全文获取类型
收费全文 | 14910篇 |
免费 | 2134篇 |
国内免费 | 2658篇 |
专业分类
测绘学 | 3295篇 |
大气科学 | 2199篇 |
地球物理 | 2214篇 |
地质学 | 6237篇 |
海洋学 | 1710篇 |
天文学 | 409篇 |
综合类 | 1313篇 |
自然地理 | 2325篇 |
出版年
2024年 | 35篇 |
2023年 | 121篇 |
2022年 | 341篇 |
2021年 | 452篇 |
2020年 | 471篇 |
2019年 | 579篇 |
2018年 | 402篇 |
2017年 | 553篇 |
2016年 | 516篇 |
2015年 | 632篇 |
2014年 | 779篇 |
2013年 | 787篇 |
2012年 | 899篇 |
2011年 | 1014篇 |
2010年 | 808篇 |
2009年 | 854篇 |
2008年 | 891篇 |
2007年 | 1075篇 |
2006年 | 1014篇 |
2005年 | 979篇 |
2004年 | 903篇 |
2003年 | 766篇 |
2002年 | 768篇 |
2001年 | 589篇 |
2000年 | 568篇 |
1999年 | 462篇 |
1998年 | 451篇 |
1997年 | 382篇 |
1996年 | 330篇 |
1995年 | 288篇 |
1994年 | 269篇 |
1993年 | 190篇 |
1992年 | 142篇 |
1991年 | 106篇 |
1990年 | 81篇 |
1989年 | 80篇 |
1988年 | 45篇 |
1987年 | 36篇 |
1986年 | 19篇 |
1985年 | 10篇 |
1984年 | 5篇 |
1982年 | 1篇 |
1981年 | 1篇 |
1980年 | 1篇 |
1979年 | 3篇 |
1978年 | 1篇 |
1954年 | 3篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
991.
Igor Jemcov 《Environmental Geology》2007,51(5):767-773
The management of groundwater flow systems in karst regions appears, at present, to be the most important procedure for solving
water deficiency problems during periods of low rainfall. Faced with a lack of data for characterizing the water supply potential
of karst aquifers, analyses of spring hydrographs may provide valuable indirect information regarding the structure of karst
hydrogeological systems. To estimate the optimal exploitation capacities of karstic sources, a stochastic-conceptual approach
was applied in case studies from the Serbian karst. Water supply potentials were initially evaluated on the basis of groundwater
budgets. Further steps towards defining optimal “exploitable” regimes included analyses of storage changes in karst water
reservoirs under natural conditions and calculation of the potential expansion of currently tapped sources. The results obtained
through these analyses are a significant contribution to feasibility studies and aid in the avoidance of problems of overexploitation. 相似文献
992.
Deep-large faults in the central continental margin of eastern China are well developed. Based on the regularity of spatial
and temporal distribution of the faults, four fault systems were divided: the Yanshan orogenic belt fault system, the Qinling-Dabie-Sulu
orogenic belt fault system, the Tanlu fault system and the East China Sea shelf basin-Okinawa trough fault system. The four
fault systems exhibit different migration behaviors. The Yanshan orogenic belt fault system deflected from an EW to a NE direction,
then to a NNE direction during the Indo-Chinese epoch-Yanshanian epoch. The thrust-nappe strength of the Qinling-Dabie orogenic
belt fault system showed the tendency that the strength was greater in the south and east, but weaker in the north and west.
This fault system faulted in the east and folded in the west from the Indo-Chinese epoch to the early Yanshanian epoch. At
the same time, the faults also had a diachronous migration from east to west from the Indo-Chinese epoch to the early Yanshanian
epoch. On the contrary, the thrust-nappe strength was greater in the north and west, weaker in the south and east during the
late Yanshanian epoch-early Himalayan epoch. The Tanlu fault system caused the basin to migrate from west to east and south
to north. The migration regularity of the East China Sea shelf basin-Okinawa trough fault system shows that the formation
age became younger in the west. The four fault systems and their migration regularities were respectively the results of four
different geodynamic backgrounds. The Yanshan orogenic belt fault system derived from the intracontinental orogeny. The Qinling-Dabie-Sulu
orogenic belt fault system derived from the collision of plates and intracontinental subduction. The Tanlu fault system derived
from the strike-slip movement and the East China Sea shelf basin-Okinawa trough fault system derived from plate subduction
and retreat of the subduction belt.
Translated from Journal of Jilin University (Earth Science Edition), 2005, 35(5): 554–563 [译自: 吉林大学学报 (地球科学版)] 相似文献
993.
首先进行了系统动力学方法应用于水资源承载能力评价的理论分析,提出了基于水资源供需紧张度系数的水资源承载能力系统动力学评价思路。进而结合江苏省水资源特点,计算了包含经济增长率、供水水平和保证率三组参数8种典型方案的江苏省水资源承载能力,为江苏省水资源承载能力建设提供了依据。 相似文献
994.
995.
996.
Vulnerability of groundwater in Quaternary aquifers to organic contaminants: a case study in Wuhan City,China 总被引:5,自引:0,他引:5
Yanxin Wang Broder J. Merkel Yilian Li Hui Ye Surong Fu Dana Ihm 《Environmental Geology》2007,53(3):479-484
More than 30 organic contaminants were detected in shallow groundwaters at Wuhan, the largest city in central China. Seriously
contaminated groundwaters were from densely populated, industrial and commercial areas. Abnormal concentrations were found
in groundwater from Hankou, downtown Wuhan: trimethylbenzene up to 29 μg/L, tetramethylbenzene up to 866 μg/L, and trichloroethene
up to 9.5 μg/L. Benzene, Toluene, Ethylene and Xylene (BTEX) contamination of groundwater is serious and widespread at Wuhan,
ranging between 0.14 and 25.0 μg/L. Considering the hydrogeological conditions of most Chinese cities, DRAMIC, a modified
version of the widely used DRASTIC model, was proposed by the authors for assessing vulnerability of groundwater to contamination.
The factors D, R, A and I in DRAMIC model are the same as in DRASTIC. The factor topography is ignored. The factor soil media is substituted by a new factor aquifer thickness (M) and the factor hydraulic conductivity of the aquifer by a new factor impact of contaminant (C). The equation for determining the DRAMIC Index is: DRAMIC = 5D
R + 3R
R + 4A
R + 2M
R + 5I
R + 1C
R. The calculated DRAMIC Index can be used to identify areas that are more likely to be susceptible to groundwater contamination
relative to each other. The higher the DRAMIC Index is, the greater the groundwater pollution potential. Applying DRAMIC,
a GIS-based vulnerability map for Wuhan city was prepared. Interestingly, places such as downtown Hankou, where enhanced concentrations
of BTEX have been detected, correspond quite well with those with higher DRAMIC ratings. 相似文献
997.
野外露头沉积学描述计算机辅助系统的任务是要帮助地质工作者实现野外露头沉积学描述信息的数字化处理,即利用计算机实现方便的数据录入、存储、管理、输出、辅助分析等。从地质模型分析入手,给出了系统的功能模型、模块划分和数据库模型。本系统的特点是实现了有关地质信息标准化采集、管理和处理分析,可为盆地分析、成岩成矿分析和区域地质调查工作提供技术支持。 相似文献
998.
天然气藏勘探的成功或失利,取决于气藏圈闭的封堵系统和散失系统。介绍了四川盆地气藏圈闭封堵系统和散失系统的类型、分布范围和对气藏圈闭的保存和破坏作用。气藏圈闭封堵系统的优劣取决于圈闭的有效封堵面与区域盖层的有效整体封闭条件和区域水动力停滞带环境条件,封堵系统良好的圈闭,勘探成功率高。气藏圈闭散失系统由缺乏区域盖层有效整体封闭条件的剥蚀区、区域水动力自由交替带环境、通天断层或潜伏通天断层组成。散失系统导致圈闭失效,从而造成勘探失利。通过对四川盆地天然气藏的破坏与保存条件的多个实例剖析,提出在四川盆地及我国南方海相天然气勘探中应当重视对天然气藏破坏与保存条件的研究,以利于天然气藏勘探区块、目标的选择和勘探效率的提高。 相似文献
999.
裂陷盆地中的构造变换带及其石油地质意义 总被引:16,自引:0,他引:16
构造变换带是裂陷盆地中的重要构造变形。讨论了构造变换带的含义、类型及对油气聚集的意义。裂陷盆地主干正断层之间的几何关系可以分为同向倾斜、背向倾斜和相向倾斜共3种组合方式;正断层之间的构造变换方式可以分为缓冲式、接力式、消长式、传递式和消减式等5种形式,构成15种类型的构造变换带。不同方式的断裂组合所形成的不同构造变换带类型会随着主干正断层位移的渐进增大发生相应的转变。构造变换带是有利的油气聚集区带:(1)它常常是主边界断裂带上地形高差变化较小的部位,是主要碎屑物源注入裂陷盆地的入口处,有利于发育储集层;(2)长期处于盆地内部相对高的构造部位,而且近邻生油凹陷,是油气运移指向区带;(3)它是裂陷盆地构造变形相对复杂的区带,有利于发育多种样式的油气圈闭。 相似文献
1000.
Wang Yong Hou Zengqian Mo Xuanxue Dong Fangliu Bi Xianmei Zeng Pusheng 《Frontiers of Earth Science》2007,1(3):322-332
More than 140 middle-small sized deposits or minerals are present in the Weishan-Yongping ore concentration area which is
located in the southern part of a typical Lanping strike-slip and pull-apart basin. It has plenty of mineral resources derived
from the collision between the Indian and Asian plates. The ore-forming fluid system in the Weishan-Yongping ore concentration
area can be divided into two subsystems, namely, the Zijinshan subsystem and Gonglang arc subsystem. The ore-forming fluids
of Cu, Co deposits in the Gonglang arc fluid subsystem have δD values between −83.8‰ and −69‰, δ18O values between 4.17‰ and 10.45‰, and δ13C values between −13.6‰ and 3.7‰, suggesting that the ore-forming fluids of Cu, Co deposits were derived mainly from magmatic
water and partly from formation water. The ore-forming fluids of Au, Pb, Zn, Fe deposits in the Zijinshan subsystem have δD
values between −117.4‰ and −76‰, δ18O values between 5.32‰ and 9.56‰, and Δ13C values between −10.07‰ and −1.5‰. The ore-forming fluids of Sb deposits have δD values between −95‰ and −78‰, δ18O values between 4.5‰ and 32.3‰, and Δ13C values between −26.4‰ and −1.9‰. Hence, the ore-forming fluids of the Zijinshan subsystem must have been derived mainly
from formation water and partly from magmatic water. Affected by the collision between the Indian and Asian plates, ore-forming
fluids in Weishan-Yongping basin migrated considerably from southwest to northeast. At first, the Gonglang arc subsystem with
high temperature and high salinity was formed. With the development of the ore-forming fluids, the Zijinshan subsystem with
lower temperature and lower salinity was subsequently formed.
Translated from Mineral Deposits, 2006, 25(1): 60–70 [译自: 矿床地质] 相似文献