全文获取类型
收费全文 | 15711篇 |
免费 | 3130篇 |
国内免费 | 3874篇 |
专业分类
测绘学 | 1248篇 |
大气科学 | 3171篇 |
地球物理 | 4066篇 |
地质学 | 8021篇 |
海洋学 | 2013篇 |
天文学 | 763篇 |
综合类 | 1541篇 |
自然地理 | 1892篇 |
出版年
2024年 | 83篇 |
2023年 | 325篇 |
2022年 | 736篇 |
2021年 | 890篇 |
2020年 | 679篇 |
2019年 | 786篇 |
2018年 | 896篇 |
2017年 | 820篇 |
2016年 | 898篇 |
2015年 | 800篇 |
2014年 | 976篇 |
2013年 | 953篇 |
2012年 | 902篇 |
2011年 | 900篇 |
2010年 | 913篇 |
2009年 | 883篇 |
2008年 | 844篇 |
2007年 | 752篇 |
2006年 | 591篇 |
2005年 | 515篇 |
2004年 | 503篇 |
2003年 | 521篇 |
2002年 | 599篇 |
2001年 | 543篇 |
2000年 | 535篇 |
1999年 | 686篇 |
1998年 | 594篇 |
1997年 | 560篇 |
1996年 | 543篇 |
1995年 | 413篇 |
1994年 | 381篇 |
1993年 | 331篇 |
1992年 | 265篇 |
1991年 | 205篇 |
1990年 | 193篇 |
1989年 | 143篇 |
1988年 | 123篇 |
1987年 | 99篇 |
1986年 | 81篇 |
1985年 | 58篇 |
1984年 | 43篇 |
1983年 | 28篇 |
1982年 | 29篇 |
1981年 | 26篇 |
1980年 | 22篇 |
1979年 | 10篇 |
1977年 | 5篇 |
1976年 | 4篇 |
1962年 | 4篇 |
1958年 | 5篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
331.
Petrology, geochemistry and isotopic ages of eclogites from the Dulan UHPM Terrane, the North Qaidam, NW China 总被引:35,自引:0,他引:35
The Dulan eclogite–gneiss region is located in the eastern part of the North Qaidam eclogite belt, NW China. Widespread evidence demonstrates that this region is a typical ultrahigh-pressure (UHP) metamorphic terrane. Eclogites occur as lenses or layers in both granitic and pelitic gneisses. Two distinguished sub-belts can be recognized and differ in mineralogy, petrology and geochemistry. The North Dulan Belt (NDB) has tholeiitic protoliths with high TiO2 and lower Al2O3 and MgO contents. REE patterns and trace element contents resemble those of N-type and E-type MORB. In contrast, eclogites in the South Dulan Belt (SDB) are of island arc protoliths with low TiO2, high Al2O3 and show LREE-enriched and HFSE-depleted patterns. Sm–Nd isotope analyses give isochron ages of 458–497 Ma for eclogite-facies metamorphism for the two sub-belts. The ages are similar to those of Yuka and Altun eclogites in the western extension of the North Qaidam-Altun eclogite belt. The Dulan UHP metamorphic terrane, together with several other recently recognized eclogite-bearing terrenes within the North Qaidam-Altun HP-UHP belt, constitute the key to the understanding of the tectonic evolution of the northern Tibetan Plateau. The entire UHP belt extends for more than 1000 km from the Dulan UHP terrane in the southeast to the Altun eclogite–gneiss terrane in the west. This super-belt marks an early Paleozoic continental collision zone between the Qaidam Massif and the Qilian Massif. 相似文献
332.
Horie Kei Maki Norio Kohiyama Masayuki Lu Hengjian Tanaka Satoshi Hashitera Shin Shigekawa Kishie Hayashi Haruo 《Natural Hazards》2003,29(3):341-370
Rebuilding of victims' livelihoods was a crucial issue in the restoration process in the1995 Hanshin-Awaji Earthquake Disaster. Housing damage assessment influencedmost of the rebuilding of the livelihood in the long term, because the Victim Certificatesissued by the local governments based on the results of the Housing damage assessmentwas required to receive most of the individual assistance measures. In the process ofHousing damage assessment, many complex problems arose, leading to extensivework on the part of the disaster responders. Consequently, a considerable number ofvictims were dissatisfied with the assessment and applied for a resurvey. Due to a floodof requests for resurvey, disaster responders had to work on damage assessment, leavingrelief activities aside.In order to facilitate Housing damage assessment, this paper discusses thefollowing five points: (1) the processes and the problems of assessments performedin the Hanshin-Awaji Earthquake Disaster, (2) the changes in the nature of informationneeded by the victims, (3) the improvements over the present damage assessment, (4)the housing situation in Japan, and (5) the international situation on damage assessment.It is obvious from the results that a poor damage assessment system and the size ofthe disaster produced a very large work load. Differences in appreciation among theinvestigators also contributed to unfair assessments and led to the victims beingincreasingly dissatisfied by the survey results. Finally, a design concept for acomprehensive damage assessment system, which has been derived from theabove five points, is proposed for post-disaster management. 相似文献
333.
ZHANGJin MAZongjin RENWenjun LEIYongliang 《大地构造与成矿学(英文版)》2003,27(1):165-178
There are many thrust-related structures occurring in the Paleozoic strata of the Niushou Mountain in the central part of Ningxia Hui Autonomous Region. The fault-related folds are the typical structures in this area. Based on the analysis about these structures and their relationships, the processes by which these structures of the Miboshan Formation were formed are reconstructed, and the strata underwent about three stages of deformation: (1) horizontal shortening, (2) folding, and (3) thrusting. And the fact that the Niushou Mountain is the leading edge of an old thrust sheet was proved, the Niushou Mountain, the Daluo Mountain and the Xiaoluo Mountain together constitute the front part of this old thrust zone, so the Niushou Mountain and the Ordovician strata in the central and southern parts of Ningxia now are likely allochthons. In the period from middle Ordovician to Devonian, the areas of the central and southern Ningxia belonged to the back-arc foreland basin of North Qilianshan orogen, which was adjacent to the continent in the north. In the later part of the early Paleozoic period, the Niushou Mountain was formed after the closure of the back-arc foreland basin. 相似文献
334.
Cretaceous deformation history of the middle Tan-Lu fault zone in Shandong Province, eastern China 总被引:13,自引:0,他引:13
Based on field analysis of fault-slip data from different rock units of the Cretaceous basins along the middle part of the Tan-Lu fault zone (Shandong Province, eastern China), we document polyphase tectonic stress fields and address the changes in sense of motion of the Tan-Lu fault zone during the Cretaceous. The Cretaceous deformation history of the Tan-Lu fault zone can be divided into four main stages. The first stage, during the earliest Cretaceous, was dominated by N-S extension responsible for the formation of the Jiaolai basin. We interpret this extension to be related to dextral strike-slip pull-apart opening guided by the Tan-Lu fault zone. The second stage, during the middle Early Cretaceous, was overwhelmingly rift-dominated and characterized by widespread silicic to intermediate volcanism, normal faulting and basin subsidence. It was at this stage that the Tan-Lu-parallel Yi-Shu Rift was initiated by E-W to WNW-ESE extension. The tectonic regime then changed during the late Early Cretaceous to NW-SE-oriented transpression, causing inversion of the Early Cretaceous rift basin and sinistral slip along the Tan-Lu fault zone. During the Late Cretaceous, dextral activation of the Tan-Lu fault zone resulted in pull-apart opening of the Zhucheng basin, which was subsequently deformed by NE-SW compression. This deformation chronology of the Tan-Lu fault zone and the associated Cretaceous basins allow us to constrain the regional kinematic models as related to subduction along the eastern margin of Asia, or related to collision in the Tibet region. 相似文献
335.
ZhangBingshan TangLiangjie JinZhijun DaiJunsheng ZhangMingli ZhangBingshan 《中国地质大学学报(英文版)》2003,14(1):65-72
The purpose of this paper is to analyze the regional fault systems of Qaidam basin and ad-jacent orogenic belts. Field investigation and seismic interpretation indicate that five regional fault sys-tans occurred in the Qaidam and adjacent nment.qin belts, controlling the development and evolution of the Qaidam basin. These fault systems are: (1)north Qaidam-Qilian Mountain fault system; (2) south Qaidam-East Kunhm Mountain fault system;(3)Altun strike-slip fault system; (4) Elashan strike-slip fault system, and (5) Gansen-Xiaochaidan fault system. It is indicated that the fault systems controlled the orientation of the Qaidam basin, the formation and distribution of secondary faults within the basin,the migration of depocenters and the distribution of hydrocarbon accmnulation belt. 相似文献
336.
337.
338.
利用1960~2000年青岛、射阳、徐州3站08时探空资料及日照站08时地面气象资料,分析了日照地区出现的16次降雹天气的时空分布特征,在对降雹天气分型的基础上利用积云数值模式计算降雹因子,用降雹因子和单站要素因子建立历史降雹因子个例库,用历史实况资料建立实况个例库,用距离相似法实现日照地区短时冰雹定时、定点、定量的客观预报。 相似文献
339.
340.
1994年1月至2000年12月北京地区若干社区脑卒中发病人数与同期气象资料分析结果表明:北京地区脑卒中发病有明显的季节性,冬春季高发,夏秋季低发;出血性脑卒中发病是春秋季高发,夏季低发;缺血性脑卒中发病是夏季高,秋季低。脑卒中发病与气温、气压和相对湿度有密切关系;寒冷与高温,气温、气压的剧烈变化等,可能是诱发脑卒中的重要气象因素。 相似文献