全文获取类型
收费全文 | 1775篇 |
免费 | 379篇 |
国内免费 | 137篇 |
专业分类
测绘学 | 95篇 |
大气科学 | 40篇 |
地球物理 | 39篇 |
地质学 | 344篇 |
海洋学 | 47篇 |
天文学 | 1657篇 |
综合类 | 28篇 |
自然地理 | 41篇 |
出版年
2024年 | 32篇 |
2023年 | 71篇 |
2022年 | 74篇 |
2021年 | 118篇 |
2020年 | 93篇 |
2019年 | 90篇 |
2018年 | 20篇 |
2017年 | 11篇 |
2016年 | 9篇 |
2015年 | 68篇 |
2014年 | 68篇 |
2013年 | 54篇 |
2012年 | 94篇 |
2011年 | 211篇 |
2010年 | 149篇 |
2009年 | 150篇 |
2008年 | 109篇 |
2007年 | 123篇 |
2006年 | 80篇 |
2005年 | 68篇 |
2004年 | 47篇 |
2003年 | 48篇 |
2002年 | 50篇 |
2001年 | 30篇 |
2000年 | 34篇 |
1999年 | 44篇 |
1998年 | 46篇 |
1997年 | 51篇 |
1996年 | 29篇 |
1995年 | 43篇 |
1994年 | 33篇 |
1993年 | 26篇 |
1992年 | 25篇 |
1991年 | 26篇 |
1990年 | 31篇 |
1989年 | 18篇 |
1988年 | 7篇 |
1987年 | 5篇 |
1986年 | 6篇 |
排序方式: 共有2291条查询结果,搜索用时 0 毫秒
871.
《水文地质工程地质》2010,(3):121-121
<正>从3月下旬开始,国土资源部分别从13个省(区)和中国地质调查局所属单位调集技术人员1100多人,钻机230台(套),物探设备18台(套),组成6个应急找水小分队、18个应急找水小组,230个钻井分队分赴西南抗旱一线找水打井。截至5月5日,已成 相似文献
872.
Abstract: The Lower Cambrian Nagaur Sandstone (Marwar Supergroup) has yielded trace fossils Treptichnus, Cruziana, serially repeated Rusophycus, Diplichnites, Monomorphichnus, Bergaueria, arthropod swimming traces and leap frogging marks of Cruziana ichnofacies. This ichnofossils assemblage is dominantly preserved in fine to medium grained red sandstone beds of the Mohra Member (Nagaur Sandstone). The presence of graded rip-up clasts, current ripples, dune cross-stratification with mud drapes and tidal bundles indicates a subtidal paleoenvironment for the deposition of Nagaur Sandstone Formation, which is corroborated by the Cruziana ichnofacies trace fossil assemblage. 相似文献
873.
874.
875.
876.
<正>从5月1日开始,全国地质灾害气象预警预报信息以国土资源部和中国气象局名义通过中央电视台、国土资源部门户网、中国地质环境信息网等途径向社会公众发布的同时,还将通过《中国国土资源报手机报》向全国国土资源管理部门的有关领导手机及时报道。 相似文献
877.
在提取东昆仑东段都兰地区11个1:2.5万地球化学测量项目16种共同测试元素原始数据的基础上,进行了数理指标及多元统计分析,以期从整体角度为该区寻找原生矿床及后期研究提供表生地球化学依据。分析显示:Au元素以强丰度背景拟合值、高剔除比率、高离散分布特征、强叠加值为特征,为区内主要的成矿元素,其次As、Sb、Cu、Ni、Cr、Co、Ag、Pb、Zn等元素丰度背景拟合值与剔除比率高,高强数据多,可作为第二类成矿元素;高温热液元素为背景的稀有稀土元素组合,浓集系数、丰度背景拟合值均表现为富集曲线,但变异系数与叠加作用较弱,可作为第三类成矿元素。通过多元统计分析,将全区元素划分为Ag-Zn-Pb、Cr-Co-Ni-Cu、Y-La-Sn、As-Mo-Sb、Au、W-Bi等六类,并且由各元素的因子得分极值绘制了地球化学分区图,从表生地球化学角度阐明了有利的成矿区段。 相似文献
878.
基于断层面强度的非均匀性,将断层面的宏观破裂过程看作是断面局部微元的破裂累积过程,假设断层局部微元强度遵循Weibull概率分布,从统计力学角度推导出了宏观的断层载荷.变形的全过程本构关系.采用一维地震力学模型,以远场位移a为控制变量,用稳定性理论研究了地震不稳定性问题.研究表明,系统刚度比(围岩刚度与断层刚度之比)β是影响地震发生的重要参数,只有当β<1时才会出现地震失稳,且应力突跳发生在平衡路径曲线的位移转向点,并给出了地震过程的3个重要参数(地震后断层半错距、地震应力降和释放的弹性能)的表达式.当β≥1时,不会发生地震,仅是缓慢的断层滑动,属于无震滑动. 相似文献
879.
Abstract: We present results tending to characterize the new records of invertebrates from the Yacoraite Formation (Maastrichtian-Danian). The fossils reported come from two stratigraphic sections exposed in the surroundings of Maimará and Jueya, province of Jujuy, northwestern Argentina. The selection was based on geological and paleontological evidence. The recovered fossils include gastropods and invertebrate fossil traces, including Planolites, Skolithos and Gastrochanoelites ichnogenus. As result of our review, we discussed the possibility of assigning the analyzed gastropods to the family Zygopleuridae (gene. et. sp. indet.), as an approximation to the taxonomic resolution of this fossil fauna. The trace fossils were assigned to the archetypical Glossifungites ichnofacies. The study of the fossil assemblage allowed us to define a shallow depositional environment, characteristic of a marine context with high-energy conditions. 相似文献
880.
Abstract: In the present study, the major and trace element compositions, as well as Sr, Nd isotopic compositions and K-Ar age data in mafic dikes from Hainan Island, China, have been analyzed. Whole-rock K-Ar dating yielded a magmatic duration of 61–98 Ma for mafic dikes. Mafic dikes have a very high concentration of incompatible elements, for example, Ba, Rb, Sr, K, rare earth elements, and especially light rare earth elements (LREE), and negative anomalies of Nb, Ta, and Ti in the normalized trace element patterns. The initial 87Sr/86Sr ratios and εSr(t) of the mafic dikes are 0.70634–0.71193 and +27.7 to +112.2, respectively. In the 87Sr/86Sr versus εNd(t) diagram, the Hainan Island mafic dikes plot between fields for depleted mantle and enriched mantle type 2. All these characteristics show that the mantle (source region) of mafic dikes in this area experienced metasomatism by fluids relatively enriched in LREE and large ion lithophile elements. The genesis of Hainan Island mafic dikes is explained as a result of the mixing of asthenospheric mantle with lithospheric mantle that experienced metasomatism by the subduction of the Pacific Plate. This is different from the Hainan Island Cenozoic basalts mainly derived from depleted asthenospheric mantle, and possibly, minor metasomatised lithospheric mantle. This study suggests that the Mesozoic and Cenozoic lithospheric revolutions in Hainan Island can be divided into three stages: (1) the compression orogenesis stage before 98 Ma. The dominant factor during this stage is the subduction of the ancient Pacific Plate beneath this area. The lithospheric mantle changed into enriched mantle type 2 by metasomatism; (2) the thinning and extension stage during 61–98 Ma. The dominant factor during this stage is that the asthenospheric mantle invaded and corroded the lithospheric mantle; and (3) the large-scale thinning and extension stage after 61 Ma. The large-scale asthenospheric upwelling results in the strong erupting of Cenozoic basalts, large-scale thinning of the lithosphere, the southward translating and counterclockwise rotating of Hainan Island, and the opening of the South China Sea. 相似文献