全文获取类型
收费全文 | 5564篇 |
免费 | 1107篇 |
国内免费 | 1535篇 |
专业分类
测绘学 | 307篇 |
大气科学 | 1225篇 |
地球物理 | 1649篇 |
地质学 | 2829篇 |
海洋学 | 702篇 |
天文学 | 438篇 |
综合类 | 471篇 |
自然地理 | 585篇 |
出版年
2024年 | 23篇 |
2023年 | 104篇 |
2022年 | 240篇 |
2021年 | 277篇 |
2020年 | 237篇 |
2019年 | 253篇 |
2018年 | 275篇 |
2017年 | 271篇 |
2016年 | 291篇 |
2015年 | 300篇 |
2014年 | 302篇 |
2013年 | 320篇 |
2012年 | 299篇 |
2011年 | 333篇 |
2010年 | 280篇 |
2009年 | 318篇 |
2008年 | 286篇 |
2007年 | 253篇 |
2006年 | 240篇 |
2005年 | 226篇 |
2004年 | 190篇 |
2003年 | 212篇 |
2002年 | 203篇 |
2001年 | 237篇 |
2000年 | 216篇 |
1999年 | 277篇 |
1998年 | 206篇 |
1997年 | 254篇 |
1996年 | 201篇 |
1995年 | 148篇 |
1994年 | 177篇 |
1993年 | 133篇 |
1992年 | 101篇 |
1991年 | 61篇 |
1990年 | 72篇 |
1989年 | 50篇 |
1988年 | 60篇 |
1987年 | 44篇 |
1986年 | 32篇 |
1985年 | 21篇 |
1984年 | 23篇 |
1983年 | 17篇 |
1982年 | 23篇 |
1981年 | 14篇 |
1980年 | 10篇 |
1979年 | 13篇 |
1977年 | 7篇 |
1975年 | 8篇 |
1973年 | 6篇 |
1958年 | 9篇 |
排序方式: 共有8206条查询结果,搜索用时 218 毫秒
221.
222.
预测和控制深基坑变形的抗隆起稳定系数法 总被引:1,自引:0,他引:1
本文讨论了在软土基坑工程设计施工中所涉及到的抗隆起稳定系数的合理计算方法;通过对大量上海深基坑工程的计算分析并结合现场实测数据论证了利用抗隆起稳定系数进行基坑变形预测和控制的合理性,并提出了适用稳定系数法控制基坑变形的设计计算预测公式:δh/H~Ks关系式。 相似文献
223.
南秦岭十里坪锑矿床成矿时代及成因的初步研究 总被引:1,自引:1,他引:1
十里坪锑矿床受赵川陆缘隆_滑构造的主滑脱拆离带的控制。矿体呈脉状赋存于韧_脆性主滑脱带上部的脆性次级断层_节理中,矿石类型主要为萤石石英辉锑矿型。围岩为太古宙_元古宙变质岩系,围岩蚀变弱。成矿流体属H2O_CO2_NaCl体系,流体包裹体盐度w(NaCleq)为3.6%~11.3%,均一温度为109~232℃,形成压力大致为800×105Pa。硫、铅同位素研究表明,矿质主要来源于变火山岩围岩;氢、氧同位素显示,成矿流体以大气降水为主,初步将该矿床定为变质岩源就地式大气降水热液矿床。矿石中萤石Sm_Nd等时线年龄为(392±24)Ma,与南秦岭北部晚古生代拗陷区热水喷流_沉积成矿时代相一致,它们都形成于秦岭微板块泥盆纪非造山裂解阶段。 相似文献
224.
A rainfall-induced shallow landslide is a major hazard in mountainous terrain, but a time-space based approach is still an unsettled issue for mapping rainfall-induced shallow landslide hazards. Rain induces a rise of the groundwater level and an increase in pore water pressure that results in slope failures. In this study, an integrated infinite slope analysis model has been developed to evaluate the influence of infiltration on surficial stability of slopes by the limit equilibrium method. Based on this new integrated infinite slope analysis model, a time-space based approach has been implemented to map the distributed landslide hazard in a GIS (Geographic Information Systems) and to evaluate the shallow slope failure induced by a particular rainfall event that accounts for the rainfall intensity and duration. The case study results in a comprehensive time-space landslide hazard map that illustrates the change of the safety factor and the depth of the wetting front over time. 相似文献
225.
Methane-rich fluid inclusions in skarn near the giant REE–Nb–Fe deposit at Bayan Obo, Northern China
We report fluid inclusion data for skarn, formed at the contact between Hercynian granitoids and dolomite of the Proterozoic Bayan Obo Group, in the vicinity of Bayan Obo REE–Nb–Fe deposit, Inner Mongolia, China. Three types of fluid inclusions are identified: two-phase CH4-rich, three-phase liquid–vapour–solid and two-phase aqueous inclusions. Using microthermometry and laser Raman microprobe analysis to calculate isochores for CH4-bearing inclusions, we estimate fluid trapping conditions at T=280 to 344 °C and P<1 to 2.3 kbar. Such conditions are compatible with formation of CH4 inclusions as a result of reaction between graphite in the country rocks (black slate sequence) and fluids derived from magma. The lack of carbonaceous material in the inclusions supports the hypothesis that CH4 was generated during fluid migration rather than by in situ reaction. In contrast to the skarn, and despite the fact that similar graphite-bearing slates are found in the host rocks, no CH4-bearing inclusions have been so far reported from Bayan Obo REE ores. We therefore conclude that the skarn-forming fluids in the contact aureole of the Hercynian granitoids were not involved at any stage in the formation of the Bayan Obo deposit. 相似文献
226.
Continental crustal growth and the supercontinental cycle: evidence from the Central Asian Orogenic Belt 总被引:15,自引:0,他引:15
Dawei Hong Jisheng Zhang Tao Wang Shiguang Wang Xilin Xie 《Journal of Asian Earth Sciences》2004,23(5):799
Studies of supercontinental cycle are mainly concentrated on the assembly, breakup and dispersal of supercontinents, and studies of continental crustal growth largely on the growth and loss (recycling) of the crust. These two problems have long been studied separately from each other. The Paleozoic–Mesozoic granites in the Central Asian Orogenic Belt have commonly positive Nd values, implying large-scale continental crustal growth in the Phanerozoic. They coincided temporally and spatially with the Phanerozoic Pangea supercontinental cycle, and overlapped in space with the P-wave high-V anomalies and calculated positions of subducted slabs for the last 180 Ma, all this suggests that the Phanerozoic Laurasia supercontinental assembly was accompanied by large-scale continental crustal growth in central Asia. Based on these observations, this paper proposes that there may be close and original correlations between a supercontinental cycle, continental crustal growth and catastrophic slab avalanches in the mantle. In this model we suggest that rapid continental crustal growth occurred during supercontinent assembly, whereas during supercontinental breakup and dispersal new additions of the crust were balanced by losses, resulting in a steady state system. Supercontinental cycle and continental crustal growth are both governed by changing patterns of mantle convection. 相似文献
227.
228.
流动VLBI天线系统噪声温度及天线效率测量 总被引:1,自引:0,他引:1
我国自行研制的第一套流动VLBI系统——DCW—01型流动VLBI测量仪,目前已在国家重大科学工程“中国地壳运动观测网络”中投入使用。在流动VLBI的观测试验中,天线系统噪声温度和天线效率是观测前系统调试和检测的两项重要内容。天线系统噪声温度是衡量流动VLBI观测系统内部噪声程度的特性指标;天线效率反映了天线系统对到达天线能量的刊用率,在很多计算公式中是一个很重要的参数。因此,精确地测量它们的值是进行相关处理和计算的前提。文中结合我国流动VLBI观测站的研制与建设,介绍了流动VLBI测量仪的天线及接收机系统,并详细阐述了其天线系统噪声温度和天线效率的测量。 相似文献
229.
岩石水压致裂和诱发地震的实验研究 总被引:5,自引:0,他引:5
用7种岩石各制备了几类不同预裂纹的系列试件,并在不同围压下进行水压致裂强度实验。结合典型的水库诱发地震的实际资料和现今构造应力场的实验结果,以及应用岩石强度理论和岩石断裂力学的一些原理、方法,进行岩石孔隙水压诱发地震的探讨。初步结果为:(1)若岩体内构造应力很小,一定大小的孔隙水压力σp,可直接使岩体内的薄弱面致裂并发生小地震。(2)若构造应力较大,存在两类诱发地震的可能:①对岩体浅部一些走向与构造应力的主压应力σ1方向相近的薄弱面,σp可促使其发生张性破裂并诱发小地震。②当构造应力接近于断裂的抗剪强度时,因σp,降低了断裂面上的正应力σn,使原处于稳定状态的断裂失稳,发生滑移破裂并诱发出地震。σp导致断裂的破裂深度增大,使诱发地震的震级大于原潜在的地震震级。(3)各种岩体均存在着一个极限深度,此深度后不再有诱发地震。 相似文献
230.