry and wet forest swamps, being slightly apt to the dry one, (3) the transitional tree density between the thick and loose ones, and (4) the low moor that was the transitional zone between two high moors during peat accumulation. 相似文献
890.