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101.
Tungsten(or wolfram,W),one of the crucial metal sources,is widely used in electronics,oil,chemical and military industries.China owns abundant tungsten resources(~60%of the world reserves and~80%of the world’s production),of which the area from Southern Jiangxi-Northern GuangdongSouthern Hunan is the most significant ore belt in south China.Understanding ore genesis and distribution as well as the process of fine mineralization will further benefit the prospecting and exploration of tungsten deposits.The accurate determination of the age of mineralization is at the front line in the study of ore deposit and the premise for solving and understanding the above problems. 相似文献
102.
LI Yonggang ZHAI Mingguo YANG Jinhui MIAO Laicheng & GUAN HongInstitute of Geology Geophysics Chinese Academy of Sciences Beijing China Correspondence should be addressed to Li Yonggang 《中国科学D辑(英文版)》2004,47(2):115-121
The Anjiayingzi gold deposit in Chifeng County, Inner Mongolia is located in the central part of the gold mineralization belt of the northern margin of the North China Craton (NCC), and is adjacent to the Paleozoic Inner Mongolia-Da Hinggan Mountains orogenic belt in the north. The Chifeng-Kaiyuan fault, which separates the NCC from this orogenic belt, is considered to be a regional ore-controlling structure. The Anjiayingzi gold deposit is a mediate-size quartz lode-gold deposit and is hosted by the Anjiayingzi quartz monzonite that was emplaced into the basement composed of early Precambrian gneisses. Rhyolitic and porphyritic dikes are generally associated with the gold mineralization. Zircon U-Pb analyses suggest that the Anjiayingzi granite was emplaced from 132 Ma to 138 Ma, while the rhyolitic dikes that occupy the same fracture system as the gold-bearing quartz veins and locally crosscut the gold lodes crystallized from 125 Ma to 127 Ma. These results constrain the mineralization age between 126 相似文献
103.
本文运用滤波和K-L变换对全波列声测井数据进行处理。滤波能去掉某些高、低频噪音;K-L变换,能削弱相干或不相干的噪音,分离或去掉各种波型,以加强S波信噪比。 相似文献
104.
105.
106.
Hui Xie Lusheng Zhu Qifeng Xu Jun Wang Wei Liu Jinhui Jiang Yan Meng 《Environmental Earth Sciences》2011,62(1):93-99
A 1,1,1-trichloro-2,2-bis(4-chlorophenyl)ethane (DDT)-degrading bacterium was isolated from soil samples that had been enriched
with DDT over a prolonged period of time; these samples were collected from the sewer sludge of a pesticide factory and from
DDT-contaminated fields. This consortium was acclimated by repeated passage through a mineral salt medium containing increasing
concentrations of DDT. We examined the effects of various factors such as the pH, temperature, concentration of DDT, and the
presence of an additional carbon source on the degradation rate of DDT. Based on the analysis of the phenotype, physiological
and biochemical characteristics, and 16S rDNA, the strain KK was identified to belong to the bacteria Alcaligenes. The results showed that at the end of 10 days, the rate of degradation of DDT by the strain KK was 66.5%. When the additional
carbon source concentration, pH, concentration of DDT, and cultivation temperature is 0.5%, 6, 10 mg l−1, and 30°C, respectively, the biodegradation rate peaks. The results also suggested that (1) bacterial growth increases positively
with an increase in the carbon source concentration; (2) the appropriate pH is between 8.0 and 10.0; and (3) the optimal temperature
and DDT concentration are 30°C and 10 mg l−1, respectively. 相似文献
107.
Liangyuan Zhao Chi Zhu Chuangxin Gao Jinhui Jiang Jiaoyan Yang Shao Yang 《Environmental Earth Sciences》2011,64(2):581-588
Capability of three species of aquatic macrophytes to remediate pentachlorophenol (PCP)-contaminated sediments starting with
initial concentration of 2,000 μg kg−1 dw (dry weight) was investigated. Negative effect of PCP on the plant growth, chlorophyll contents and root activities (p > 0.05) of the three species of aquatic macrophytes during remediation was not observed. PCP removal was significantly enhanced
in the phytoremediated sediments in comparison with the control sediments after 90 days treatment (p < 0.05), and the removal rates of PCP in the sediments planted with P. communis Trin, T. orientalis and S. validus Vahl were 90.35 ± 0.03, 99.23 ± 0.02 and 99.33 ± 0.01%, respectively, while the rate was 29.87 ± 0.05% in the control sediments.
Bioaccumulation by three macrophytes was confirmed; the maximum PCP contents in the roots of P. communis Trin, T. orientalis and S. validus Vahl were 419.50 ± 0.71, 1,833.33 ± 7.37 and 2,090.00 ± 2.65 μg kg−1 at the 30th day, respectively. In conclusion, P. communis Trin, T. orientalis and S. validus Vahl may act as promising tools for the PCP phytoremediation in aquatic environment, especially S. validus Vahl. 相似文献
108.
109.
针对国(境)外地震专报产出过程中遇到的信息搜索困难、内容不规范、难以满足时效性等问题,基于C#编程语言,设计开发了国(境)外地震专报背景信息交互式产出系统。该系统只需值班人员少许的参与,自动获取人口信息、海啸信息、震中附近一定范围内的历史地震目录,生成地震的人口伤亡信息,最终产出word格式的地震专报。 相似文献
110.
Qingdong Zeng Yongbin Wang Song Zhang Jianming Liu Kezhang Qin Jinhui Yang Weidong Sun Wenjun Qu 《Resource Geology》2013,63(1):99-109
Mesozoic ore deposits in Zhejiang Province, Southeast China, are divided into the northwestern and southeastern Zhejiang metallogenic belts along the Jiangshan–Shaoxing Fault. The metal ore deposits found in these belts are epithermal Au–Ag deposits, hydrothermal‐vein Ag–Pb–Zn deposits, porphyry–skarn Mo (Fe) deposits, and vein‐type Mo deposits. There is a close spatial–temporal relationship between the Mesozoic ore deposits and Mesozoic volcanic–intrusive complexes. Zircon U–Pb dating of the ore‐related intrusive rocks and molybdenite Re–Os dating from two typical deposits (Tongcun Mo deposit and Zhilingtou Au–Ag deposit) in the two metallogenic belts show the early and late Yanshanian ages for mineralization. SIMS U–Pb data of zircons from the Tongcun Mo deposit and Zhilingtou Au–Ag deposit indicate that the host granitoids crystallized at 169.7 ± 9.7 Ma (2σ) and 113.6 ± 1 Ma (2σ), respectively. Re–Os analysis of six molybdenite samples from the Tongcun Mo deposit yields an isochron age of 163.9 ± 1.9 Ma (2σ). Re–Os analyses of five molybdenite samples from the porphyry Mo orebodies of the Zhilingtou Au‐Ag deposit yield an isochron age of 110.1 ± 1.8 Ma (2σ). Our results suggest that the metal mineralization in the Zhejiang Province, southeast China formed during at least two stages, i.e., Middle Jurassic and Early Cretaceous, coeval with the granitic magmatism. 相似文献