全文获取类型
收费全文 | 1229篇 |
免费 | 279篇 |
国内免费 | 840篇 |
专业分类
测绘学 | 13篇 |
大气科学 | 2篇 |
地球物理 | 40篇 |
地质学 | 2117篇 |
海洋学 | 79篇 |
综合类 | 72篇 |
自然地理 | 25篇 |
出版年
2024年 | 5篇 |
2023年 | 23篇 |
2022年 | 38篇 |
2021年 | 47篇 |
2020年 | 35篇 |
2019年 | 60篇 |
2018年 | 54篇 |
2017年 | 67篇 |
2016年 | 87篇 |
2015年 | 89篇 |
2014年 | 119篇 |
2013年 | 122篇 |
2012年 | 161篇 |
2011年 | 112篇 |
2010年 | 122篇 |
2009年 | 121篇 |
2008年 | 90篇 |
2007年 | 115篇 |
2006年 | 123篇 |
2005年 | 91篇 |
2004年 | 86篇 |
2003年 | 82篇 |
2002年 | 59篇 |
2001年 | 42篇 |
2000年 | 63篇 |
1999年 | 64篇 |
1998年 | 47篇 |
1997年 | 47篇 |
1996年 | 51篇 |
1995年 | 33篇 |
1994年 | 20篇 |
1993年 | 15篇 |
1992年 | 14篇 |
1991年 | 10篇 |
1990年 | 5篇 |
1989年 | 9篇 |
1988年 | 5篇 |
1987年 | 5篇 |
1986年 | 2篇 |
1985年 | 4篇 |
1984年 | 2篇 |
1983年 | 1篇 |
1979年 | 1篇 |
排序方式: 共有2348条查询结果,搜索用时 15 毫秒
151.
西藏玉龙铜矿床次生氧化富集作用机制 总被引:8,自引:0,他引:8
作文阐述了西藏玉龙铜矿床成矿过程中的“沉积初步富集期”和“西藏玉龙铜矿床次生氧化成矿作用模式”,这不仅对指导当前生产具有重要的现实意义,而且为在玉龙铜矿带进一步找矿共作劈了新的方向。 相似文献
152.
153.
1∶20万区域化探扫面圈定出“三江”地区北段某多元素异常带,呈北西南东向条带状展布。由W、Mo、Cu、Bi、U、Sn、Ag、Cd、Pb、Zn、As、Ba、Hg、Au等高中低温热液成矿与伴生元素组成于一体,具典型的浓度分带与组分分带特征。它位于玉龙斑岩铜矿带北侧,对该异常带的解剖,具重要的理论与实际意义。 相似文献
154.
Victor B. MAGLAMBAYAN † Daizo ISHIYAMA Toshio MIZUTA Akira IMAI Yohei ISHIKAWA 《Resource Geology》1998,48(2):87-104
Abstract: The Bulawan deposit is located in the porphyry copper belt of southwest Negros island, Philippines. Propylitic, K–feldspar, sericitic, and carbonate alteration types can be distinguished in the deposit. Propylite alteration occurs mainly in Cretaceous-Eocene andesitic lavas and agglomerates while K–feldspar, sericite and carbonate alteration types occur mostly in the Middle Miocene dacite porphyry breccia pipes and stocks which were intruded into the andesites. K-feldspar zones occur in the inner parts of the sericitized zone. Sericite alteration overprinted the propylitized and K-feldspar alteration zones, at lower temperature than epidote and chlorite in the propylitized zone. Carbonate alteration is associated with the mineralization in the center of the breccia pipes and along faults. Mineralization consists of gold-silver telluride ores that are hosted by the carbonate– and sericite-altered dacite porphyry breccia pipes. The Bulawan ores occur mainly as disseminations, but unlike many epithermal gold deposits, lack classical epithermal colloform and crustiform quartz veins. The ore minerals are sphalerite, galena, chalcopyrite, pyrite and tetrahedite-tennantite with minor amounts of electrum, calaverite, petzite, sylvanite, hessite, tellurobismuthite, coloradoite, altaite, and rucklidgeite. Electrum and telluride minerals are associated mostly with calcite and dolomite-ankerite minerals. Fluid inclusions in quartz and calcite in clasts of propylitized andesite in the breccia pipes homogenize from about 300° to 400°C while fluid inclusions in quartz, calcite and sphalerite within the dacite porphyry breccia pipes homogenize between 300° to 310°C. The ores were formed around 300°C from hydrothermal solutions with salinity of about 6. 6 wt % NaCl equivalent. The presence of sylvanite and calaverite as intergrowths with each other, and the Ag content of calaverite are consistent with the above temperature estimate. Based on paragenesis, the Bulawan deposit formed in a pyrite-stable environment, with pH between 3. 4 and 5. 5, fO2 between 10-32 to 10-30 atm, fS2 between 10-9.8 to 10-7.8 atm, fTe2 between 10-8.9 to 10-6.5 atm, and total sulfur content about 10-2.8 molal. The dominant reduced sulfur species in the ore solutions may have been H2S(aq), and the likely aqueous tellurium species were H2Te(aq) and H2TeO3(aq). The ore minerals in the Bulawan deposit were probably formed by mixing of slightly saline and low salinity fluids. 相似文献
155.
Abstract: Myanmar is rich in mineral resources, and of potential importance are the deposits of antimony, chromium, nickel, PGM, copper, gold, lead, zinc, silver, tin and tungsten, which form district metallogenic provinces within the six geomor–phic–tectonic units. In terms of past production and potential mineral wealth Myanmar ranks high among Asian countries. The last few decades witnessed a dramatic fall in mineral production, but undoubtedly, the high level of mineral potential remains unrealized. This paper reveals mineral belts with a high level of economic potential which form attractive targets for mineral exploration and some individual mineral deposits of significant magnitude and grade, creating opportunities for development and mining investment. 相似文献
156.
稀矿山式铁铜矿床与奥林匹克坝式铜多金属矿床的对比研究 总被引:3,自引:0,他引:3
东川稀矿山式铁铜矿床与奥林匹克坝式铜、铀、金、稀土矿床对比研究表明,有其相似的地质构造背景和某些相近的成矿特征,但在某些成矿条件和矿化特征上又存在较大的差异。因此,在我国某些地质构造环境有利,稀矿山式铜多金属矿发育的地区,提出寻找类似奥林匹克坝式超大型铜多金属矿床,同时也应该注意稀矿山式铁铜矿床的成矿特征和评价标志。 相似文献
157.
根据福建省最新岩石测量成果得出的各岩类铜元素丰度,讨论和初步确定了福建铜的矿源层(岩)。提出可按照丰度值高低,铜的初始赋存状态与被解离的难易,有无矿床(点)及具找矿意义的异常产出这3项因素,进一步将矿源层(岩)划分为较可靠的、可能的和潜在的3个级别。 相似文献
158.
研究了滇池螺蛳(Margarya melanioides)分布和底泥营养成分之间的关系。2013年在滇池87个采样点采集螺蛳和底泥样本,图示分析所有采样点的活的螺蛳数量,确定活螺在滇池中的分布位点及分布密度;选择8个采样点的底泥样本,进行16项营养元素(有机质、磷、氮、锌、铁、锰、镁、钙、铜、钠、钾、砷、汞、铅、镉、铬)含量测定,分析这些样本营养元素的差异。根据这8个采样点中有无螺蛳生长,将8个底泥样本分为两组,采用完全随机设计两样本比较的t检验,结果两组样本间仅铜的含量有统计学差异(P0.05),这可能是由于滇池螺蛳的生长有效富集了重金属铜元素,使有螺区域比无螺区域底泥中铜的含量明显减少。这在一定程度上说明了螺蛳生长与底泥的关系,可为滇池污染防治及螺蛳种群保护提供相关的科学依据。 相似文献
159.
以中国南海常见的多毛类——华美盘管虫(Hydroides elegans)作为受试生物,分别研究了吡啶硫酮铜和吡啶硫酮锌对早期不同发育阶段的华美盘管虫的急性毒理效应。发现暴露于吡啶硫酮铜的华美盘管虫精子和卵子的受精半数抑制浓度(IC50)分别为19.49μg/L和88.44μg/L,担轮幼虫24 h半数致死浓度(24h-LC50)和48 h半数致死浓度(48h-LC50)分别为7.35μg/L和5.00μg/L,后担轮幼虫24h-LC50和48h-LC50分别为8.57μg/L和5.87μg/L;暴露于吡啶硫酮锌的华美盘管虫精子和卵子的受精IC50分别为36.74μg/L和159.59μg/L,担轮幼虫24 h-LC50和48 h-LC50分别为8.57μg/L和6.67μg/L,后担轮幼虫24 h-LC50和48 h-LC50分别为12.03μg/L和8.07μg/L。表明华美盘管虫早期发育的不同阶段对吡啶硫酮铜和吡啶硫酮锌的敏感性表现出一定差异,与配子受精率和后担轮幼虫的毒性反应相比,担轮幼虫对吡啶硫酮铜和吡啶硫酮锌的毒性表现出较高的敏感性;而且,对吡啶硫酮铜的敏感性普遍高于吡啶硫酮锌。 相似文献
160.
Lei Yanju Zhang Wenbing Xu Wei Zhang Yanjiao Zhou Huihui Mai Kangsen 《中国海洋大学学报(英文版)》2015,14(3):511-521
The aim of this study was to compare the effects of waterborne copper(Cu) and cadmium(Cd) on survival, anti-oxidative response, lipid peroxidation and metal accumulation in abalone Haliotis discus hannai. Experimental animals(initial weight: 7.49 g ± 0.01 g) were exposed to graded concentrations of waterborne Cu(0.02, 0.04, 0.06, 0.08 mg L-1) or Cd(0.025, 0.05, 0.25, 0.5mg L-1) for 28 days, respectively. Activities of the anti-oxidative enzymes(catalase, CAT; superoxide dismutase, SOD; glutathione peroxidases, GPx; glutathione S-transferase, GST), contents of the reduced glutathione(GSH) and malondiadehyde(MDA) in the hepatopancreas, and metal accumulation in hepatopancreas and muscles were analyzed after 0, 1, 3, 6, 10, 15, 21, 28 days of metal exposure, respectively. Results showed that 0.04 mg L-1, 0.06 mg L-1 and 0.08 mg L-1 Cu caused 100% death of abalone on the 21 st, 10 th and 6th day, respectively. However, no dead abalone was found during the 28-day waterborne Cd exposure at all experimental concentrations. Generally, activities of SOD and GST in hepatopancreas under all Cu concentrations followed a decrease trend as the exposure time prolonged. However, these activities were firstly increased and then decreased to the control level and increased again during Cd exposure. Activities of CAT in all Cu exposure treatments were higher than those in the control. These activities were firstly increased and then decreased to the control level and increased again during Cd exposure. Contents of MDA in hepatopancreas in all Cu treatments significantly increased first and then decreased to the control level. However, the MDA contents in hepatopancreas were not significantly changed during the 28-day Cd exposure. The metals accumulation in both hepatopancreas and muscles of abalone significantly increased with the increase of waterborne metals concentration and exposure time. These results indicated that H. discus hannai has a positive anti-oxidative defense against Cu or Cd. In conclusion, anti-oxidative mechanism in abalone to resist waterborne Cu did not follow the same pattern as that for waterborne Cd. 相似文献