全文获取类型
收费全文 | 196篇 |
免费 | 40篇 |
国内免费 | 44篇 |
专业分类
测绘学 | 4篇 |
地球物理 | 85篇 |
地质学 | 166篇 |
海洋学 | 9篇 |
综合类 | 3篇 |
自然地理 | 13篇 |
出版年
2023年 | 1篇 |
2022年 | 3篇 |
2021年 | 2篇 |
2020年 | 5篇 |
2019年 | 7篇 |
2018年 | 5篇 |
2017年 | 10篇 |
2016年 | 5篇 |
2015年 | 12篇 |
2014年 | 9篇 |
2013年 | 17篇 |
2012年 | 17篇 |
2011年 | 18篇 |
2010年 | 12篇 |
2009年 | 18篇 |
2008年 | 15篇 |
2007年 | 14篇 |
2006年 | 13篇 |
2005年 | 13篇 |
2004年 | 4篇 |
2003年 | 19篇 |
2002年 | 11篇 |
2001年 | 9篇 |
2000年 | 2篇 |
1999年 | 1篇 |
1998年 | 8篇 |
1997年 | 8篇 |
1996年 | 1篇 |
1995年 | 4篇 |
1994年 | 2篇 |
1993年 | 3篇 |
1991年 | 1篇 |
1989年 | 5篇 |
1988年 | 2篇 |
1987年 | 1篇 |
1983年 | 1篇 |
1981年 | 1篇 |
1978年 | 1篇 |
排序方式: 共有280条查询结果,搜索用时 15 毫秒
271.
272.
曾德威 《成都信息工程学院学报》1993,(1)
本文结合平面边界元法和平面多极子展开法,求解平面分层埋入体的电磁散射。这种方法具有高速、占用内存少的优点。 相似文献
273.
Laurent Désindes Laurent Bailly Jacques Leroy Marc Lespinasse 《Comptes Rendus Geoscience》2005,337(9):832-840
The comparative study of two French high-purity silica placers of European class suitable for the electrometallurgy of silicon and ferrosilicon, located at Boudeau and Thédirac, in the Dordogne and Lot departments respectively, indicates strong similarities as regards the sources and the transportation of quartz, as well as a same process of undercover karstification as a determining factor in the formation of the deposits. The main difference lies in the number of the stages necessary to the formation of the trap. This comparative study allows the constitution of dynamic models for the genesis of these economic quartz concentrations. To cite this article: L. Désindes et al., C. R. Geoscience 337 (2005). 相似文献
274.
详细的钻井地质学、地球物理和地球化学研究表明,塔河油田南部奥陶系内部和顶部发育多幕次的加里东期岩溶作用,主要表现在奥陶系内部牙形石带缺失、钻井放空和泥浆漏失、地震剖面上奥陶统反射波组底部上超和顶部削截,以及溶洞充填方解石的Sr同位素特征等方面。加里东期岩溶储层主要受不整合面、断裂、岩性和古地貌等因素控制,表现出明显的断控和层控特征。由此预测该储层发育区位于古风化壳剥蚀区、加里东期断裂发育区和滩相储层发育区的叠合部位,主要位于阿克库勒凸起的轴部倾没端和塔河西南部、东南部的北东向、近南北向断裂发育区。 相似文献
275.
D. Nedjar M. Hamane M. Bensafi S.M. Elachachi D. Breysse 《Soil Dynamics and Earthquake Engineering》2007,27(2):111-115
Seismic response of buried pipes in longitudinal direction is studied. The effect of the variation of geotechnical properties of the surrounding soil on the stiffness, mass and damping of the soil is considered. The soil–structure interaction depends on pipe stiffness, joint stiffness, the variation of the soil stiffness and the soil mass and damping. Variations of the properties of the surrounding soil along the pipe are described by the random field theory. A numerical model is developed in order to simulate the effects of the variation of the soil on displacements, bending moments in the pipe and also to carry out a statistical analysis. The influence of different parameters regarding design and safety level of the pipe is conducted. 相似文献
276.
Fifty buried manganese nodules at different depth intervals were recovered in 12 sediment cores from the Central Indian Ocean Basin (CIOB). A maximum of 15 buried nodules were encountered in one sediment core (AAS-22/GC-07) and the deepest nodule was recovered at 5.50 m below seafloor in core AAS-04/GC-5A. Approximately 80% of the buried nodules are small in size (2 cm diameter) in contrast to the Atlantic Ocean and Peru Basin (Pacific Ocean) where the majority of the buried nodules are large, 8 cm and >6 cm, respectively. Buried nodule size decreases with core depth and this distribution appears to be similar to the phenomenon of “Brazil Nut Effect”. Buried nodules exhibit both smooth and rough surface textures and are ellipsoidal, elongated, rounded, sub rounded, irregular and polynucleated. Buried nodules from siliceous ooze are enriched in Mn, Cu, Ni, Zn, Mo, Ga, V and Rb whereas those from red clay are enriched in Fe, Co, Ti, U, Th, Y, Cr, Nb and Rare Earth Elements (REE). Buried nodules from siliceous ooze suggest their formation under hydrogenetic, early digenetic and diagenetic processes whereas those from red clay are of hydrogenetic origin.REE are enriched more than 1.5 times in buried nodules from red clay compared to siliceous ooze. However, the mode of incorporation of REE into buried nodules from both sedimentary environments is by a single authigenic phase consisting of Fe–Ti–P. Shale-normalized REE patterns and Ce anomalies suggest that nodules from siliceous ooze formed under more oxidizing conditions than those from red clay. Nodules buried at depths between 1.5 and 2.5 m are diagenetic (Mn/Fe ratio 10–15), formed in highly oxic environments (large positive Ce anomalies) and record aeolian dust (high Eu anomalies). Chemical composition, surface texture and morphology of buried nodules are similar to those of surface nodules from the same basin. Furthermore, buried nodule compositions do not exhibit any distinct patterns within the core depth, suggesting that buried nodules neither grow nor dissolve after their burial in the sediment column. 相似文献
277.
鄂尔多斯盆地高桥构造平缓地区奥陶系碳酸盐岩岩溶古地貌特征与储层分布 总被引:1,自引:0,他引:1
鄂尔多斯盆地高桥地区构造平缓,奥陶系顶部碳酸盐岩岩溶古地貌以岩溶潜台发育,而岩溶高地和岩溶斜坡发育局限为特征,岩溶斜坡区和岩溶潜台的东部沟槽区为储层发育区。本文综合利用大量岩心、薄片资料观察、物性实验数据和钻井、测井、地震等资料对高桥地区马家沟组顶的古岩溶识别标志进行了分析,恢复了岩溶古地貌,对岩溶古地貌类型(单元)进行了划分并分析其与储层的关系。高桥地区地层学标志,岩石学标志,矿物学标志,古岩溶发育的形迹说明奥陶系马家沟顶存在沉积间断、古岩溶作用已经是不容置疑的事实;按古风化壳出露层位,结合地震相追踪成果,落实沟槽分布,编制该区前石炭纪古地质图,运用古地质图法、印模法和残厚法恢复高桥岩溶古地貌,编制出岩溶古地貌图。根据岩溶古地貌,按岩溶单元划分为岩溶高地、岩溶斜坡和岩溶潜台三个二级地貌(类型)单元,岩溶高地可进一步分为岩溶台地、溶洼(洼地)2种三级微地貌类型。岩溶潜台进一步可划分为岩溶台地、溶洼、溶丘(残丘)、沟槽4种三级微地貌类型。高桥处于构造平缓地区,岩溶高地、岩溶斜坡区发育局限,大范围为岩溶潜台区且潜台区东侧沟槽(主沟槽、次沟槽)比较发育。岩溶高地整体储集性较东部岩溶斜坡区及岩溶潜台区差。岩溶斜坡区发育两套岩溶系统,储层条件相对较好,成藏要素配套较好,是下一步勘探开发的有利区域之一。岩溶潜台区总体岩溶作用减弱,储层发育程度变弱,东部沟槽区,因沟槽的存在,加强了垂向岩溶作用深度,间接增加侧向溶蚀作用,岩溶作用变好,储层发育程度增加,加上裂缝的影响,可以形成相对较好的储层。 相似文献
278.
279.
Existing relationships for lateral backfill pressures on pipelines assume that the trench is adequately wide to contain the failure surface. This condition is commonly violated in design and construction practice, putting at risk the pipeline safety. In this context, size and shape effects for trenches excavated in stiff soils and rocks, are numerically investigated, through experimentally-calibrated parametric analyses. It is shown that, for narrow trenches, ultimate pressures and yield displacements may increase up to an order of magnitude compared to “infinite-trench” values, while excavation of inclined walls reduces the above detrimental effects. Simplified relations are developed to aid pipeline design. 相似文献
280.
2.5D磁法反演估算铁矿资源量,关键是在垂直磁异常走向上求拟合模型的截面积。该文利用一种常见模型拟合4种实测磁场,发现铁矿截面积与埋深和磁性大小有一定的规律:磁化强度一定时,截面积与埋深呈线性正相关;埋深一定时,截面积与磁化强度呈近似指数形式的反相关。固定深部或外围磁性体参数,单独考虑浅部或中间铁矿模型时也有这种规律。在无钻孔资料及磁性资料不清楚时,磁化强度100 000×10-3~150 000×10-3A/m为估算铁矿资源量的最佳磁参数。因磁法反演的多解性,此类方法适用于钻孔验证前的资源量估计。 相似文献