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151.
152.
金银丰度的高低不是控制金银矿化的决定性因素。有利于金矿化的因素包括:较高的金银丰度;全银的几何平均值与算术平均值比较;金分布及银分布均为多峰偏态,对数分布为正态-正偏;易释放金比例高;地层中金银形成的元素组合同区域金银矿床的矿化元素组合接近。 相似文献
153.
N. P. Sukumaran 《Journal of Earth System Science》1994,103(4):489-497
Examined in this paper is the tentative history of the depositional flux of230Thxs (the unsupported fraction of230Th scavenged from the overlying water column), for the Late Quaternary period from a sediment core of the Central Indian Basin
(CIB). The measured depositional flux of230Thxs is found substantially higher than that of the possible theoretical flux from the overlying water column. Historical records,
reconstructed from the230Thxs chronology suggests that the depositional flux has varied considerably with time, reflecting an enhanced scavenging during
the Holocene and the preceding interglacial periods whereas, comparatively lower flux than the predicted one occurred during
the Last Glacial Maximum (LGM) period. The average ratio of the measured depositional flux to that of the predicted flux from
the overlying water column, indicates that the core site acts as a sink for230Thxs and based on the existence of bottom current activity; the230Thxs could be the result of focusing of younger sediments. The depositional index (Di) has also been calculated to quantify the
extent of lateral supply throughout the core with time. The estimated (Di) suggests that bottom focusing and feeble deposition
and/or winnowing processes had occurred and that the former was most prevalent during the Holocene and the preceding interglacials,
whereas the latter was observed at the LGM period. 相似文献
154.
P. R. Sheorey 《Geotechnical and Geological Engineering》1984,2(2):133-140
Summary Indian coal measures have widely varying caving characteristics. The maximum roof span of a longwall or depillaring panel at the time of nether roof collapse is shown to have a direct relation withRQD from a study of 12 case histories. A similar relation between maximum unsupported span of openings and rock mass quality as defined by theQ-system was also demonstrated. A simple nomogram is presented to predict the face advance required to cause roof collapse when theRQD or rock mass quality is known. 相似文献
155.
Roof bolting in underground mining: a state-of-the-art review 总被引:1,自引:1,他引:1
Conclusions With continuing investigations and developments, roof bolting today can in most cases successfully reinforce the mine roof in underground mining. In order to cope with the increasing use of roof bolts, efforts should be made to maximize the safety and minimize the cost. With regard to mechanical bolting, two important parameters need more advanced improvements and study, namely, optimum design of the shape and type of expansion shell and optimum bolt tension for a specific bolt pattern. For the fully grouted resin bolt, the most critical requirement is to develop a fast-setting, low-cost, intoxic, inflammable grouting material that can be used in the high speed mining cycle. It should be noted that geological conditions such as the strata type, rock properties,in situ stress, and planes of weakness play an important role in the successful application of any roof bolting system. These factors should be specified as accurately and quantitatively as possible in the design of any roof bolting system. Finally, proper and careful installation and continuous monitoring are imperative for the success of any roof bolting system. 相似文献
156.
碳同位素与早元古代地层对比 总被引:2,自引:0,他引:2
本文首次较详细地研究了早元古代碳酸盐地层的碳同位素组成,样品采自华北早元古代标准地层单元──山西五台地区滹沱群,结果表明碳同位素组成随地质时代有明显的变化,并与地层层位有很好的对应关系。作者认为,碳同位素对于早元古代碳酸盐地层的对比是很有用的。 相似文献
157.
松辽分水岭东段白土山组成因与时代 总被引:3,自引:1,他引:3
综合考虑松辽分水岭东段地区白土山组的地层分布、沉积特征、地貌部位及第四纪以来松辽分水岭的演化过程、松辽水系的变迁,认为其为河流冲积物,形成时代为早更新世早期。 相似文献
158.
A. H. Wilson 《Geotechnical and Geological Engineering》1983,1(2):91-187
Summary The characteristics of soft rocks typical of the British Coal Measures are defined and a series of working hypotheses are developed to provide improved design methods for underground roadway and face supports and pillars in coal mines. Proposed design equations are tested against case history data. 相似文献
159.
J.M. Grove 《Climatic change》2001,48(1):53-82
The "Little Ice Age" was the most recent period during which glaciers extended globally, their fronts oscillating about advanced positions. It is frequently taken as having started in the sixteenth or seventeenth century and ending somewhere between 1850 and 1890, but Porter (1981) pointed out that the "Little Ice Age" may 'have begun at least three centuries earlier in the North Atlantic region than is generally inferred'. The glacial fluctuations of the last millennium have been traced in the greatest detail in the Swiss Alps, where the "Little Ice Age" is now seen as starting with advances in the thirteenth century, and reaching an initial culmination in the fourteenth century. In the discussion here, evidence from Canada, Greenland, Iceland, Spitsbergen and Scandinavia is compared with that from Switzerland. Such comparisons have been facilitated by improved methods of calibrating radiocarbon dates to calendar dates and by increasing availability of evidence revealed during the current retreat phase. It is concluded that the "Little Ice Age" was initiated before the early fourteenth century in regions surrounding the North Atlantic. 相似文献
160.
通过对位于东亚季风区中东部与西部边缘的两个高分辨率黄土剖面记录的对比研究,发现它们不仅捕捉到了20个Dansgaard Oeschger事件与6个Heinrich事件,而且黄土记录与GRIP冰芯记录的这些快速气候波动基本上是同步的。暗示在整个末次冰期,东亚季风气候同样存在千年—百年尺度上的快速波动。所不同的是,西面的沙沟剖面对这些快速气候波动的反应比东面的王官剖面敏感。结合末次冰期中国黄土记录的先前研究结果,我们发现,自西向东Dansgaard Oeschger旋回的幅度逐渐变小,推测这主要是由西风与东亚夏季风共同作用所造成的。 相似文献