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991.
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993.
以淀粉为主要原料,合成了新型多羟基糖苷防塌剂DTG-1。对合成样品的理化性能、页岩抑制作用、水溶液活度、生物毒性以及对泥页岩半透膜膜效率的影响规律进行了测定,考察了DTG-1在淡水、盐水和饱和盐水钻井液中对钻井液流变性能和滤失造壁性能的影响,并对DTG-1稳定井壁及改善钻井液流型的作用机理进行了分析。研究表明,用淀粉合成的多羟基糖苷,具有一定的抑制泥页岩水化膨胀、分散和提高泥页岩的膜效率的作用,能有效降低钻井液的水活度,属于无毒、环保型钻井液处理剂;DTG-1对高密度钻井液具有很好的流型改善作用,用DTG-1配制的钻井液具有组成简单、流变性易调整、高温稳定性好、抗污染性强等特点。 相似文献
994.
沂水龙泉站金矿与成矿有关的主要地质体以新太古代泰山岩群与燕山期花岗岩金含量较高。对黄铁矿地球化学的研究资料表明:早期黄铁矿为金矿物的主载矿物。稀土元素分布特征反映了成矿流体由早期相对中偏高温(260~330℃)和还原的环境向晚期低温和氧化环境演变的趋势。对方解石、石英包裹体的研究表明:包裹体均一温度变化范围较宽,在107~550℃之间,可分为125~160℃,177~230℃和260~330℃3个温度峰值集中区,分别反映了以中温石英为代表的早期成矿阶段(260~330℃),以中低温石英和方解石为代表的中期成矿阶段(177~260℃)和以低温方解石为代表的晚期成矿阶段(125~160℃)。其冰点温度变化于-2~-8.6℃之间,盐度在3.39wt%~12.39wt%之间。 相似文献
995.
Research on experiment and calculation of foam bursting device 总被引:1,自引:0,他引:1
Hazaea Mohammed Youhong SUN Ould El HousseinYarbana Longxiang XU Al-Aswar Fahmi 《世界地质(英文版)》2007,10(1)
This research presents experimental data on mechanical foam bursting device, based on the high speed of air fluid impinging insidethe foam bursting device, foam bubbles disrupted as a consequence of pressures changed very quickly as shear force and their impact forces. Experimental data on foam-bursting capacity have been presented. Designed device can provide effective foam bursting on collapse foam. 相似文献
996.
会泽铅锌矿床成矿作用受构造控制明显,主要与压扭性断裂作用有关.H、O、C、S、Pb同位素和包裹体资料、断裂构造地球化学和矿床地球化学分析表明,矿床形成于持续开放体系条件,并且持续开放体系下的(断裂)构造作用控制了矿床成矿元素的活化迁移与含矿流体的形成、流体的迁移汇聚及矿液的沉淀与矿床的定位.持续开放体系下的构造(断裂)作用对矿床的形成起了决定性作用. 相似文献
997.
T. M. Boundy C. L. Donohue E. J. Essene K. Mezger H. Austrheim 《Journal of Metamorphic Geology》2002,20(7):649-667
Eclogite facies carbonate rocks have been discovered associated with the granulite–eclogite transitional rocks within Bergen Arc system, Caledonian Orogen of western Norway. The local occurrences of marbles and calc‐silicates are found subparallel to the mafic eclogite facies shear zones on Holsnøy Island. Marbles contain the assemblage calcite (Ca0.99Sr0.01CO3), calcian strontianite (Ca0.18?0.44Sr0.53?0.84CO3), clinopyroxene (Jd7?32), epidote/allanite (Ps0?33), titanite, garnet (Alm52?56Grs28?33Pyp11?16), barite (Ba0.90?0.99Sr0.01?0.10SO4), celestine (Sr0.67?0.98Ba0.01?0.23Ca0.01?0.11SO4), and one apparently homogeneous grain of intermediate composition (Ba0.49Ca0.01Sr0.50SO4). Adjacent eclogites have clinopyroxene with similar jadeite contents (Jd14?34) and similar garnet (Alm51?60Grs26?36Pyp8?14) compositions. The marbles have high contents of Sr (9500–11000 p.p.m) and Y (115–130 p.p.m). However, low concentrations of some key trace elements (110–160 p.p.m. Ba and <5 p.p.m. Nb) appear to indicate that the marble is not a metamorphosed carbonatite. The 87Sr/86Sr ratios range from 0.7051 to 0.7059. Field and petrological relationships suggest that metasomatic reactions and fluids played a significant role in producing and/or modifying the marbles. The breakdown of scapolite in the granulite into carbonates and sulphates during eclogite facies metamorphism may have contributed to the metasomatic formation of the marbles along shear zones. Fluids involved during subduction are an important catalyst for metamorphism and are recognized to have played a critical role in the localized transformation from granulite to eclogite in the Holsnøy Island area. Thermobarometry indicates 640–690 °C and 18–20 kbar for adjacent eclogites and temperatures of 580–650 °C for the calc‐silicates. The marble assemblages are consistent with fluid that is dominantly comprised of H2O (XCO2 < 0.03) under high‐pressure conditions. Phase equilibria of the marbles constrain the fO2 of the fluids and imply oxidizing conditions of the deep crustal fluids. At present the source of the fluids remains unresolved. The results provide additional insights into the variable and evolving nature of fluids related to subduction and high‐pressure metamorphism. 相似文献
998.
Laboratory experiments are described which provide insight into the interaction of intermediate depth boundary currents (IDBCs) with interrupted sloping topography. Specifically, they contribute to the debate over meddy formation on the Iberian continental slope. The experiments were performed in a rectilinear rotating tank filled initially with a linearly-stratified fluid. A false bottom sloped away from the side-wall along which the current flowed, and was interrupted by a gap of variable length. The effects of varying gap length and rotation rate on the boundary current were observed.In the first of two sets of experiments, the current flowed above the slope, along the vertical sidewall. In the second, the current flowed along the sloping bottom. In the former, current nose speed was consistent with geostrophic predictions, but decreased in the presence of a gap in the topography. Kelvin wave radiation is postulated as a reason for this. The IDBCs exhibited vortical lateral intrusions at values of the Burger number Bu=(N0/Ω)2 at which counterpart flat-bottom studies had been stable, implying that the sloping topography had a de-stabilising effect. Energy measurements and qualitative observations suggest the intrusions were due to mixed barotropic/baroclinic instabilities, the latter dominating at higher rotation rates.In the second configuration, four distinct flows were observed, distinguished by the deformation radius:gap width ratio RD/G*. For a range of values of RD/G*, attached eddies formed at the upstream end of the gap. They remained at this position, unlike those in similar studies of surface boundary currents (Klinger, 1993). Their persistence and ability to move downstream – salient factors for meddy – formation were greater for a finite gap size than a permanent change from sloping to flat bottom. 相似文献
999.
古代与现代火山成因块状硫化物矿床研究进展 总被引:8,自引:1,他引:8
火山成因块状硫化物(VolcanogenicMas siveSulfide,简称VMS)矿床可见于前寒武纪至现代的各个地质时代。现代海底热液成矿作用为研究VMS矿床提供了一种新的途径,DSDP/ODP钻探资料揭示:①VMS矿床虽然可产生于不同环境,但均与张裂断陷有关。②成矿物质可能来源有 2种:一种是含矿火山岩系及下伏基底物质的淋滤;另一种是深部岩浆房挥发份的直接释放。③洋中脊海底热液循环呈双扩散对流模式。在有沉积物覆盖的洋中脊,热液循环更多地考虑流体与沉积物相互作用产生的效果。④从矿物组合的空间分布来看,热液硫化物堆积体上部以烟囱体为主,下部以块状硫化物为主,深部以网脉状硫化物为主,这在不同热液活动区似乎具有普遍性。
VMS矿床的矿化模式反映的是一种热液成因,这种热液是深部(1~3 km)岩浆侵入所引起并通过海水在热穹隆之上循环产生的。VMS矿床的深入研究要求我们致力于发现新的矿产地,提高样品采集、分析技术,加强海底热液活动与构造、岩浆作用和环境演变的一体化研究。 相似文献
VMS矿床的矿化模式反映的是一种热液成因,这种热液是深部(1~3 km)岩浆侵入所引起并通过海水在热穹隆之上循环产生的。VMS矿床的深入研究要求我们致力于发现新的矿产地,提高样品采集、分析技术,加强海底热液活动与构造、岩浆作用和环境演变的一体化研究。 相似文献
1000.