全文获取类型
收费全文 | 304篇 |
免费 | 68篇 |
国内免费 | 33篇 |
专业分类
测绘学 | 15篇 |
大气科学 | 41篇 |
地球物理 | 141篇 |
地质学 | 138篇 |
海洋学 | 25篇 |
天文学 | 12篇 |
综合类 | 19篇 |
自然地理 | 14篇 |
出版年
2023年 | 4篇 |
2022年 | 1篇 |
2021年 | 6篇 |
2020年 | 12篇 |
2019年 | 14篇 |
2018年 | 6篇 |
2017年 | 18篇 |
2016年 | 11篇 |
2015年 | 12篇 |
2014年 | 16篇 |
2013年 | 21篇 |
2012年 | 14篇 |
2011年 | 25篇 |
2010年 | 21篇 |
2009年 | 28篇 |
2008年 | 24篇 |
2007年 | 24篇 |
2006年 | 18篇 |
2005年 | 14篇 |
2004年 | 11篇 |
2003年 | 10篇 |
2002年 | 12篇 |
2001年 | 8篇 |
2000年 | 6篇 |
1999年 | 8篇 |
1998年 | 5篇 |
1997年 | 4篇 |
1996年 | 12篇 |
1995年 | 10篇 |
1994年 | 6篇 |
1993年 | 5篇 |
1992年 | 3篇 |
1991年 | 3篇 |
1990年 | 5篇 |
1989年 | 1篇 |
1988年 | 1篇 |
1986年 | 2篇 |
1985年 | 1篇 |
1984年 | 2篇 |
1982年 | 1篇 |
排序方式: 共有405条查询结果,搜索用时 31 毫秒
31.
提出了一种基于正交投影的波束形成算法.首先由MVDR算法确定初始权向量;其次根据该权向量与其它用户波达角方向的关系,建立干扰信号的导向矢量矩阵;然后通过正交投影原理,将期望信号的导向矢量投影到干扰信号的零空间上,从而求得最优权值.仿真结果证明了该算法的有效性. 相似文献
32.
Tsunami is one of a few kinds of natural disasters that leave people some time for escape. This escape time, which is essentially the time for the giant wave to propagate from the epicentre to a coast, has to be estimated without delay upon the occurrence of the incident. With the advancement of water wave theories, much work has been done to model the propagation of tsunamis from deep oceans to shallow water. The authors argue that while much emphasis has been put on the expansion of the high-tech early warning system and the development of complicated tsunami models, a simple-to-use yet accurate predictive model is still wanting. This paper presents a handy linear wave model, which is capable of estimating the arrival time of a tsunami with very good accuracy, as has been verified by comparison with past incidents. With the availability of such a simple model, even local communities without access to a high-tech warning system can readily estimate the time left for emergency evacuation. 相似文献
33.
The dynamics of a pair of satellites similar to Enceladus–Dione is investigated with a two-degrees-of-freedom model written
in the domain of the planar general three-body problem. Using surfaces of section and spectral analysis methods, we study
the phase space of the system in terms of several parameters, including the most recent data. A detailed study of the main
possible regimes of motion is presented, and in particular we show that, besides the two separated resonances, the phase space
is replete of secondary resonances. 相似文献
34.
35.
会泽超大型富锗铅锌矿、澜沧老厂大—超大型银铅多金属矿床和保山金厂河航磁异常深部找矿,先后取得重大突破,推动云南新一轮新、老矿山和磁异常区深部找矿积极性。建议禄丰中兴井125#—元谋甘泉村航磁异常、巧家药山航磁异常与石屏龙潭含多金属铁帽等的深部找矿应及早提上议事日程。 相似文献
36.
2010年7·27四川汉源二蛮山滑坡-碎屑流特征与成因机理研究 总被引:6,自引:0,他引:6
2010年7月27日凌晨4时许,四川省汉源县万工乡二蛮山发生大规模滑坡,约48×104m3的强风化玄武岩体,在前期降雨的影响下高位高速滑出,随即解体转化为碎屑流,沿沟谷高速运动,沿途不断携卷和铲刮堆积于沟床及两侧斜坡的表层松散物质,使滑体的体积和含水量不断增大。当运动到沟谷中段时,因沟道在此向右偏转,在强大的惯性力作用下,部分碎屑流体冲向左岸斜坡,将居住于此的双合村一组5户村民房屋掩埋,造成20人失踪;另一部分碎屑流体继续沿沟谷高速运动近1.4km才最终停止。约30m in后,堆积于沟谷中段深切沟道内的滑坡堆积物,在重力作用下再次启动,形成二次滑坡。二次滑坡缓慢蠕滑流动数小时,最终到达万工新集镇,将部分房屋推倒掩埋,造成92户房屋受损、1500人被迫紧急转移。本文在对灾害现场进行详细地质调查的基础上,结合现场测绘、颗分试验、航拍等手段,对二蛮山滑坡体的基本特征进行了较深入的调查研究,对滑坡发生及成灾原因进行了初步分析。结果表明,滑源区相对突出的地形条件、风化破碎的玄武岩体和有利的结构面组合是滑坡发生的基本条件;前期降雨期间爆发的泥石流对滑源区坡脚的掏蚀、强降雨的饱水加载作用以及雨水沿陡倾张裂结构面的下渗软化作用,是诱发滑坡发生的直接原因。二蛮山沟谷原为一高频泥石流沟,滑坡发生前并无明显的滑坡迹象,滑坡的发生表现出极强的隐蔽性和突发性以及高位高速远程运动和危害巨大的特点,同时,主滑坡发生后在短时间内滑坡区再次启动发生二次滑坡,这些现象和特点具有特殊性,也具有典型性,值得深入研究。 相似文献
37.
Kevin R. Chamberlain Axel K. Schmitt Susan M. Swapp T. Mark Harrison Norbert Swoboda-Colberg Wouter Bleeker Tony D. Peterson Charles W. Jefferson Andrei K. Khudoley 《Precambrian Research》2010
An in situ U–Pb SIMS (IN-SIMS) method to date micro-baddeleyite crystals as small as 3 μm is presented with results from three samples that span a variety of ages and geologic settings. The method complements ID-TIMS geochronology by extending the range of dateable crystals to sizes smaller than can be recovered by physical separation. X-ray mapping and BSE imaging are used to locate target grains in thin section, followed by SIMS analysis on a CAMECA ims 1270, using the field aperture in the transfer column to screen out ions from host phases. Internal age precisions for the method are anticipated to range from 0.1% for Precambrian rocks to 3–7% for Phanerozoic rocks. Results establish a 2689 ± 5 Ma age for mafic dikes in the Wyoming craton, USA, a 1540 ± 30 Ma age for a subaerial lava flow from the Thelon Basin of northern Canada, and a 457 ± 34 Ma age for mafic dikes in the platform sequence of southeastern Siberia. The method is ideal for relatively non-destructive dating of small samples such as extraterrestrial rocks and precious terrestrial samples. 相似文献
38.
海拉尔盆地贝尔凹陷白垩系南屯组和铜体庙组凝灰质砂岩、凝灰质泥岩、沉凝灰岩和凝灰岩储层是该区主要产层。油气储集空间以次生孔隙为主。大量碱性矿物组合如柯绿泥石、钠板石、碳钠铝石、方沸石、绿磷石、铈褐帘石、铁绿泥石等的存在,证明发生了大规模碱性溶解和交代作用。晶屑、玻屑、长石和粘土等填隙物均发生不同程度的溶解现象。研究表明,次生孔隙是凝灰质储层大规模碱交代作用的结果,预示盆地深部存在油气储集空间并富集油气。 相似文献
39.
尽管塔里木盆地石炭系富含有机质且已发现其生成的原油,但关于石炭系烃源岩热演化研究却很薄弱。根据基础地质资料、古地温梯度和实测镜质体反射率数据,本文定量模拟了塔里木盆地6口典型井的石炭系烃源岩热演化史和这套烃源岩底界、顶界在二叠纪末期、三叠纪末期、白垩纪末期及现今成熟度的平面分布规律。塔北隆起南部、塔西南坳陷和阿瓦提凹陷在石炭-二叠纪作为沉降中心接受了巨厚的沉积物,造成这些地区石炭系烃源岩底界成熟度在二叠纪末期达到0.9%~1.3%(中-高成熟),顶界为0.5%~0.9%(低-中成熟),成为有利生油区。中生代时期,塔里木盆地中、东部长期处于沉降状态,石炭系烃源岩处于成熟演化阶段。白垩纪末期,塔中低凸起和满加尔凹陷的石炭系底界成熟度为0.7%~0.9%(中成熟),顶界为0.5%~0.7%(低成熟),而塘古孜巴斯坳陷底界成熟度为0.9%~1.1%(中-高成熟),顶界为0.7%~0.9%(中成熟)。受羌塘地体、拉萨地体、印度板块分别与欧亚板块南缘碰撞远程效应的影响,塔西南坳陷和巴楚隆起在中生代一直处于隆升剥蚀状态,烃源岩热演化进入停滞状态。新生代以来,塔西南坳陷和阿瓦提凹陷演化为前陆盆地,再次接受了巨厚沉积物,致使石炭系烃源岩快速成熟演化,底-顶界成熟度现今已超过2.0%,进入干气阶段。满加尔凹陷石炭系烃源岩自石炭纪至今一直处于成熟演化阶段,现今达到最大,为0.8%~1.0%。另外,热史研究表明塔西南坳陷和阿瓦提凹陷石炭系烃源岩具有二次生烃潜力。本研究不仅丰富了塔里木盆地石炭系烃源岩热史研究成果,而且对油气勘探与开发具有重要的指导意义。 相似文献
40.
Guangyou Zhu Shuichang Zhang Barry Jay Katz Jin Su Xue Wang Zihui Feng Jie Cui Xingwang Liu 《Chemie der Erde / Geochemistry》2014
The Western Slope of the Songliao Basin is rich in heavy oil resources (>70 × 108 bbl), around which there are shallow gas reservoirs (∼1.0 × 1012 m3). The gas is dominated by methane with a dryness over 0.99, and the non-hydrocarbon component being overwelmingly nitrogen. Carbon isotope composition of methane and its homologs is depleted in 13C, with δ13C1 values being in the range of −55‰ to −75‰, δ13C2 being in the range of −40‰ to −53‰ and δ13C3 being in the range of −30‰ to −42‰, respectively. These values differ significantly from those solution gases source in the Daqing oilfield. This study concludes that heavy oils along the Western Slope were derived from mature source rocks in the Qijia-Gulong Depression, that were biodegraded. The low reservoir temperature (30–50 °C) and low salinity of formation water with neutral to alkaline pH (NaHCO3) appeared ideal for microbial activity and thus biodegradation. Natural gas along the Western Slope appears mainly to have originated from biodegradation and the formation of heavy oil. This origin is suggested by the heavy δ13C of CO2 (−18.78‰ to 0.95‰) which suggests that the methane was produced via fermentation as the terminal decomposition stage of the oil. 相似文献