全文获取类型
收费全文 | 16930篇 |
免费 | 4121篇 |
国内免费 | 6110篇 |
专业分类
测绘学 | 3454篇 |
大气科学 | 2442篇 |
地球物理 | 3074篇 |
地质学 | 10770篇 |
海洋学 | 3245篇 |
天文学 | 303篇 |
综合类 | 1343篇 |
自然地理 | 2530篇 |
出版年
2024年 | 140篇 |
2023年 | 385篇 |
2022年 | 1015篇 |
2021年 | 1311篇 |
2020年 | 1054篇 |
2019年 | 1162篇 |
2018年 | 1067篇 |
2017年 | 1016篇 |
2016年 | 1011篇 |
2015年 | 1210篇 |
2014年 | 1135篇 |
2013年 | 1464篇 |
2012年 | 1597篇 |
2011年 | 1580篇 |
2010年 | 1457篇 |
2009年 | 1407篇 |
2008年 | 1524篇 |
2007年 | 1359篇 |
2006年 | 1405篇 |
2005年 | 1117篇 |
2004年 | 882篇 |
2003年 | 581篇 |
2002年 | 598篇 |
2001年 | 578篇 |
2000年 | 425篇 |
1999年 | 256篇 |
1998年 | 81篇 |
1997年 | 54篇 |
1996年 | 46篇 |
1995年 | 30篇 |
1994年 | 26篇 |
1993年 | 18篇 |
1992年 | 35篇 |
1991年 | 7篇 |
1990年 | 25篇 |
1989年 | 8篇 |
1988年 | 4篇 |
1987年 | 15篇 |
1986年 | 7篇 |
1985年 | 9篇 |
1984年 | 13篇 |
1983年 | 8篇 |
1982年 | 5篇 |
1981年 | 3篇 |
1979年 | 5篇 |
1977年 | 2篇 |
1965年 | 2篇 |
1964年 | 2篇 |
1957年 | 4篇 |
1954年 | 5篇 |
排序方式: 共有10000条查询结果,搜索用时 15 毫秒
991.
长江属于特大型河流、其河床纵向冲刷深度影响到穿、跨越长江工程的方案设计与施工方法确定,本文通过几个对长江南京河段河床纵向冲刷深度厘定结构的对比分析,剖析了这几种厘定方法的适应性,长江多年非汛期水下地形图测量结果,实际反映的是河道多年冲淤动态趋势,不能代表洪水期大洪水对河床的冲刷作用,这种冲刷深度不能正确反映其河床纵向冲刷深度;汛期实测的纵向冲刷深度,有时包含着深槽与浅滩相互转化过程的假象,不能依此为根据而定,相似性取值(即相似比尺)的影响,各家试验结果有所不同,再者。由于动床河工模型试验周期较长,对于时间紧迫的工程决策,往簇难以采用,而采用工程地质分析法确定河床纵向冲刷深度亦较适宜。 相似文献
992.
土钉与护坡桩综合结构在软土基坑支护中的应用 总被引:9,自引:0,他引:9
本文介绍了在软土地层中土钉护坡桩综合支护体系的设计与施工,实践证明,在软土深基坑支护设计中,应用综合支护体系,可以发挥各种支护体系的优点,弥补各种支护体系的不足,从而节省工程造价,缩短工期。 相似文献
993.
复杂地质构造波动方程数值模拟 总被引:3,自引:2,他引:3
利用全声波方程进行地震波场的数值模拟,虽然可以计算全声波波场值,但是也常常会出现层间多次波,给资料解释造成一定的困难。作者在本文中根据无反射声波方程,采用有限差分数值解法,实现了自激自收时间剖面的制作,避免了层间多次波的产生。本方法不但允许速度有纵向变化,而且允许速度有横向变化,这使得模拟复杂地质构造的地震响应成为可能。实际计算结果表明,该方法是一种行之有效的自激自收时间剖面的计算机数值模拟方法。 相似文献
994.
995.
YANG Jingsui XU Zhiqin SONG Shuguang ZHANG Jianxin WU Cailai SHI Rendeng LI Haibing Maurice BRUNEL Paul TAPPONNIER Institute of Geology Chinese Academy of Geological Science Baiwanzhuang Rd. Beijing China Department of Earth Sciences University of Montpellier II Montpellier France Institut de Physique du Globe Paris Cedex France 《《地质学报》英文版》2002,76(1):63-68
Coesite was discovered as inclusions in zircon separates from pelitic gneiss associated with a large eclogite body in the North Qaidam ultrahigh-pressure (UHP) terrane. Some graphite inclusions were also found. This finding suggested the occurrence of in-situ UHP metamorphism and that the terrane was most likely recrystallized at pressures below the diamond stability field. It supported other previous indirect UHP evidence, such as polycrystalline quartz inclusions in eclogitic garnet, quartz lamellae in omphacite and P-T estimates for both eclogite and garnet peridotite. The U-Pb and Sm-Nd ages of the North Qaidam eclogite indicated that subduction of continental crust occurred in the Early Palaeozoic, which probably recorded a collision between the Sino-Korean and Yangtze plates. 相似文献
996.
DONG Shuwen Chinese Academy of Geological Sciences Baiwanzhuang Ro Beijing WU Hongling LIU Xiaochun XUE Huaimin Institute of Geomechanics Chinese Academy of Geological Sciences Beijing Fei Zhenbi 《《地质学报》英文版》2002,76(1):69-80
Up to now it is known that almost all ultrahigh-pressure (UHP) metamorphism of non-impact origin occurred in continent-continent collisional orogenic belt, as has been evidenced by many outcrops in the eastern hemisphere. UHP metamorphic rocks are represented by coesite- and diamond-bearing eclogites and eclogite facies metamorphic rocks formed at 650-800℃ and 2.6-3.5 GPa, and most of the protoliths of UHP rocks are volcanic-sedimentary sequences of continental crust. From these it may be deduced that deep subduction of continental crust may have occurred. However, UHP rocks are exposed on the surface or occur near the surface now, which implies that they have been exhumed from great depths. The mechanism of deep subduction of continental crust and subsequent exhumation has been a hot topic of the research on continental dynamics, but there are divergent views. The focus of the dispute is how deep continental crust is subducted so that UHP rocks can be formed and what mechanism causes it to be subducte 相似文献
997.
A Report on a Biotite-Calcic Hornblende Geothermometer 总被引:1,自引:0,他引:1
WU Chunming PAN Yusheng WANG Kaiyi ZHANG Jian Institute of Geology Chinese Academy of Geological Sciences Beijing Institute of Geology Geophysics Chinese Academy of Sciences Beijing Department of Earth Sciences The Graduate School Chinese Academy of Sciences Beijing 《《地质学报》英文版》2002,76(1):126-131
This paper presents a biotite-calcic hornblende geothermometer which was empirically calibrated based on the gamet-biotite geothermometer and the gamet-plagioclase-hornblende-quartz geobarometer, in the ranges of 560-800℃ (T) and 0.26-1.4 GPa (P) using the data of metadolerite, amphibolite, metagabbro, and metapelite collected from the literature. Biotite was treated as symmetric Fe-Mg-AlVI-Ti quaternary solid solution, and calcic hornblende was simplified as symmetric Fe-Mg binary solid solution. The resulting thermometer may rebuild the input garnet-biotite temperatures well within an uncertainty of ±50℃. Errors of ±0.2 GPa for input pressure, along with analytical errors of ?% for the relevant mineral compositions, may lead to a random error of ±16℃ for this thermometer, so that the thermometer is almost independent of pressure estimates. The thermometer may clearly discriminate different rocks of lower amphibolite, upper amphibolite and granulite facies on a high confidence level. It is assume 相似文献
998.
Discovery of Radiolarian Fossils from the Aiketik Group at the Western End of the South Tianshan Mountains of Chinaand Its Implications 总被引:1,自引:0,他引:1
LI Yuejun WANG Zhaoming WU Haoruo HUANG Zhibin TAN Zejinand LUO Juncheng Institute of Geology Geophysics Chinese Academy of Sciences Beijing Tarim Oil Field Company PetroChin Korl Xinjiang Zhu Xiling 《《地质学报》英文版》2002,76(2):146-154
The Aiketik Group, distributed at the western end of the South Tianshan Mountains, China, is an important lithostratigraphic unit involved in the South Tianshan orogen. It is separated from the adjacent rocks by faults. Generally, the geologists ascribed it to the Upper Carboniferous according to Pseudostaffella sp., Profusulinella sp. and Fusulinella sp. found from the limestone and sandy limestone of Aiketik. Our radiolarian fossils were obtained from the chert samples collected from the Haladaok section located at the upper Tuoshihan River. The fossils mainly include Albaillella undulata Deflandre, Albaillella paradoxa Deflandre, Albaillella sp. aff. A. paradoxa Deflandre, Albaillella sp. cf. A. deflandrei Gourmelon, Albaillella sp., Albaillella excelsa Ishiga, Kito and Imoto (?), Belowea variabilis (Ormiston et Lane), Callella cf. C. parvispinosa Won, Entactinia cf. E. tortispina Ormiston et Lane, Entactinia aff. E. tortispina Ormiston et Lane, Entactinia variospina Won, Entactinia sp., Eostylodicty 相似文献
999.
1000.
塔河油田下奥陶统碳酸盐岩储层对比及储层剖面模型 总被引:5,自引:2,他引:5
塔河油田奥陶系储层为岩溶缝洞型的碳酸盐岩储层,缝洞储层的形成与古岩溶作用密切相关,风化壳期岩溶作用对储集空间的发育程度有明显的控制作用。不同的储集空间类型受控于不同的岩溶古地貌单元。裂缝性储层主要分布于风化壳型岩溶不发育地区,或褶皱和断裂构造较发育的变化强烈部位;裂缝-孔洞型储层的分布与古岩溶发育带和岩溶斜坡地区密切相关;裂缝-溶洞型储层其分布与裂缝及古岩溶发育带密切相关,常常是在古岩溶高地边缘或部分岩溶斜坡区,多位于多组构造线的交汇处及褶皱的轴部等。为进一步探讨研究区缝洞型碳酸盐岩储层的空间展布规律,根据暴露区淡水岩溶作用发育特点,依据碳酸盐岩储层的波阻抗响应特征、测井曲线、测试成果及开发动态资料,在恢复古岩溶地貌的基础上,对塔河油田(6区)的岩溶值得层进行了划分与对比。研究结果显示高产井多位于古岩溶地貌相对较高部位,而产量较少或没有出油气的井,则位于岩溶地貌相对较低部位。表明早期的古地貌形态对奥陶系碳酸盐岩溶蚀孔洞的发育具有明显的控制作用。岩溶储层的垂向发育和分布主要受碳酸盐岩古岩溶风化壳垂向分带性的影响,纵向上由风化壳顶面向下储层发育逐渐变差。以奥陶系古风化壳顶面为界,向下每60m为单位,对深度0-60m、60-120m、120-180m、180-240m岩溶储层的纵横向分布特征进行了分析,并建立了相应的储层剖面结构模型。 相似文献