全文获取类型
收费全文 | 464篇 |
免费 | 81篇 |
国内免费 | 169篇 |
专业分类
测绘学 | 5篇 |
大气科学 | 1篇 |
地球物理 | 59篇 |
地质学 | 563篇 |
海洋学 | 29篇 |
天文学 | 1篇 |
综合类 | 22篇 |
自然地理 | 34篇 |
出版年
2023年 | 2篇 |
2022年 | 8篇 |
2021年 | 14篇 |
2020年 | 22篇 |
2019年 | 27篇 |
2018年 | 16篇 |
2017年 | 27篇 |
2016年 | 38篇 |
2015年 | 20篇 |
2014年 | 33篇 |
2013年 | 36篇 |
2012年 | 22篇 |
2011年 | 39篇 |
2010年 | 27篇 |
2009年 | 42篇 |
2008年 | 32篇 |
2007年 | 21篇 |
2006年 | 34篇 |
2005年 | 22篇 |
2004年 | 20篇 |
2003年 | 15篇 |
2002年 | 18篇 |
2001年 | 18篇 |
2000年 | 22篇 |
1999年 | 19篇 |
1998年 | 14篇 |
1997年 | 12篇 |
1996年 | 14篇 |
1995年 | 12篇 |
1994年 | 13篇 |
1993年 | 12篇 |
1992年 | 12篇 |
1991年 | 8篇 |
1990年 | 6篇 |
1989年 | 7篇 |
1988年 | 1篇 |
1987年 | 1篇 |
1986年 | 4篇 |
1985年 | 2篇 |
1984年 | 1篇 |
1981年 | 1篇 |
排序方式: 共有714条查询结果,搜索用时 15 毫秒
101.
大兴安岭成矿带北段区域地球化学背景与成矿带划分 总被引:1,自引:0,他引:1
大兴安岭成矿带是中国最重要的有色金属成矿带之一,资源潜力巨大,其北段是中国除新疆以外唯一存在地质空白的地区,矿产勘查与研究程度低。笔者通过对其区域地球化学场特征、大中型内生金属矿床分布规律、区域控矿地质条件的研究,初步认为本区优势内生金属矿产是钼矿、银铅锌矿,其次是金矿和铜矿,潜力矿种是铀矿;以德尔布干、鄂伦春-伊尔施两条深断裂为界,其两侧地球化学背景、成矿环境、矿种及成矿类型差异很大,并将大兴安岭成矿带北段划分为:德尔布干Ⅲ1、大兴安岭西坡Ⅲ2、嫩江Ⅲ3等3个Ⅲ级成矿亚带10个Ⅳ级成矿区。 相似文献
102.
During the last decades, several integrated studies of Tethyan Jurassic/Cretaceous boundary
sections from different countries were published with the objective to indicate problems for the selection
of biological, chemical or physical markers suitable for identification of the Jurassic/Cretaceous
boundary e the only system boundary within the Phanerozoic still not fixed by GSSP. Drawing the
boundary between the Jurassic and Cretaceous systems is a matter of global scale discussions. The
problem of proposing possible J/K boundary stratotypes results from lack of a global index fossils,
global sea level drop, paleogeographic changes causing development of isolated facies areas, as well
as from the effect of Late Cimmerian Orogeny. This contribution summarizes and comments data on
J/K boundary interval obtained from several important Tethyan sections and shows still existing problems
and discrepancies in its determination. 相似文献
103.
104.
白龙江中上游地区金矿控矿因素及成矿模式探讨 总被引:2,自引:1,他引:2
白龙江中上游地区微细浸染型金矿,是受地层和构造双重控制的金矿床。在阐述矿床空间分布规律、控矿因素、区域矿化和地球化学特征等基础上,初步建立了地质地球化学成矿模式。 相似文献
105.
凉城地区1∶5万水系沉积物地球化学测量中,发现并圈定了43个以Au、Ag、Pb、Cu、Zn等为特征组合元素的综合异常,优选5处找矿远景区,经过异常查证和地质评价,优选找矿靶区,发现多处银、金、铅多金属矿(化)点及有进一步工作价值的矿产地,其中有3处被列为内蒙古地质勘查基金项目,获得了较好的找矿效果。 相似文献
106.
天水地区第三系地层属于西秦岭甘肃群,梁家山隧道洞身穿越天水盆地第三系泥岩,为确定隧道围岩的地质特性,进行了泥岩样品的地球化学成分与矿物成分测试。将梁家山隧道泥岩的测试结果与天水秦安县下山剖面泥岩的结果进行对比分析和相关分析。结果表明:二者之间存在较好的相关性,能够描述梁家山隧道泥岩的地层岩性、区域地质背景及其演化等工程地质特性,为进一步研究天水盆地的物质组成、风化特征、沉积环境和构造背景提供依据。同时也为利用隧道工程修建研究相关地学问题提供范例和基础数据。 相似文献
107.
108.
James U.L. Baldini Frank McDermott Dirk L. Hoffmann David A. Richards Nicholas Clipson 《Earth and Planetary Science Letters》2008,272(1-2):118-129
Cave air PCO2 at two Irish sites varied dramatically on daily to seasonal timescales, potentially affecting the timing of calcite deposition and consequently climate proxy records derived from stalagmites collected at the same sites. Temperature-dependent biochemical processes in the soil control CO2 production, resulting in high summer PCO2 values and low winter values at both sites. Large Large-amplitude, high-frequency variations superimposed on this seasonal cycle reflect cave air circulation. Here we model stalagmite growth rates, which are controlled partly by CO2 degassing rates from drip water, by considering both the seasonal and high-frequency cave air PCO2 variations. Modeled hourly growth rates for stalagmite CC-Bil from Crag Cave in SW Ireland reach maxima in late December (0.063 μm h− 1) and minima in late June/early July (0.033 μm h− 1). For well-mixed ‘diffuse flow’ cave drips such as those that feed CC-Bil, high summer cave air PCO2 depresses summer calcite deposition, while low winter PCO2 promotes degassing and enhances deposition rates. In stalagmites fed by well-mixed drips lacking seasonal variations in δ18O, integrated annual stalagmite calcite δ18O is unaffected; however, seasonality in cave air PCO2 may influence non-conservative geochemical climate proxies (e.g., δ13C, Sr/Ca). Stalagmites fed by ‘seasonal’ drips whose hydrochemical properties vary in response to seasonality may have higher growth rates in summer because soil air PCO2 may increase relative to cave air PCO2 due to higher soil temperatures. This in turn may bias stalagmite calcite δ18O records towards isotopically heavier summer drip water δ18O values, resulting in elevated calcite δ18O values compared to the ‘equilibrium’ values predicted by calcite–water isotope fractionation equations. Interpretations of stalagmite-based paleoclimate proxies should therefore consider the consequences of cave air PCO2 variability and the resulting intra-annual variability in calcite deposition rates. 相似文献
109.
By implementing the moisture-based form of Richards’ equation into the geochemical modelling framework PHREEQC, a generic tool for the simulation of one-dimensional flow and solute transport in the vadose zone undergoing complex geochemical reactions was developed. A second-order, cell-centred, explicit finite difference scheme was employed for the numerical solution of the partial differential equations of flow and transport. In this scheme, the charge-balanced soil solution is treated as an assembly of elements, where changes in water and solute contents result from fluxes of elements across cell boundaries. Therefore, water flow is considered in terms of oxygen and hydrogen transport. 相似文献
110.
Geochemical changes across the Ordovician-Silurian transition on the Yangtze Platform,South China 总被引:1,自引:0,他引:1
The trace element and rare earth element (REE) variations across the Ordovician-Silurian succession are presented from two
outcrop sections on the Yangtze Platform: the Nanbazi section, Guizhou Province, deposited in a shallow platform interior
setting, and the Wangjiawan section, Hubei Province, deposited in a deeper basinal environment. Geochemical analysis of closely
spaced samples through three intervals, the Wufeng, Guanyinqiao and Longmaxi, revealed vast palaeoceanographic changes. Some
geochemical proxies, including Th/U, Ni/Co, V/Cr, and V/(V+Ni) ratios, together with sedimentary facies and biotic data, indicate
that an anoxic condition on the most of the Yangtze Platform during the Wufeng and Longmaxi intervals, but an oxic condition
during the Guanyinqiao time. The shift of the anoxic to the oxic environment during the Guanyinqiao time coincided with a
global sea-level lowstand, in parallel with the global glaciation. The Longmaxian anoxic environment was a result of a global
sea-level rise, which may be synchronized with a mainly catastrophic event in the latest Ordovician. Although the two sections
generally show similar variation patterns of trace and REE concentrations and some element ratios, a minor difference occurs
between the Wangjiawan and Nanbazi sections, likely reflecting a difference in depositional setting during the accumulation.
Such an oceanic oxygen-level variation may add a useful constraint to the current arguments on the cause and consequence of
the latest Ordovician mass extinction.
Supported by National Basic Research Program of China (Grant No. 2005CB422101) 相似文献