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71.
南京汤山洞穴石笋稳定同位素指示的气候与环境意义 总被引:16,自引:1,他引:15
对南京汤山葫芦洞南壁钙板上一支长82mm石笋进行了高精度热电离质谱(TIMS)定年及氧碳同位素分析。结果表明,该支短石笋生长时段长达300ka左或(距今463~159ka),其底部年龄进一步证实南京直立人生存时代早于450kaBP。δ^13C值在MIS6/7界线上的显著漂移揭示了一次土壤侵蚀事件,结束了洞穴文化层的堆积历史。 相似文献
72.
LONG Shengxiang WANG ChuanResearch Institute of Petroleum Geology China National StarPetroleum Corporation CNSPC Xueyuan R Beijing LI Yuzhan Exploration Department CNSPC Xueyuan R Beijing 《《地质学报》英文版》2000,74(3):666-673
The gas resources assessment expert system is one of the advanced methods for appraising oil and gas resources. The establishment of a knowledge base is the focal task in developing the expert system. This paper presents a summary of the mechanism and the major controlling factors in the formation of gas pools in the southeast uplift of the Songliao basin. Then an appropriate assessment model is established for trapping the gas resources and a knowledge base built in the expert system to realize the model. By using the expert system to appraise the gas-bearing probability of 25 major traps of the Quantou and Denglouku Formations in the Shiwu-Dehui area, the authors have proved that the expert system is suitable for appraising traps in the Songliao basin and similar basins. 相似文献
73.
Calcite and quartz veins in the gabbroic and dunite rocks of the Semial ophiolite (UAE) were selected for fluid inclusion analysis. The inclusions contain both aqueous low-salinity and hydrocarbon-dominated fluids. Mi-crothermometry data indicate that the aqueous fluids contain 0.22 to 1.45 equivalent wt% NaCl and occasionally contain traces of hydrocarbons. Homogenization to liquid occurred between 91 and 152℃. Modeling based on these fluid inclusion observations indicates that the trapping conditions of t... 相似文献
74.
本文对小质量X射线双星的准周期振荡的差频模型做了修正和补充。修正的要点是:要考虑柱吸积过程中的粘滞阻尼。由此即可成功地解释QPO天体GX5-1的双分支谱特性。 相似文献
75.
76.
Ronald STEEL 《《地质学报》英文版》2009,83(1)
In recent years,with the development of terrestrial sequence stratigraphy,more attention has been focused on the study of the terrestrial lacustrine sequence stratigraphic model globally. Different viewpoints are preferred by researchers.Under the guidance of the theory of sequence stratigraphy,the findings of this paper indicate that climate is a major factor controlling the formation of the fourth-order sequence,based upon the study of the sequence stratigraphy in the Green River Formation of the Uinta... 相似文献
77.
通过研究库车地区的地震活动性 ,由地震分布的规律性推断可能的基底断裂 ,并分析了基底活动断裂与地表构造的对应关系、盖层变形和基底变形特征的差异及成因。结果表明 :1)地震震中分布揭示库车坳陷内对应东、西秋里塔格背斜带位置上 ,基底中发育东秋里塔格深断裂和南、北秋里塔格深断裂 ;另外 ,依奇克里克背斜和亚肯背斜位置上也存在对应的深断裂 ,这表明地表构造的形成受深部构造的控制。 2 )依奇克里克构造西端至东秋 5井连线位置上发育 1条NE向走滑断裂 ,在拜城西侧发 1条NW走向的活动断裂 ,这 2条切穿构造走向的活动断裂是库车坳陷构造分段的主因。 3)基底和盖层变形特征的差异主要源于二者之间介质特性的差异。盆地基底岩石圈强度非常高 ,决定了其变形以脆性破裂———地震活动为主 ;而盖层中沉积岩层强度较弱 ,且存在煤和膏盐等极软弱的薄层 ,在构造挤压作用下 ,可以产生黏性或塑性流动大变形及顺层无震滑脱 相似文献
78.
澜沧江断裂带的新生代走滑运动学特点 总被引:10,自引:1,他引:9
通过对澜沧江断裂带北、中、南段新生代构造形迹的运动学解析,结合前人工作,论证了澜沧江断裂在新生代早期(古新世-中始新世末)、中期(晚始新世-渐新世末)、晚期(中新世-第四纪)的走滑运动序列为:中、南段,右行→左行→右行;北段,左行→左行→右行。研究表明,澜沧江断裂带早期主要表现为中、南段的右行逆冲和北段的左行逆冲,与同期发生的昌都-思茅地体颈缩事件相对应,其地球动力学背景与太平洋板块向西推挤作用以及扬子-华南板块与印度板块发生的强烈东西向碰撞挤压有关;中期,整个断裂发生左行逆冲,其地球动力学背景与南海盆地的扩张作用及其扬子-华南板块相对于印度板块北移所致的左行扭动相适应:晚期,整个断裂右行走滑,与太平洋构造域的南海盆地扩张终止,昌都思茅地体整体向南东逃逸相适应。 相似文献
79.
Erosion, sediment transportation and accumulation in rivers 总被引:8,自引:5,他引:3
N. I. ALEKSEEVSKIY K. M. BERKOVICH and R. S. CHALOV Prof. Head of the Hydrology Department Faculty of Geography Moscow State University Moscow Russia Prof. Leading researcher Lab. of Soil Erosion Fluvial Processes Faculty of Geography Moscow State University Moscow Russia Prof. Head of the Lab. of Soil Erosion Fluvial Processes Faculty of Geography Moscow State University Moscow Russia 《国际泥沙研究》2008,23(2):93-105
The present paper analyses the interrelation between erosion, sediment transportation and accumulation proposed by N. I. Makkaveyev (1908-1983) and its further development in modem studies of river channel processes in Russia. Spatio-temporal linkages between erosion and accumulation are defined considering channel processes at different scales - river longitudinal profile, channel morphological patterns, alluvial bedforms (bars, dunes) and individual sediment particles. Relations between river geomorphic activity, flow transportation capacity and sediment budgets are established (sediment input and output; channel bed erosion and sediment entrainment into flow - termination of sediment transport and its deposition). Channel planforms, floodplain segments separated by the latter and alluvial channel bedforms are shown to be geomorphic expressions of sediment transport process at different spatial and temporal scales. This paper is dedicated to the 100th anniversary of N. I. Makkaveyev, Professor of the Moscow State University, author of the book "River channel and erosion in its basin" (1955). That book is regarded in Russia as the pioneering work which initiated the complex hydrological and geographical studies of channel processes and laid a basis for the theory of unified fluvial erosion-accumulation process. 相似文献
80.
WANG Nianxiang GU Lei
Senior Engineer Geotechnical Engineering Department Nanjing Hydraulic Research Institute Nanjing P. R. China.
Engineer Plan Statistics 《中国海洋工程》1999,(2)
-According to the Mohr-Coulomb yield criterion,the stress field of the infinite slope is derivedunder a vertical uniform load q on the top of the slope.It is indicated that elastic and elasto-plastic stateswould occur in the slope.When q is smaller than the critical load,q_p,the slope is in the elastic state.Ifq equals q_p,the slope is in the critical state,and the plastic deformation would occur along the critical an-gle.With the increase of q,the plastic zone would extend,and the slope is in the elasto-plastic state.Ifq equals limit load,the slope is in the limit equilibrium state.The slope may be divided into three zones.Some charts of the critical angle,the critical and limit load coefficients are presented in this paper. 相似文献