全文获取类型
收费全文 | 1270篇 |
免费 | 250篇 |
国内免费 | 607篇 |
专业分类
测绘学 | 6篇 |
大气科学 | 11篇 |
地球物理 | 140篇 |
地质学 | 1739篇 |
海洋学 | 22篇 |
天文学 | 96篇 |
综合类 | 89篇 |
自然地理 | 24篇 |
出版年
2024年 | 6篇 |
2023年 | 25篇 |
2022年 | 30篇 |
2021年 | 49篇 |
2020年 | 44篇 |
2019年 | 62篇 |
2018年 | 59篇 |
2017年 | 71篇 |
2016年 | 75篇 |
2015年 | 60篇 |
2014年 | 89篇 |
2013年 | 124篇 |
2012年 | 101篇 |
2011年 | 83篇 |
2010年 | 54篇 |
2009年 | 98篇 |
2008年 | 78篇 |
2007年 | 86篇 |
2006年 | 99篇 |
2005年 | 75篇 |
2004年 | 68篇 |
2003年 | 76篇 |
2002年 | 71篇 |
2001年 | 51篇 |
2000年 | 53篇 |
1999年 | 53篇 |
1998年 | 42篇 |
1997年 | 57篇 |
1996年 | 47篇 |
1995年 | 46篇 |
1994年 | 35篇 |
1993年 | 39篇 |
1992年 | 30篇 |
1991年 | 18篇 |
1990年 | 18篇 |
1989年 | 14篇 |
1988年 | 13篇 |
1987年 | 8篇 |
1986年 | 1篇 |
1985年 | 4篇 |
1984年 | 7篇 |
1983年 | 1篇 |
1982年 | 3篇 |
1981年 | 1篇 |
1975年 | 2篇 |
1973年 | 1篇 |
排序方式: 共有2127条查询结果,搜索用时 15 毫秒
941.
The history of glacial advances and retreats of the East Antarctic ice sheet during the Holocene is not well-known, due to limited field evidence in both the marine and terrestrial realm. A 257-cm-long sediment core was recovered from a marine inlet in the Rauer Group, East Antarctica, 1.8 km in front of the present ice-sheet margin. Radiocarbon dating and lithological characteristics reveal that the core comprises a complete marine record since 4500 yr. A significant ice-sheet expansion beyond present ice margins therefore did not occur during this period. 相似文献
942.
The purpose of this study is to investigate the enrichment level and dispersion patterns of Se and associated elements in rocks, soils and crops which were collected in the Dukpyung and the Chubu areas covered with black shales of the Okchon Group in Korea. Rock and soil samples were analyzed for Se including multiple elements by ICP, ICP-MS and INAA, and crop samples by INAA. Soil pH and loss-on-ignition (LOI) were also measured. 相似文献
943.
江西庐山地区位于江南造山带的东段北侧,出露前震旦纪星子群和双桥群变质岩,最近在双桥山群地层中发现了一套枕状构造发育的细碧岩-角斑岩组合。通过对细碧岩-角斑岩组合和与其紧密共生的英安岩的元素地球化学研究发现该组合具有洋岛型玄武岩的特点,形成环境为陆壳基础上的弧后小洋盆;英安岩中SHRIMP锆石U-Pb测年得到表面年龄介于830~850Ma,其206Pb-238U加权平均年龄为(840±7)Ma。因此,皖南(歙县)缝合带有可能呈近东西向一直延伸到赣北的庐山地区,而江南造山带至少在830~850Ma期间仍未关闭;同时也证明双桥山群是中、下扬子地块"一盖多底"中基底的一部分。 相似文献
944.
宁夏香山群徐家圈组发现深水复合流沉积构造 总被引:8,自引:1,他引:7
宁夏香山群徐家圈组是由灰绿、黄绿色轻微变质中—细粒砂岩、钙质砂岩及粉砂岩和页岩(板岩)组成的深水沉积。在上部灰绿色页岩所夹的中层钙质粉砂岩中发现了复合流层理、准平行层理、不对称小型丘状交错层理;在下部灰绿色厚层—块状中—细粒长石石英砂岩的顶面发现了小型波痕,波痕的形态、波长与波高的分布规律均表现出复合流(combined-flow)的沉积特征。本文根据水槽实验和现代海洋沉积观测所总结出的复合流底床相图和前人在研究地层中较浅海浊流(超重流)与波浪所形成的复合流沉积时给出的复合流沉积示意图,分别对徐家圈组所发现的①小型2D波痕至小型3D波痕的演化和②复合流层理、平行层理、准平行层理和小型丘状交错层理的叠置关系及其纹层所反映的流动方向与沉积时浊流方向的关系,进行了解释。结果表明,所发现的复合流层理、准平行层理、不对称小型丘状交错层理及小型波痕应为复合流沉积,并依据徐家圈组存在内波、内潮汐沉积的事实,推测为深水短周期内波与浊流形成的复合流沉积。这可能是地层中深水复合流沉积构造的首次发现,同时也是内波与浊流形成的复合流沉积的首次发现。 相似文献
945.
西秦岭大草滩群的形成时代和构造意义探讨 总被引:2,自引:0,他引:2
大草滩群a岩组中最年轻的一组锆石206Pb/238U年龄加权平均值为404.9±4.8 Ma(MSWD=0.11),b岩组中最年轻的锆石206Pb/238U年龄值为385±5 Ma,c岩组样品中最年轻的锆石206Pb/238U年龄值为375±6 Ma,这一结果将大草滩群的最大沉积时代有效地限定在405~375 Ma之间。结合生物化石组合资料,大草滩群的时代归属于晚泥盆世。根据岩石组合、沉积相、构造变形、形成时代和物源分析等资料综合研究表明,晚泥盆世大草滩群河湖相粗粒碎屑岩形成时的大地构造背景是位于安第斯型活动大陆边缘的弧前拉张—裂陷盆地,作为北秦岭微陆(+岩浆弧)与华北大陆西南缘碰撞的沉积响应,是碰撞造山作用以后南部洋壳持续俯冲阶段同火山—岩浆活动的弧前沉积体系。 相似文献
946.
Stratigraphy and sedimentology of the Upper Cretaceous to Paleogene Kilwa Group, southern coastal Tanzania 总被引:2,自引:0,他引:2
Christopher J. Nicholas Paul N. Pearson Paul R. Bown Tom Dunkley Jones Brian T. Huber Amina Karega Jackie A. Lees Ian K. McMillan Aoife OHalloran Joyce M. Singano Bridget S. Wade 《Journal of African Earth Sciences》2006,45(4-5):431-466
The geology of southern coastal Tanzania has remained poorly understood since the first comments on its stratigraphy were made over 100 years ago. However, new field surveys combined with shallow drilling along the coast between Kilwa and Lindi are beginning to resolve the depositional history and structural evolution of this region over the past 85 Ma. Here we present the first attempt to synthesize the results of these studies to provide a coherent sedimentological, litho- and sequence stratigraphic framework, including new geological maps, for the Upper Cretaceous and Paleogene of the coastal zone.Santonian to Oligocene sediments crop out along a broad coastal belt south of the Rufiji River from the Kilwa peninsula to Lindi Creek in southern Tanzania. During 55 Ma, over 1 km of a broadly homogeneous, mid to outer shelf clay-dominated succession was deposited across the passive margin, which we define here as the Kilwa Group. This lies disconformably across the shelf on Albian marls and is itself unconformably overlain by shallow water Miocene clays and more recent limestones, sands and gravels. Four formations can be identified within the Kilwa Group on the basis of characteristic secondary lithologies and facies, described here for the first time; the Nangurukuru, Kivinje, Masoko and Pande Formations. These formations include conformable stratigraphic intervals through both the Paleocene–Eocene and Eocene–Oligocene boundaries. Within the Kilwa Group, 12 sequence stratigraphic cycles can be identified at present, demonstrating relatively uniform and continual subsidence across the margin from Santonian to Early Oligocene time. A further major bounding surface is present between the Upper Cretaceous and Paleogene, but this may become partly conformable in the Lindi area. Although the principal lithology in all formations is clay or claystone, there are more permeable intervals containing pervasive coarser siliciclastic sediments and these have yielded traces of crude oil which is likely to have migrated from lower in the succession. The Kilwa Group thus also provides important new evidence for petroleum play development in the southern coastal zone. 相似文献
947.
城市群体建筑物震害模拟方法研究 总被引:2,自引:0,他引:2
本文针对目前进行城市群体建筑物震害预测时,在数据收集和计算工作中遇到的实际困难,提出了一种简化的震害计算方法——单元破坏度指数法。同时将该计算模型嵌入到ArcView 9.0的GIS平台中,并以Oracle数据库为支撑,结合青岛市的实际数据,对城市群体建筑物的震害进行了模拟。结果表明,单元破坏度指数法不仅大大简化了数据收集和处理的工作量,而且计算结果的精度同样能满足工程应用的要求,与GIS相结合可以客观快速地模拟出城市群体建筑物的震害程度及其空间分布。 相似文献
948.
沱沱河盆地通天河剖面渐新世雅西措群发现一套产于湖泛过程中的柱状叠层石。通过对叠层石纹层形态和显微组构的研究,发现这些叠层石具有典型的富藻纹层和富屑纹层交替的显微结构特征,发育三级生长节律,纹层对之间渐变接触,纹层带之间间断明显。采用激光微区取样的方法,针对4块样品的8个纹层对,系统采集了16对碳氧同位素数据,结果是富藻纹层同位素值整体上均高于富屑纹层,正相关性明显。这表明富藻纹层生长时期气候炎热湿润,富屑纹层生长时期相对寒冷干燥。认为湖相叠层石生长受周期性气候变化的控制,其韵律纹层记录了丰富的古气候信息。 相似文献
949.
950.
L. Monaco M. Bellazzini F. R. Ferraro E. Pancino 《Monthly notices of the Royal Astronomical Society》2005,356(4):1396-1402
We present an analysis of the density profile in the central region of the Sagittarius dwarf spheroidal galaxy. A strong density enhancement of Sgr stars is observed. The position of the peak of the detected cusp is indistinguishable from the centre of M54. The photometric properties of the cusp are fully compatible with those observed in the nuclei of dwarf elliptical galaxies, indicating that the Sgr dSph would appear as a nucleated galaxy independently of the presence of M54 at its centre. 相似文献