全文获取类型
收费全文 | 1920篇 |
免费 | 446篇 |
国内免费 | 519篇 |
专业分类
测绘学 | 10篇 |
大气科学 | 83篇 |
地球物理 | 96篇 |
地质学 | 1704篇 |
海洋学 | 98篇 |
天文学 | 727篇 |
综合类 | 69篇 |
自然地理 | 98篇 |
出版年
2024年 | 21篇 |
2023年 | 50篇 |
2022年 | 118篇 |
2021年 | 141篇 |
2020年 | 122篇 |
2019年 | 133篇 |
2018年 | 105篇 |
2017年 | 106篇 |
2016年 | 187篇 |
2015年 | 108篇 |
2014年 | 141篇 |
2013年 | 119篇 |
2012年 | 107篇 |
2011年 | 90篇 |
2010年 | 64篇 |
2009年 | 141篇 |
2008年 | 106篇 |
2007年 | 154篇 |
2006年 | 163篇 |
2005年 | 127篇 |
2004年 | 110篇 |
2003年 | 88篇 |
2002年 | 61篇 |
2001年 | 57篇 |
2000年 | 54篇 |
1999年 | 65篇 |
1998年 | 40篇 |
1997年 | 18篇 |
1996年 | 10篇 |
1995年 | 10篇 |
1994年 | 12篇 |
1993年 | 8篇 |
1992年 | 10篇 |
1991年 | 5篇 |
1990年 | 5篇 |
1989年 | 4篇 |
1988年 | 8篇 |
1987年 | 1篇 |
1986年 | 8篇 |
1985年 | 5篇 |
1984年 | 2篇 |
1981年 | 1篇 |
排序方式: 共有2885条查询结果,搜索用时 78 毫秒
61.
系统岩心观察和高密度薄片鉴定等分析测试资料研究结果显示,济阳坳陷沙三下-沙四上泥页岩成分组成及构造类型主要受沉积作用控制,岩石结构特征主要受成岩作用控制。根据泥页岩中方解石成因及重结晶程度,结合岩石成分及构造特征,将济阳坳陷沙三下-沙四上泥页岩划分为沉积主控型、沉积-成岩双控型及成岩主控型三大成因相。沉积主控型分布最为广泛,岩相类型多样,构造特征反映成因环境;沉积-成岩双控型主要见于纹层状岩相,由泥质纹层与显晶粒状方解石纹层互层构成;成岩主控型以柱状、柱纤状方解石垂直层面呈脉状、透镜状产出为特征。成岩主控型和沉积-成岩双控型泥页岩与页岩油气关系密切,是重要的有利成因相类型。 相似文献
62.
涪陵地区页岩层蕴含着丰富的天然气资源,具有较大的开采前景。区块主要目的层为上奥陶统五峰组-下志留统龙马溪组下部页岩气层。上部泥页岩地层井壁稳定性差,地层承压能力低,溶洞发育、易坍塌、易漏失;海相沉积地层流体分布复杂,部分地层岩性变化大,可钻性差,机械钻速较低;采用丛式布井,水平井井眼轨迹复杂,靶前位移大,大井眼定向扭方位困难、托压严重。现场试验使用了旋转导向、扭力冲击器、旋冲马达、水力振荡器等新技术、新工具,大幅度提高机械钻速,缩短钻井周期,取得一定的经济效益。阐述了几种新技术和新工具的工作原理、现场应用情况,并对其经济效果进行了评价。 相似文献
63.
64.
65.
66.
Cretaceous-Paleocene organic-rich sediments in Egypt occur as an east-west trending belt extending from the Quseir-Safaga district (Red Sea) to the Kharga-Dakhla (Western Desert) region. They are associated with the Duwi Formation (phosphate-bearing) and the overlying Dakhla Formation (deeper epicontinental shale/marl). This study aims to reconstruct the paleo-redox conditions during deposition of these thermally immature organic-rich sediments using carbon-sulfur-iron systematics and trace metal proxies in two cores, one each from the Quseir and Abu Tartur areas. Paleoproductivity, based on P content, seems to have been higher in the Quseir section than in the Abu Tartur section. The Quseir section also records a relatively greater occurrence of anoxic conditions during the accumulation of these sediments than the Abu Tartur section. This difference is indicated by its markedly higher total organic carbon (TOC) content as well as higher contributions of redox-sensitive and sulfide-forming metals (Mo, U, Ni, V, and Co). A weak correlation exists between S and TOC, and a positive S intercept (>1) was observed in most of the rock units of the study sections. A high consistency between the TOC-S-Fe relations and trace metals findings was found. The uppermost Duwi and the lowermost Dakhla strata, which have the highest TOC and represent a maximum sea transgression during the Late Cretaceous, have the highest contents of redox-sensitive trace metals. The carbonate-dominated transgressive Baris and Beida members of the Dakhla Formation record relatively stronger oxygen-depleted conditions during their accumulation than others, which led to relatively higher TOC contents and redox-sensitive metal accumulations. A scenario for the environmental conditions that existed during the deposition of these organic-rich successions, based on compiled trace metals and TOC-S-Fe implications, is reconstructed here. 相似文献
67.
When trying to improve gas productivity from unconventional sources a first aim is to understand gas storage and gas flow potential through the rock by investigating the microstructure, mineralogy and matrix porosity of unfractured shale. The porosity and mineralogy of the Mulgrave Shale member of the Whitby Mudstone Formation (UK) were characterized using a combination of microscopy, X-ray diffraction and gas adsorption methods on samples collected from outcrops. The Whitby Mudstone is an analogue for the Dutch Posidonia Shale which is a possible unconventional source for gas. The Mulgrave shale member of the Whitby Mudstone Formation can microstructurally be subdivided into a fossil rich (>15%) upper half and a sub-mm mineralogically laminated lower half. All clasts are embedded within a fine-grained matrix (all grains < 2 μm) implying that any possible flow of gas will depend on the porosity and the pore network present within this matrix. The visible SEM porosity (pore diameter > 100 nm) is in the order of 0.5–2.5% and shows a non-connected pore network in 2D. Gas adsorption (N2, Ar, He) porosity (pore diameters down to 2 nm) has been measured to be 0.3–7%. Overall more than 40% of the visible porosity is present within the matrix. Comparing the Whitby Mudstone Formation to other (producing) gas shales shows that the rock plots in the low porosity and high clay mineral content range, which could imply that Whitby Mudstone shales could be less favourable to mechanical fracturing than other gas shales. Estimated permeability indicates values in the micro-to nano-darcy range. 相似文献
68.
《世界地质(英文版)》2016,(1):48-54
The unconventional oil and gas resources presented in oil shales have meant these potential sources of hydrocarbons,which has become a research focus. China contains abundant oil shale resources,ranking fourth in the world,with ca. 7 254. 48 × 10~8 t within 24 provinces,including 48 basins and 81 oil shale deposits. About 48% of the total oil shale resources are concentrated in the eastern resource region,with a further 22% in the central resource region. 65% of the total quantity of oil shale resources is present at depths of 0-500 m,with 17% of the total resources being defined as high-quality oil shales yielding more than 10% oil by weight.Chinese oil shale resources are generally hosted by Mesozoic sediments that account for 78% of the total resources. In terms of the geographical distribution of these resources,some 45% are located in plain regions,and different oil shale basins have various characteristics. The oil shale resources in China represent a highly prospective future source of hydrocarbons. These resources having potential use not only in power generation and oil refining but also in agriculture,metal and chemical productions,and environmental protection. 相似文献
69.
针对柴达木盆地北缘鱼卡凹陷中侏罗统大煤沟组泥页岩,利用地震频谱曲线在不同流体介质储层中的形态、斜率、主频与中心频率的差值等属性参数特征,识别陆相泥页岩层系的地震频谱属性特征,预测含气性。研究结果表明,中侏罗统大煤沟组上部能量系数较低,平均为0.6719,下部能量系数较高,平均为0.7521,结合现场含气量和全烃特征认为,可以以能量系数0.7为界线,作为识别下部和上部含气性的标志,下部明显比上部含气性好。平面上进一步圈定了2个有利目标区,得到柴页1井勘探验证。因此,频谱分解技术可应用于中国陆相页岩气的勘查开发。 相似文献
70.
页岩储层测井评价是后期压裂改造工程的基础,通过分析柴页1井常规测井曲线特征,结合特殊测井和岩心样品分析化验数据,综合评价了中侏罗统大煤沟组页岩岩性、物性、地球化学、含气性、可压裂性等特征,获得了储层评价及工程改造参数。柴页1井中侏罗统大煤沟组至少发育128.1m厚的富有机质页岩,具有高伽马、高声波时差、高中子、高电阻、低密度的特点;测井计算有利的富有机质页岩的总有机碳含量介于3.20%~4.20%之间,总含气量介于1.50~4.50m3/t之间,有利页岩层段脆性矿物含量介于45%~75%之间,划分出3个有利层组,第Ⅰ层组和第Ⅱ层组具有杨氏模量高、泊松比低的特点,有利于后期射孔压裂。 相似文献