全文获取类型
收费全文 | 2415篇 |
免费 | 493篇 |
国内免费 | 574篇 |
专业分类
测绘学 | 208篇 |
大气科学 | 418篇 |
地球物理 | 447篇 |
地质学 | 1437篇 |
海洋学 | 325篇 |
天文学 | 117篇 |
综合类 | 194篇 |
自然地理 | 336篇 |
出版年
2024年 | 5篇 |
2023年 | 30篇 |
2022年 | 85篇 |
2021年 | 90篇 |
2020年 | 79篇 |
2019年 | 86篇 |
2018年 | 121篇 |
2017年 | 101篇 |
2016年 | 86篇 |
2015年 | 101篇 |
2014年 | 94篇 |
2013年 | 130篇 |
2012年 | 120篇 |
2011年 | 142篇 |
2010年 | 178篇 |
2009年 | 152篇 |
2008年 | 133篇 |
2007年 | 129篇 |
2006年 | 126篇 |
2005年 | 91篇 |
2004年 | 107篇 |
2003年 | 101篇 |
2002年 | 141篇 |
2001年 | 128篇 |
2000年 | 115篇 |
1999年 | 123篇 |
1998年 | 103篇 |
1997年 | 83篇 |
1996年 | 96篇 |
1995年 | 84篇 |
1994年 | 71篇 |
1993年 | 53篇 |
1992年 | 46篇 |
1991年 | 32篇 |
1990年 | 35篇 |
1989年 | 19篇 |
1988年 | 13篇 |
1987年 | 7篇 |
1986年 | 9篇 |
1985年 | 9篇 |
1984年 | 7篇 |
1983年 | 7篇 |
1982年 | 7篇 |
1981年 | 1篇 |
1980年 | 2篇 |
1979年 | 1篇 |
1977年 | 2篇 |
1958年 | 1篇 |
排序方式: 共有3482条查询结果,搜索用时 281 毫秒
181.
综合物探方法在松辽盆地北部基底结构研究中的应用 总被引:3,自引:0,他引:3
根据综合地球物理方法,查明松辽盆地北部基底的断裂26条,其中岩石圈断裂6条,壳断裂5条,基底断裂15条;盆地基底岩性由五种类型所组成一前寒武系变质岩、糜棱岩、下古生界变质岩、二叠系浅变质岩及花岗岩。为盆地演化及含油气性提供重要信息。 相似文献
182.
This paper discusses the Cretaceous-Tertiary magnetic polarity sequence of the the Hengyang Basin on the basis of magnetostratigraphic study. The age of each stratigraphic unit has been determined with the magnetic polarity time scale combined with 39Ar/40Ar dating, thus providing evidence for determining the geological ages of different formations. The authors assign the age of the Dongjing Formation of the Hengyang Basin to Early Cretaceous, the Shenhuangshan Formation to Early-Late Cretaceous, the Daijiaping Formation to Late Cretaceous, and the Dongtang and Xialiushi formations to Palaeocene. 相似文献
183.
关于生命起源研究的问题及其主攻方向的探讨 总被引:1,自引:0,他引:1
本文综述和分析了近几十年来国内外关于生命起源的研究的问题及各种假说和见解,提出物质的起源是生命起源问题研究的核心,生命起源问题应是研究原始地球的非生命物质如何演变成为生命物质的,地球上分子手性的起源是生命起源问题研究的主攻方向,有机分子光学活性百发生在由化学进化转入生物进化这一过渡阶段。 相似文献
184.
185.
地壳与上地幔是人类居住与获取各种资源、能源,改造和利用自然的重要场所,是地球科学的基础与生长点,六十年代以来发展迅猛。中国大陆、海域和过渡带地区的地壳和上地幔物理探索,在全球板块构造和驱动机制的研究具有特殊地位,文中分别就1)青藏高原地区的地壳结构,2)青海、甘肃地区地壳结构和地壳中的高速块层,3)中原地区的地壳与上地幔结构,4)京津及外围地区的地壳结构,5)隋县—南京—启东和隋县—安阳人工地震探测面的观测,6)利用面波和远震P波确定中国地壳和上地幔结构,7)中国地壳结构的基本轮廓等方面进行了讨论。 相似文献
186.
Starting November 1999 we are carrying out simultaneous seeing observations with the Solar Differential Image Motion Monitor (S-DIMM) at the Fuxian Lake station of the Yunnan Observatory and a solar scintillometer of the type used in the recent site survey by one of us (Beckers et al., 1997). The purpose was to compare the two methods of assessing the daytime atmospheric seeing for a lake site. We report here the first results of this comparison. We find that the relation between the seeing as measured by the S-DIMM (the Fried parameter r
0) and the scintillation in the solar irradiance (I) differs greatly from the relation found by Seykora (1993) for NSO/Sac Peak. We conclude that the I measurements give a good indication for the amount of near-Earth seeing but that they are a poor proxy for the total atmospheric seeing. We interpret the simultaneous (r
0, I) observations in terms of an atmospheric seeing model and find good quantitative agreement with a model in which a fraction () of the seeing originated near the Earth (ground or water) and the rest (1–) originates at higher layers. For lake sites is small all day and the seeing is determined primarily by the refractive index variations at higher atmospheric layers. For land sites is small in the early morning but rapidly increases as the day progresses, near-Earth seeing dominating there most of the time. 相似文献
187.
Inference of mantle viscosity from GRACE and relative sea level data 总被引:12,自引:0,他引:12
Gravity Recovery And Climate Experiment (GRACE) satellite observations of secular changes in gravity near Hudson Bay, and geological measurements of relative sea level (RSL) changes over the last 10 000 yr in the same region, are used in a Monte Carlo inversion to infer-mantle viscosity structure. The GRACE secular change in gravity shows a significant positive anomaly over a broad region (>3000 km) near Hudson Bay with a maximum of ∼2.5 μGal yr−1 slightly west of Hudson Bay. The pattern of this anomaly is remarkably consistent with that predicted for postglacial rebound using the ICE-5G deglaciation history, strongly suggesting a postglacial rebound origin for the gravity change. We find that the GRACE and RSL data are insensitive to mantle viscosity below 1800 km depth, a conclusion similar to that from previous studies that used only RSL data. For a mantle with homogeneous viscosity, the GRACE and RSL data require a viscosity between 1.4 × 1021 and 2.3 × 1021 Pa s. An inversion for two mantle viscosity layers separated at a depth of 670 km, shows an ensemble of viscosity structures compatible with the data. While the lowest misfit occurs for upper- and lower-mantle viscosities of 5.3 × 1020 and 2.3 × 1021 Pa s, respectively, a weaker upper mantle may be compensated by a stronger lower mantle, such that there exist other models that also provide a reasonable fit to the data. We find that the GRACE and RSL data used in this study cannot resolve more than two layers in the upper 1800 km of the mantle. 相似文献
188.
189.
LD2000 System with 3S and Multi—sensor 总被引:2,自引:0,他引:2
This paper introduces a car-borne road information collecting and updating system (LD2000) developed by Wuhan Technical University of Surveying and Mapping.This system is capable of collecting road network information and creating digital road network effectively by means of GPS,GIS and multi-sensor integration.The design and development of LD 2000 system are also presented in this paper. 相似文献
190.
××地块水泥土室内配合比试验 总被引:1,自引:0,他引:1
针对目前国内外水泥土强度测定的试验方法,还未形成规范操作的情况下,该文主要从室内试验的角度,阐述了水 泥土试验的目的、试验设备、试样的制备以及试验的方法,从而确定出最佳的水泥掺入比,同时对水泥土与原状土的 物理力学性质以及水泥土的强度增长机理作初步的探讨。 相似文献