全文获取类型
收费全文 | 2873篇 |
免费 | 522篇 |
国内免费 | 740篇 |
专业分类
测绘学 | 206篇 |
大气科学 | 504篇 |
地球物理 | 681篇 |
地质学 | 1615篇 |
海洋学 | 382篇 |
天文学 | 161篇 |
综合类 | 219篇 |
自然地理 | 367篇 |
出版年
2024年 | 17篇 |
2023年 | 52篇 |
2022年 | 156篇 |
2021年 | 149篇 |
2020年 | 140篇 |
2019年 | 201篇 |
2018年 | 169篇 |
2017年 | 155篇 |
2016年 | 155篇 |
2015年 | 157篇 |
2014年 | 165篇 |
2013年 | 236篇 |
2012年 | 192篇 |
2011年 | 174篇 |
2010年 | 161篇 |
2009年 | 168篇 |
2008年 | 134篇 |
2007年 | 141篇 |
2006年 | 124篇 |
2005年 | 88篇 |
2004年 | 66篇 |
2003年 | 69篇 |
2002年 | 82篇 |
2001年 | 86篇 |
2000年 | 90篇 |
1999年 | 103篇 |
1998年 | 102篇 |
1997年 | 82篇 |
1996年 | 83篇 |
1995年 | 68篇 |
1994年 | 55篇 |
1993年 | 56篇 |
1992年 | 56篇 |
1991年 | 36篇 |
1990年 | 36篇 |
1989年 | 26篇 |
1988年 | 19篇 |
1987年 | 14篇 |
1986年 | 11篇 |
1985年 | 7篇 |
1984年 | 9篇 |
1983年 | 13篇 |
1982年 | 4篇 |
1981年 | 5篇 |
1979年 | 4篇 |
1978年 | 4篇 |
1977年 | 8篇 |
1976年 | 2篇 |
1969年 | 1篇 |
1968年 | 1篇 |
排序方式: 共有4135条查询结果,搜索用时 187 毫秒
991.
Natural weak acidic groundwater occurs in the unconfined and confined aquifers consisting of Quaternary and Neogene unconsolidated sediments near Beihai in southern Guangxi, China. Under natural conditions the groundwater has low TDS(less than 200 mg L-1) and low concentrations of trace elements(less than 100 μg L-1) with a deceasing tend in contents of the Lanthanides(rare earth elements, less than 1 μg L-1) towards higher atomic number. The groundwater ranges in p H from 3.33 to 7.0 with an average value of 5.12(even lower than that of local rainwater, 5.88). p H values in the groundwater are a bit higher in rainy seasons than those in dry seasons and do not show significant increasing or decreasing trend with time. The average p H value in groundwater in the confined aquifers is even a bit lower than that in the unconfined aquifer. Comprehensive analyses of the groundwater environment suggest that H+ in the groundwater may be derived from dissociation of H2CO3, release of the absorbed H3O+ in clay layers and the acidity of rainwater. The H2CO3 in the groundwater may be formed by dissolution of CO2(g). Minerals in the unconsolidated sediment are predominated by quartz with small amount of clay minerals. The sediments undergoing a long-term weathering contain low levels of soluble constitutes. Lack of alkaline substances in the groundwater system is also helpful in the accumulation of acidity of the groundwater. 相似文献
992.
993.
Shirong Ye Dezhong Chen Yanyan Liu Peng Jiang Weiming Tang Pengfei Xia 《GPS Solutions》2015,19(4):545-557
994.
对13个大质量恒星形成区样本进行了SiO(2-1)、CH_3OH(2-1)和C~(34)S(2-1)热线的观测.在9个分子云核中,3条热线同时被探测到.这9个SiO探测中,有3个是新探测到的且它们强度都相对较弱.所有探测到的谱线都有较明显的线翼,这可能是外向流出现的证据.SiO谱线的线宽最宽,这也更进一步表明SiO辐射可能是来自高速的外向流,即更靠近外向流的激发源.估算了各分子谱线的旋转温度,柱密度和相对元素丰度.结果表明SiO和CH_3OH元素丰度之间有较好的相关性,相关系数R=0.77,但是SiO和C~(34)S元素丰度之间却没有任何相关性. 相似文献
995.
Lithosphere extension and upwelling of asthenosphere at post-collisional stage of an orogenic cycle generally induce diverse magmatism and/or associated high-temperature metamorphism. Nevertheless, the intimate coexistence of post-collisional magmatic activity and high-temperature metamorphism is rare.In this contribution, a lithological assemblage composing of diverse magmatic rocks deriving from distinct magma sources and coeval high-temperature metamorphism was identified in eastern Kunlun.Petrography, ages, mineral chemistry and whole-rock geochemistry demonstrated that those intimately coexistent diverse rocks were genetically related to post-collisional extension. The garnet-bearing mafic granulites in Jinshuikou area interior of the East Kunlun Orogenic Belt are mainly composed of garnet,orthopyroxene, and plagioclase, with peak metamorphic P–T conditions of ~ 701–756 ℃and 5.6–7.0 kbar,representing a granulite-facies metamorphism at 409.7 ± 1.7 Ma. The diverse contemporaneous magmatic rocks including hornblendites, gabbros and granites yield zircon U–Pb ages of 408.6 ± 2.5 Ma,413.4 ± 4.6 Ma, and 387–407 Ma, respectively. The hornblendites show N-MORB-like REE patterns with(La/Sm)Nvalues of 0.85–0.94. They have positive zircon εHf(t) values of 0.1–4.9 and whole-rock εNd(t) values of 3.9–4.7 but relatively high(87Sr/86Sr)ivalues of 0.7081 to 0.7088. These features demonstrate that the hornblendites derived from a depleted asthenospheric mantle source with minor continental crustal materials in source. As for the gabbros, they exhibit arc-like elemental signatures, low zircon εHf(t) values(-4.3 to 2.5) and variable whole-rock εNd(t) values(-4.9 to 1.2) as well as high(87Sr/86 Sr)ivalues(0.7068 to 0.7126), arguing for that they were originated from partial melting of heterogeneous lithospheric mantle anteriorly metasomatized by subducted-sediment released melts. Geochemistry of the granites defines their strongly peraluminous S-type signatures. Zircons from the granites yield a large range of εHf(t) values ranging from -30.8 to -5.1, while the whole-rock samples yield consistent(87Sr/86 Sr)ivalues(0.7301 to 0.7342) and negative εNd(t) values(-10.1 to -12.4). These features indicate that the S-type granites could be generated by reworking of an ancient crust. Taken together, the penecontemporaneous magmatism and metamorphic event, demonstrated the early-middle Devonian transition from crustal thickening to extensional collapse. The post-collisional mantle-derived magmas serve as an essential driving force for the high-temperature granulite-facies metamorphism and anataxis of the crust associated with formation of S-type granite. This study not only constructs a more detail Proto-Tethys evolution process of the eastern Kunlun, but also sheds new light on better understanding the intimate relationship between magmatism and metamorphism during post-collisional extensional collapse. 相似文献
996.
997.
998.
999.
东北地区“人口-经济-空间”城市化协调性研究 总被引:20,自引:6,他引:14
城市化是一个"人口-经济-空间"三维一体的过程,其内在协调与否是城市可持续发展的关键所在。为此,首先通过构建人口、经济、空间城市化内在表征指标,运用均方差赋权法,以东北地区(指的是东北三省)34个地级市为研究对象,来综合测度其人口、经济、空间城市化水平;其次运用协调度评价模型对其协调程度进行评价;并在此基础上进行分类。研究结果表明:①东北地区经济城市化主导人口、空间城市化,但整体水平不高,平均水平基本处于加速发展阶段(0.25~0.35);②人口、经济、空间城市化水平的空间分异明显,其中人口城市化整体呈现出由北往南递减的趋势,而经济城市化则成由南往北递减的趋势,两者"内在互补(互异)"趋势非常明显;③三者城市化协调度低,且区域差异明显,由南往北递减趋势非常明显;④依据彼此间协调度主宰程度,将其划分为综合协调导向型,人口-经济、人口-空间、经济-空间协调导向型4种类型。 相似文献
1000.
中国矿业城市空间形态特征及其空间分异 总被引:1,自引:0,他引:1
矿业城市是以矿产资源开采和初加工为主的资源型城市,伴随矿业城市发展的各个阶段,城市空间会呈现相应的演变过程和格局,城市经济的转型也必将带来城市空间结构的响应.矿业城市空间结构受自然资源和产业发展的影响明显,是基于自然资源与产业转型的空间可持续发展的典型研究对象之一.选取中国33个公认的典型地级矿业城市作为研究样本,提取空间结构数据进行紧凑度和分形维数的计算与统计分析,力图总结我国矿业城市对比其他类型城市在空间形态上的基本特征和空间分异规律.结果表明,矿业城市空间形态的紧凑度较低,发展呈分散态;矿业城市空间的边界比较复杂,呈不规则状态;矿业城市紧凑度与边界维数呈负相关;矿业城市空间形态受城市发展阶段、有无依托、其他组织的人为规划等因素影响,呈现一定的空间分异规律;矿业城市空间形态与人口规模和经济发展水平存在相关. 相似文献