全文获取类型
收费全文 | 7350篇 |
免费 | 1696篇 |
国内免费 | 2666篇 |
专业分类
测绘学 | 1005篇 |
大气科学 | 1418篇 |
地球物理 | 1621篇 |
地质学 | 4394篇 |
海洋学 | 1358篇 |
天文学 | 231篇 |
综合类 | 664篇 |
自然地理 | 1021篇 |
出版年
2024年 | 55篇 |
2023年 | 181篇 |
2022年 | 461篇 |
2021年 | 536篇 |
2020年 | 483篇 |
2019年 | 566篇 |
2018年 | 466篇 |
2017年 | 487篇 |
2016年 | 496篇 |
2015年 | 558篇 |
2014年 | 472篇 |
2013年 | 544篇 |
2012年 | 615篇 |
2011年 | 576篇 |
2010年 | 572篇 |
2009年 | 537篇 |
2008年 | 522篇 |
2007年 | 486篇 |
2006年 | 489篇 |
2005年 | 388篇 |
2004年 | 294篇 |
2003年 | 242篇 |
2002年 | 240篇 |
2001年 | 210篇 |
2000年 | 193篇 |
1999年 | 182篇 |
1998年 | 140篇 |
1997年 | 108篇 |
1996年 | 122篇 |
1995年 | 74篇 |
1994年 | 65篇 |
1993年 | 73篇 |
1992年 | 63篇 |
1991年 | 53篇 |
1990年 | 37篇 |
1989年 | 16篇 |
1988年 | 25篇 |
1987年 | 16篇 |
1986年 | 15篇 |
1985年 | 4篇 |
1984年 | 8篇 |
1983年 | 7篇 |
1982年 | 6篇 |
1981年 | 7篇 |
1980年 | 2篇 |
1979年 | 4篇 |
1958年 | 3篇 |
1957年 | 2篇 |
1954年 | 3篇 |
1933年 | 2篇 |
排序方式: 共有10000条查询结果,搜索用时 265 毫秒
941.
沉淀-陈化-返溶作用和压力对热液中氟钛络合物高温水解的影响及地质意义 总被引:3,自引:3,他引:0
钛是自然界中最不活泼的金属元素之一,然而越来越多的证据显示钛可以在特定条件下能进入热液流体中发生迁移,其中氟可能在其中扮演着重要的角色。本文研究了300℃和50~400MPa压力条件下氟钛络合物(K2Ti F6)的稳定性以及沉淀-陈化-返溶作用和压力对氟钛络合物水解行为的影响。研究结果显示,氟钛络合物水解的过程中,由于Ti O2沉淀物的陈化作用,在稳定的温度和压力条件下,沉淀物的返溶很难发生;但在缓慢降温和机械性振荡过程中,沉淀物的返溶会明显发生。而且,在温度不变的情况下,压力的改变对K2Ti F6水解并没有显著的影响,显示氟钛络合物不管在高压还是低压环境下均遵循近似的水解规律。本文认为主要的原因在于压力的增高会促进水解反应沉淀物的陈化,进而抑制沉淀物的返溶,但并不破坏水解反应的平衡。最后,本文提出金属络合物的形成-水解-沉淀/返溶-陈化过程是水-岩作用或热液成矿过程中高场强元素活化、迁移和成矿的主要机制。 相似文献
942.
943.
胶北地体早前寒武纪重大岩浆事件、陆壳增生及演化 总被引:4,自引:4,他引:0
早前寒武纪重大岩浆事件是早期陆壳增生及演化的主要地质作用。本文通过系统总结最近几年胶北地体早前寒武纪重大岩浆事件代表性岩石的岩相学、锆石U-Pb年代学、岩石地球化学及锆石Hf同位素研究的最新成果,厘定出太古宙~2.9Ga、2.7Ga及2.5Ga三期以TTGs岩浆事件为代表的陆壳增生事件。这些TTGs具有典型太古宙高铝TTGs的地球化学特征及正的εHf(t)值,锆石Hf模式年龄主要集中在ca.3.2~2.7Ga。两种不同的构造模式被用来理解胶北太古宙TTGs(陆壳)的成因:(1)加厚基性下地壳的部分熔融;(2)俯冲洋壳的部分熔融。根据胶北TTGs在时间上呈事件性侵位,空间上呈面状分布,以及相对较低的Mg#、Cr及Ni含量,前者可能更适合胶北TTGs的成因。确定了胶北古元古代2.2~2.0Ga黑云母/角闪石二长花岗片麻岩及~1.8Ga以二长(正长)花岗岩为代表的多期陆壳重熔事件。综合这些研究结果,初步总结出胶北早前寒武纪陆壳形成及演化历史:1)2.9Ga,主要为基性地壳(洋壳)的增生,并可能存在规模有限的、被剥蚀殆尽的太古宙早期陆壳;2)在~2.9Ga、~2.7Ga及~2.5Ga,由于地幔(热)柱上涌,ca.3.3~2.7Ga新生的加厚基性玄武质下地壳发生事件性部分熔融,并伴随有早期陆壳的重熔,形成主要由TTGs及少量陆壳重熔型(高钾)花岗岩组成的太古宙陆壳;3)ca.2.2~2.0Ga,可能由于地幔物质上涌,陆壳伸展,形成裂谷,陆壳物质重熔,形成ca.2.2~2.0Ga花岗质岩石;4)ca.1.95~1.85Ga,发生强烈的挤压碰撞构造作用,裂谷闭合,卷入挤压作用的物质发生高角闪岩相到高压麻粒岩相变质;5)~1.8Ga,地幔物质上涌,陆壳伸展减薄,陆壳物质重熔,形成~1.8Ga花岗岩。 相似文献
944.
古盐湖卤水温度对钾盐沉积的控制作用探讨 总被引:2,自引:0,他引:2
古盐湖卤水的温度对钾盐沉积的控制作用的定量研究是钾盐成矿机理分析的重点和难点。本文分析和测试陕北盐盆奥陶系马家沟组、四川盆地三叠系嘉陵江组、云南兰坪-思茅盆地白垩系及老挝沙空那空盆地白垩系等八个含盐系的石盐岩中的流体包裹体,并利用均一温度计算了古盐湖的蒸发速率。若以老挝白垩纪时盐湖的蒸发速率为标准值100,陕北奥陶纪、四川三叠纪、云南白垩纪的蒸发速率标准值分别为54、68和90,而目前在老挝和云南白垩系都找到了一定规模的钾盐矿,因此高温(气温及水温)是盐湖成钾的有利条件,在卤水演化成钾的过程中可以起到重要的"催化"作用。 相似文献
945.
946.
四川省武都水库右岸EL574 m灌浆平洞揭露出厚度2.3~9.8 m的粉细砂层,普通水泥高压灌浆无法形成可靠的防渗帷幕。采用高压旋喷、湿磨细水泥、化学灌浆的组合处理方式,取得了较好的施工效果。通过钻孔压水、大功率声波CT、单孔声波、钻孔全景数字成像等方法检测,表明达到了设计防渗要求。 相似文献
947.
This work aims to quantify sulfate ion concentrations in the system Na2SO4-H2O using Raman micro-spectroscopy.Raman spectra of sodium sulfate solutions with known concentrations were collected at ambient temperature(293 K) and in the 500 cm1-4000 cm-1 spectral region.The results indicate that the intensity of the SO42- band increases with increasing concentrations of sulfate ion.A linear correlation was found between the concentration of SO42-(c) and parameter I1,which represents the ratio of the area of the SO42- band to that of the O-H stretching band of water(As/Aw):I1=-0.00102+0.01538 c.Furthermore,we deconvoluted the O-H stretching band of water(2800 cm-1-3800 cm-1) at 3232 and 3430 cm-1 into two sub-Gaussian bands,and then defined Raman intensity of the two sub-bands as ABi(3232 cm-1) and AB2(3430 cm-1),defined the full width of half maximum(FWHM) of the two sub-bands as WB1(3232 cm-1) and WB2(3430 cm-1).A linear correlation between the concentration of SO42-(c) and parameter I2,which represents the ratio of Raman intensity of SO42-(As)(in 981 cm-1) to(AB1+AB2),was also established:I2=-0.0111+0.3653 c.However,no correlations were found between concentration of SO42-(c) and FWHM ratios,which includes the ratio of FWHM of SO42-(Ws) to WB1 WB2 and WB1+B2(the sum of WB1 and WB2),suggesting that FWHM is not suitable for quantitative studies of sulfate solutions with Raman spectroscopy.A comparison of Raman spectroscopic studies of mixed Na2SO4 and NaCI solutions with a constant SO42- concentration and variable CI- concentrations suggest that the I\ parameter is affected by CI-,whereas the I2 parameter was not.Therefore,even if the solution is not purely Na2SO4-H2O,SO42- concentrations can still be calculated from the Raman spectra if the H2O band is deconvoluted into two sub-bands,making this method potentially applicable to analysis of natural fluid inclusions. 相似文献
948.
In Europe, fossil fruits and seeds of Rhodoleia (Hamamelidaceae) have been described from the Upper Cretaceous to the Miocene, whereas no fossil record of Rhodoleia has been reported in Asia, where the modern species occur. Herein, 21 fossil leaves identified as Rhodoleia tengchongensis sp. nov. are described from the Upper Pliocene of Tengchong County, Yunnan Province, Southwest China. The fossils exhibit elliptic lamina with entire margins, simple brochidodromous major secondary veins, mixed percurrent intercostal tertiary veins, and looped exterior tertiaries. The leaf cuticle is characterized by pentagonal or hexagonal cells, stellate multicellular trichomes, and paracytic stomata. The combination of leaf architecture and cuticular characteristics suggests that the fossil leaves should be classified into the genus Rhodoleia. The fossil distributions indicate that the genus Rhodoleia might originate from Central Europe, and that migrated to Asia prior to the Late Pliocene. Additionally, insect damage is investigated, and different types of damage, such as hole feeding, margin feeding, surface feeding, and galling, are observed on the thirteen fossil leaves. Based on the damage frequencies for the fossil and extant leaves, the specific feeding behavior of insects on Rhodoleia trees appears to have been established as early as the Late Pliocene. The high occurrence of Rhodoleia insect herbivory may attract the insect-foraging birds, thereby increasing the probability of pollination. 相似文献
949.
<正>1 Introduction The organic-rich shale in Lower Silurian Longmaxi formation Sichuan Basin is marine sedimentary strata,and it has large thickness and rich resources.Therefore,it is one of the most important parts in unconventional oil and gas reservoir exploration.Eastern Sichuan area is located 相似文献
950.
YANG Minghui LI Liang ZHOU Jin JIA Huichong SUN Xiao GONG Ting DING Chao 《《地质学报》英文版》2015,89(5):1636-1648
The hydrocarbon potential of the Hangjinqi area in the northern Ordos Basin is not well known, compared to the other areas of the basin, despite its substantial petroleum system.Restoration of a depth-converted seismic profile across the Hangjinqi Fault Zone(HFZ) in the eastern Hangjinqi area shows one compression that created anticlinal structures in the Late Triassic, and two extensions in ~Middle Jurassic and Late Early Cretaceous, which were interrupted by inversions in the Late Jurassic–Early Early Cretaceous and Late Cretaceous, respectively.Hydrocarbon generation at the well locations in the Central Ordos Basin(COB) began in the Late Triassic.Basin modeling of Well Zhao-4 suggests that hydrocarbon generation from the Late Carboniferous–Early Permian coal measures of the northern Shanbei Slope peaked in the Early Cretaceous, predating the inversion in the Late Cretaceous.Most source rocks in the Shanbei Slope passed the main gas-migration phase except for the Hangjinqi area source rocks(Well Jin-48).Hydrocarbons generated from the COB are likely to have migrated northward toward the anticlinal structures and traps along the HFZ because the basin-fill strata are dipping south.Faulting that continued during the extensional phase(Late Early Cretaceous) of the Hangjinqi area probably acted as conduits for the migration of hydrocarbons.Thus, the anticlinal structures and associated traps to the north of the HFZ might have trapped hydrocarbons that were charged from the Late Carboniferous–Early Permian coal measures in the COB since the Middle Jurassic. 相似文献