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121.
Deep-well injection has been used to dispose of municipal liquid wastes in southwestern Florida since 1988. The liquid wastes
are injected into an extremely high-transmissivity zone of fractured dolomite in the Early Eocene Oldsmar Formation of the
Floridan aquifer system; this zone is commonly referred to as the Boulder Zone. Data collected during the drilling and operational
testing of southwestern Florida injection wells provide insights into the nature of the injection zone and overlying confining
beds. The location of high-transmissivity zones that are capable of accepting large quantities of waste water is vertically
and horizontally variable and cannot be predicted with certainty. A 40.9-m thick high-permeability interval in one injection
well, for example, was absent in a well drilled only 85.4 m away. Some upward migration of low-density injected fluids has
occurred, but at no site were the injected liquids detected in deep monitor wells, such as occurred at injection-well sites
along the coasts of southeastern, west-central, and east-central Florida. The primary confinement of the injected liquids
(i.e., deepest effective confining beds) consists of unfractured beds of low-permeability dolomite within the Oldsmar Formation,
whose locations are also laterally and vertically variable. The origin and controls of the distribution of fractures in the
Oldsmar Formation are poorly understood.
Received, December 1997 Revised, June 1998, August 1998 Accepted, August 1998 相似文献
122.
Tang Zhongli Gansu Bureau of Geology Mineral Resource Lanzhou Gansu Fei Zhenbi 《《地质学报》英文版》1997,71(1):49-57
Before intruding, primary magmas have undergone liquation and partial crystallization atdepth; as a result the magmas are partitioned into barren magma, ore-bearing magma, ore-richmagma and ore magma, which then ascend and are injected into the present locations once ormultiple times, thus forming ore deposits. The above-mentioned mineralizing process is knownas deep-seated magmatic liquation-injection mineralization. The volume of the barren magma isgenerally much larger than those of the ore-bearing magma, ore-rich magma and ore magma. Inthe ascending process, most of the barren magma intrudes into different locations or outpoursonto the ground surface, forming intrusions or lava flows. The rest barren magma, ore-bearingmagma, ore-rich magma and ore magma may either multiple times inject into the same space inwhich rocks and ores are formed or separately inject into different spaces in which rocks and oresare formed. The intrusions containing such deep-seated magmatic liquation-injection depositshave a much smaller volume, greater ore potential and higher ore grade than that of in-situmagmatic liquation deposits. Consequently this mineralizing process results in the formation oflarge deposits in small intrusions. 相似文献
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126.
Ground tilt measurements demonstrate that Askja is in a state of unrest, and that in the period 1988–1991 a maximum 48±3 rad tilt occurred down towards the centre of the caldera. This is consistent with 126 mm of deflation at the centre of the caldera with a 2.5–3.0 km depth to the source of deformation. The volume of the subsidence bowl is 6.2x106 m3. When combined with high precision microgravity measurements, the overall change in sub-surface mass may be quantified. After correction for the observed elevation change using the free air gradient of gravity measured for each station, the total decrease in mass is estimated to be less than 109 kg. A small residual ground inflation and net gravity increase in the southeastern part of the caldera may be caused by dyke intrusion in this region. The minimum dimensions of such an intrusion or complex of intrusions are 1 m width, up to 100 m deep and up to several hundred metres thick. 相似文献
127.
头台油田是构造—岩性油藏。裂缝型、特低渗透是其显著特点,常规注水开发后经常出现严重的油井水淹,造成油田开发低效。本文以头台油田研究为例,认为对于裂缝型特低渗透油田,采用注水吞吐采油技术,通过套管直接向地层注水,利用储层毛管力作用,进行油水置换,实现单井自注自采吞吐采油,可以改善油田开发效果,减缓产量递减。适合注水吞吐采油基本条件是岩石润湿性为弱亲水和岩石饱和非润湿相。影响注水吞吐采油效果的主要因素是储层吸水状况、微缝发育状况、储层非均质性、注入体积和关井压力等。吞吐采油技术可作为改善裂缝型特低渗透油藏开发效果的一种新的模式来研究和推广。 相似文献
128.
大型化综放开采煤层注水方案及参数确定 总被引:3,自引:0,他引:3
强调在大型化综放开采煤层中开设抬高中间巷进行煤层注水,其注水效率高,可一巷多用,防灾效果全面。结合算例,用有限元数值模拟方法模拟了在厚煤层中注水的过程,得到最小湿润范围准则为煤层厚度的1.5倍。分析了综放开采煤层注水工艺参数中注水压力、时间和钻孔间距与湿润范围的动态变化关系,给出了选取合理的注水工艺参数的方法。指出在大型化综放开采进行煤层注水,湿润时间充裕,同时,考虑到压裂并软化煤体,应采用较高的压力注水,此时,钻孔间距可扩大至35m。 相似文献
129.
分析了影响钻孔灌注桩成桩质量的桩孔超径、泥浆性能、桩头出现的杂质砼、砼的可灌性等因素,同时提出了解决问题的办法,且从砼的配制到灌注均提出了具体看法,供讨论。 相似文献
130.