全文获取类型
收费全文 | 801篇 |
免费 | 136篇 |
国内免费 | 356篇 |
专业分类
测绘学 | 44篇 |
大气科学 | 107篇 |
地球物理 | 219篇 |
地质学 | 610篇 |
海洋学 | 74篇 |
天文学 | 23篇 |
综合类 | 99篇 |
自然地理 | 117篇 |
出版年
2024年 | 10篇 |
2023年 | 29篇 |
2022年 | 40篇 |
2021年 | 40篇 |
2020年 | 15篇 |
2019年 | 46篇 |
2018年 | 37篇 |
2017年 | 26篇 |
2016年 | 31篇 |
2015年 | 48篇 |
2014年 | 71篇 |
2013年 | 58篇 |
2012年 | 41篇 |
2011年 | 53篇 |
2010年 | 43篇 |
2009年 | 50篇 |
2008年 | 44篇 |
2007年 | 56篇 |
2006年 | 71篇 |
2005年 | 36篇 |
2004年 | 37篇 |
2003年 | 48篇 |
2002年 | 35篇 |
2001年 | 33篇 |
2000年 | 44篇 |
1999年 | 31篇 |
1998年 | 26篇 |
1997年 | 23篇 |
1996年 | 24篇 |
1995年 | 19篇 |
1994年 | 20篇 |
1993年 | 17篇 |
1992年 | 20篇 |
1991年 | 18篇 |
1990年 | 15篇 |
1989年 | 12篇 |
1988年 | 11篇 |
1987年 | 4篇 |
1986年 | 1篇 |
1985年 | 2篇 |
1984年 | 1篇 |
1982年 | 2篇 |
1981年 | 1篇 |
1980年 | 1篇 |
1979年 | 2篇 |
1978年 | 1篇 |
排序方式: 共有1293条查询结果,搜索用时 15 毫秒
41.
安山岩是俯冲相关构造环境的特征岩石;对安山岩的研究,可以获得俯冲作用发生时代和俯冲过程的相关信息.报道了中天山地块南缘乌瓦门地区早志留世安山岩的年代学和地球化学特征,探讨了其岩石成因和构造属性,为南天山洋及中天山陆块南缘构造演化提供制约.研究表明,乌瓦门安山岩具有安山结构,组成矿物为普通辉石、钙质角闪石、斜长石和钾钠长石,为高钾钙碱性粗面安山岩;全岩SiO2=56.23%~59.28%,K2O=2.70%~3.37%,Na2O=3.32%~4.11%.其锆石U-Pb年龄为430 Ma,形成于早志留世晚期.微量元素组成上,富集轻稀土、亏损重稀土,(La/Yb)N=18.5~20.9;Eu负异常不明显,δEu=0.82~0.88;富集Ba、Th、U,亏损Nb、Ta、Ti;初始87Sr/86Sr比值为0.706 2~0.707 5,εNd(t)=+2.96~+3.01;这些数据揭示乌瓦门安山岩为安第斯型陆弧岩石,起源于被俯冲带相关流体交代的地幔楔,并在上升过程中受到了古老地壳的改造.早志留世晚期,南天山洋向中天山陆块下俯冲,构成成熟的洋-陆俯冲体系;中天山陆块南缘为活动大陆边缘,发育典型的安第斯型陆弧岩石组合. 相似文献
42.
云开地块东缘粤西圭岗镇附近寒武系之上不整合覆盖一套灰白色石英砾岩-含砾砂岩,由于缺乏化石和年龄依据,这套岩石的时代长期存有争议.利用LA-ICP-MS U-Pb测年手段,对该套含砾碎屑沉积岩及其上下层位进行了U-Pb测年,4件样品共获得300组有效数据,年龄变化于2 900~400 Ma,不整合面之下样品主要集中于1 100~700 Ma,不整合面之上最年轻碎屑锆石年龄集中于450~400 Ma.新的测年数据结合前人研究成果表明,云开地块东缘不整合面下伏及上覆地层的时代分别为寒武纪和泥盆纪.研究区寒武纪时期物源特征与印度、东南极洲和澳大利亚西部相似,指示该时期研究区同冈瓦纳东北缘相连,物源来自东冈瓦纳北缘南极洲、印度地块和澳大利亚之间的造山带,而泥盆纪物源主要来自邻近的云开地块.寒武系和泥盆系之间的不整合面是早古生代郁南运动与广西运动叠加的产物. 相似文献
43.
为调查庐枞矿集区中东部七家山—马口地区深部矿产资源潜力,利用小波变换方法提取深源重磁场,通过对垂向一阶导数Z与水平方向导数模S进行参数变换,突出深源重磁场的局部异常; 结合频谱激电(spectrum induced polarization,SIP)、可控源音频大地电磁测深(controlled source audio-frequency magneto tellurics,CSAMT)成果,在调查区深部查明了一条长大于3.0 km、宽大于0.5 km的高重低磁、低阻高极化异常带; 根据调查区内外已知铜矿(化)体分布规律,结合已知矿(化)体在深源重磁异常中的分布及钻孔(zk4601)钻探验证结果,认为上述异常带是铜多金属矿化蚀变带的反映,是寻找铜多金属矿的有利部位,具有较好的找矿前景。 相似文献
44.
南秦岭北缘小茅岭复式岩体主要由宋家屋场基性辉绿(辉长)岩,迷魂阵、磨沟峡和叶家湾中性-偏酸性闪长岩组成,形成于新元古代早期870~840 Ma。岩石地球化学研究显示,宋家屋场基性岩属亚碱性系列岩石,富集轻稀土元素及大离子亲石元素,Nb、Ta、Ti、P等具有弱的负异常,Zr、Hf等高场强元素的含量较高,Zr/Y、Ta/Yb比值较高,Zr/Nb比值较低,与岛弧玄武岩的地球化学特征相似,在构造环境判别图解中投于火山弧岩石区域,一些元素的富集特征可能来源于受俯冲块体流体交代的岩石圈地幔。迷魂阵、磨沟峡及叶家湾闪长岩体均属准铝质亚碱性系列岩石,具有岛弧火成岩的地球化学特征。Sr-Nd-Hf同位素地球化学分析显示,宋家屋场岩体主要来自亏损地幔源区,磨沟峡和叶家湾岩体主要为新生基性下地壳的部分熔融,而迷魂阵岩体主要为古老地壳物质的部分熔融。上述特征表明小茅岭复式岩体各组成部分可能形成于870~840 Ma俯冲相关的岛弧构造背景,俯冲块体脱水形成的流体交代上覆地幔楔,这种地幔部分熔融形成了宋家屋场角闪辉绿(辉长)岩,由于基性岩浆的加热,诱发新生基性下地壳及原古老地壳物质部分熔融,岩浆上升、侵位,形成磨沟峡、叶家湾及迷魂阵岩体。结合陡岭地区~850–780 Ma变质作用及岩浆事件相关报导,在南秦岭北缘小茅岭—陡岭隆起带上,新元古代早期存在一期构造-岩浆-变质事件,该事件的区域大地构造属性则有待进一步研究。 相似文献
45.
Trace metals in seawater and copepods in the ocean outfall area off the northern Taiwan coast 总被引:3,自引:0,他引:3
The distribution, partitioning and concentrations of trace metals (Cd, Cr, Cu, Fe, Mn, Pb and Zn) in seawater, including dissolved and particulate phases, and in copepods in the ocean outfall area off the northern coast of Taiwan were investigated. Normalization of metal concentrations to the background metal concentration to yield relative enrichment factors (EF), which were used to evaluate the contamination of dissolved and particulate trace metals in seawater around the ocean outfall. The EF results indicated that the outfall area was significantly contaminated by dissolved Fe and Zn, and by particulate Fe, Cr, Cu, Pb and Zn. In addition, most trace metals were chiefly in the particulate phase. The average percentage of total metal concentrations (dissolved plus particulate phases) bound by suspended particulate matter followed the sequence Al(95%) = Mn(95%) > Pb(88%) > Cu(86%) > Fe(72%) > Zn(32%) > Cr(17.5%) > Cd(3.4%). Therefore, metal contamination is better evaluated in solid phase than in the dissolved phase. The concentration ranges of trace metals in the copepods, Temora turbinata, Oncaea venusta and Euchaeta rimana, near the outfall were: Cd, 0.23-1.81 microg g(-1); Cr, 16.5-195 microg g(-1); Cu, 14-160 microg g(-1); Fe, 256-7255 microg g(-1); Mn, 5.5-80.8 microg g(-1); Pb, 2.6-56.2 microg g(-1); Zn, 132-3891 microg g(-1); and Al, 0.21-1.13%. Aluminum, and probably Fe, seemed to be the major elements in copepods. The concentrations of trace metals in copepods, especially Temora turbinata, near the outfall were generally higher than those obtained in the background station. The mean increase in bioconcentration factor of metals in copepods ranged from 4 to 7 and followed the sequence Al(6.4) > Cu(6.2) > Fe(6.0) > Zn(5.7) > Pb(5.6) > Cr(5.5) > Cd(5.1) > Mn(4.7). Therefore, marine copepods in the waters of northern Taiwan can accumulate trace metals over background concentrations and act as contamination indicators. 相似文献
46.
47.
WANG Wei DONG Fei SHI Lite CAO Fang 《地球空间信息科学学报》2006,9(1):49-54
Introduction Thebasiclandpriceistheaveragepriceofev eryequalparceloreverylandclassspecifiedby thegovernment,accordingtodifferentuseof landsuchascommerce,industry,residence,etc.Asanimportantroleplayingintheurban landpricesystem,thebasiclandpriceinstructs a… 相似文献
48.
Hui Li Bo Chen Li Feng Ying Li Yu Huang Jing-Wei Li Lei Lu Jian-Chao Xue Bei-Li Ying Jie Zhao Yu-Tong Yang Wei-Qun Gan Cheng Fang Ke-Fei Song Hong Wang Quan-Feng Guo Ling-Ping He Bo Zhu Cheng Zhu Lei Deng Hai-Chao Bao Cai-Xia Cao Zhong-Guang Yang 《天文和天体物理学研究(英文版)》2021,(2)
As a result of an error by the authors,in the paper"The Lyman-alpha Solar Telescope(LST)for the ASO-S Mission.I.Scientific Objectives and Overview"by Hui Li et al.(RAA 2019 Vol.19,No.11,158,doi:10.1088/1674C4527/19/11/158),there is an error occurred in Table 2 about the image size of SCI UV in the'Event'mode:the image size 4608×4608 should be replaced by 2048×2048.This correction is indicated in bold face in the following table. 相似文献
49.
Ophiopholis mirabilis is a common species with a high population density on the western coasts of the northern Pacifi c Ocean.The number of O.mirabilis has been increasing recently in the scallop aquaculture zone(the Zhangzi Island area,northern Yellow Sea)in China.To explore the mechanism of its population variation,the reproductive cycle of O.mirabilis was investigated in this area(39°04′N;122°51′E)from February 2017 through January 2018 and determined by the monthly gonad index(GI),histological examinations of the gonads and the oocyte size-frequency distribution.O.mirabilis had a clear annual reproductive cycle that was synchronous between males and females.Sea temperature and food availability played important roles in O.mirabilis reproduction.The GI value was less reliable for determining reproductive activity in O.mirabilis because the nutritive tissues within the gonads may be utilized to synthesize gametes,leading to a decrease in GI during maturation.The histological results also show that abundant nutritive phagocytes were present in the gonads of O.mirabilis,which,together with the germ cells,aff ected the weight of the gonads.In addition,the mature oocytes of O.mirabilis were relatively small(75–150μm),indicating that the larval development was planktotrophic.This study provided insights into the reproductive patterns and biology of O.mirabilis and is an essential basis for the quantity control of this species in aquaculture areas. 相似文献
50.
Zengjia XIAO Jianguo ZHAO Qingliang ZHONG Fang OUYANG Xinze LIU Bohong YAN Zhi LI Ming MA Bin WANG Xiaoqiong WANG 《中国科学:地球科学(英文版)》2023,(7):1603-1621
The rock mechanical properties and elastic anisotropy of terrestrial shale oil reservoirs are affected by various factors,such as lithology, structure, pores, fractures, and fluids. The experimental study of dynamic and static elastic properties can provide important mechanism analysis for the prediction of geological and engineering “sweet spots” in shale reservoirs. There are a large number of studies on the measurement of static mechanical properties of shale, but the experiments on dynamic c... 相似文献