全文获取类型
收费全文 | 14779篇 |
免费 | 2926篇 |
国内免费 | 3880篇 |
专业分类
测绘学 | 1376篇 |
大气科学 | 3047篇 |
地球物理 | 3754篇 |
地质学 | 7394篇 |
海洋学 | 1895篇 |
天文学 | 681篇 |
综合类 | 1517篇 |
自然地理 | 1921篇 |
出版年
2024年 | 84篇 |
2023年 | 222篇 |
2022年 | 686篇 |
2021年 | 790篇 |
2020年 | 679篇 |
2019年 | 868篇 |
2018年 | 874篇 |
2017年 | 799篇 |
2016年 | 889篇 |
2015年 | 875篇 |
2014年 | 959篇 |
2013年 | 1007篇 |
2012年 | 979篇 |
2011年 | 1028篇 |
2010年 | 977篇 |
2009年 | 970篇 |
2008年 | 906篇 |
2007年 | 921篇 |
2006年 | 740篇 |
2005年 | 603篇 |
2004年 | 488篇 |
2003年 | 458篇 |
2002年 | 474篇 |
2001年 | 461篇 |
2000年 | 464篇 |
1999年 | 490篇 |
1998年 | 398篇 |
1997年 | 396篇 |
1996年 | 321篇 |
1995年 | 278篇 |
1994年 | 321篇 |
1993年 | 241篇 |
1992年 | 190篇 |
1991年 | 141篇 |
1990年 | 110篇 |
1989年 | 82篇 |
1988年 | 104篇 |
1987年 | 53篇 |
1986年 | 47篇 |
1985年 | 40篇 |
1984年 | 36篇 |
1983年 | 32篇 |
1982年 | 38篇 |
1981年 | 27篇 |
1980年 | 8篇 |
1979年 | 11篇 |
1978年 | 5篇 |
1975年 | 2篇 |
1958年 | 7篇 |
1954年 | 4篇 |
排序方式: 共有10000条查询结果,搜索用时 242 毫秒
261.
Zhao Jinren Zhang Xiankang Zhang Chengke Ren Qingfang Cheng Shuangxi Zhang Jianshi Nie Wenying PAN Shuzhen 《中国地震研究》2003,17(2):103-112
The data from two deep seismic sounding profiles was processed and studied comprehensively. The results show that crnst-mantle structures in the investigated region obviously display layered characteristics and velocity structures and tectonic features have larger distinction in different geological structure blocks. The boundary interface C between the upper and lower crust and Moho fluctuate greatly. The shallowest depths of C (30.0km) and Moho (45.5km) under Jiashi deepen sharply from Jiashi to the western Kunlun mountain areas, where the depths of C and Moho are 44.0km and 70.0km, respectively. The higher velocity structures in the Tarim massif determine its relatively “stable“ characteristics in crust tectonics. The phenomenon in the Jiashi region, where the distribution of earthquake foci mostly range from 20kin to 40kin in depth, may infer that the local uplift of C and Moho interface, anomalonsly lower velocity bodies and deep large faults control earthquake occurrence and seismogenic processes in the Jiashi strong earthquake swarm. 相似文献
262.
263.
The relation between the gravity variation features and Ms=8.1 earthquake in Qinghai-Xizang monitoring area is analyzed preliminarily,by using spatial dynamic variation results of regional gravity field from absolute gravity and relative gravity observation in 1998 and 2000.The results show that:1)Ms\8.1 earthquake in Kulun mountain pass westem occurred in the gravity variation high gradient near gravity‘s high negative variation;2)The Main tectonic deformation and emnergy accumulation before MS=8.1 earthquake are distributed at south side of the epicenter;3)The range of gravity‘s high negative variation at east of the MS=8.1 earthquake epicenter relatively coincides with that rupture region according to field geology investigation;4)Gravity variation distribution in high negative value region is just consistent with the second shear strain‘s high value region of strain field obtained from GPS observation. 相似文献
264.
Absence of Archean basement in the South Kunlun Block: Nd-Sr-O isotopic evidence from granitoids 总被引:3,自引:0,他引:3
Abstract The West Kunlun mountain range along the northwestern margin of the Tibetan Plateau is crucial in understanding the early tectonic history of the region. It can be divided into the North and South Kunlun Blocks, of which the former is considered to be part of the Tarim Craton, whereas consensus was not reached on the nature and origin of the South Kunlun Block. Samples were collected from the 471 Ma Yirba Pluton, the 405 Ma North Kudi Pluton and the 214 Ma Arkarz Shan Intrusive Complex. These granitoids cover approximately 60% of the Kudi area in the South Kunlun Block. Sr, Nd, and O isotope compositions preclude significant involvement of mantle-derived magma in the genesis of these granitoids; therefore, they can be used to decipher the nature of lower–mid crust in the area. All samples give Mesoproterozoic Nd model ages (1.1–1.5 Ga) similar to those of the exposed metamorphic complex of this block but significantly different from those of the basement of the North Kunlun Block (2.8 Ga). This indicates that the South Kunlun Block does not have an Archean basement, and, thus, does not support the microcontinent model that suggests the South Kunlun Block was a microcontinent once separated from and later collided back with the North Kunlun Block. 相似文献
265.
0.7Ma以来的念青唐古拉山脉隆升过程——来自冰川剥蚀作用的证据 总被引:1,自引:0,他引:1
通过对念青唐古拉山冰碛地层划分及冰碛物同位素测年,发现最早一期冰碛物形成于0.7~0.6MaBP,指示自中更新世以来念青唐古拉山脉开始隆升,主峰地区发生了大规模的冰川剥蚀作用,形成了大面积分布的冰碛高平台;0.2~0.14MaBP念青唐古拉山又快速隆升,并堆积了刚刚伸出各大沟谷口的高侧碛;0.07~0.03MaBP念青唐古拉山再次小规模隆起,形成各大沟谷内的侧碛和终碛垄;0.01Ma BP还有小规模冰川活动。念青唐古拉山主峰地区的冰川剥蚀作用反映出的山脉隆升过程,可较好地与青藏高原的隆起过程相对比,它应是青藏高原隆升的响应。 相似文献
266.
267.
268.
GPS-OEM在精准农业领域中的应用实例 总被引:4,自引:0,他引:4
介绍了我中心开发的内置有GPS—OEM板的农田信息采集系统,指出了GPS—OEM在精准农业领域发展潜力。 相似文献
269.
无拓扑关系下GIS图形编辑联动的解决方法 总被引:2,自引:0,他引:2
给出了一种解决层内联动以及层间联动的方法,对于实际处理无拓扑关系下编辑联动的问题有较好的利用价值。 相似文献
270.
The West Kunlun orogenic belt is located at the conjunction of the paleo-Asian tectonic system and the Tethys tectonic system.
Petrological and mineralogical studies of the Early Cambrian metamorphic surface crust in this region have shown that in case
the metamorphism reached low-temperature granulate facies, the typical mineral assemblage is biotite-garnet-silimanite-K feldspar-plagioclase-quartz.
The peak metamorphic temperatures are within the range of 720–740°C and the pressure is 0.6 GPa ±. Three types of metamorphic
zircon have been detected in the metamorphic rocks: the complex inclusion-bearing type ; the early relic zircon inclusion-bearing
type; and the inclusion-free type. SHRIMP age determination of these three types of metamorphic zircon have revealed that
these zircons were formed principally during 400–460 Ma, indicating that pre-Cambrian metamorphic surface crust rocks underwent
low-temperature granulite facies metamorphism during the Caledonian. In combination with the geological characteristics of
this region, it is considered that when the oceanic basin was closed, there occurred intense intracontinental subduction (type
A), bringing part of the Early Cambrian metamorphic basement in this region downwards to the lower crust. Meanwhile, there
were accompanied with tectonic deformation at deep levels and medium- to high-grade metamorphism. This study provided important
chronological and mineralogical evidence for the exploration of the evolutionary mechanism and process of the West Kunlun
Early Paleozoic.
Part of the results from the research project “ Research on the West Kunlun pre-Cambrian tectonic events” under the program
“ Research on the important geological problems of China’ s pre-Cambrian” (No. 200113900070) sponsored by the China National
Geological Surveying Bureau. 相似文献