全文获取类型
收费全文 | 334篇 |
免费 | 63篇 |
国内免费 | 150篇 |
专业分类
测绘学 | 3篇 |
大气科学 | 11篇 |
地球物理 | 47篇 |
地质学 | 420篇 |
海洋学 | 32篇 |
天文学 | 2篇 |
综合类 | 18篇 |
自然地理 | 14篇 |
出版年
2024年 | 2篇 |
2023年 | 11篇 |
2022年 | 8篇 |
2021年 | 19篇 |
2020年 | 19篇 |
2019年 | 23篇 |
2018年 | 22篇 |
2017年 | 14篇 |
2016年 | 18篇 |
2015年 | 22篇 |
2014年 | 18篇 |
2013年 | 29篇 |
2012年 | 33篇 |
2011年 | 22篇 |
2010年 | 14篇 |
2009年 | 30篇 |
2008年 | 15篇 |
2007年 | 24篇 |
2006年 | 30篇 |
2005年 | 18篇 |
2004年 | 37篇 |
2003年 | 25篇 |
2002年 | 14篇 |
2001年 | 23篇 |
2000年 | 16篇 |
1999年 | 10篇 |
1998年 | 8篇 |
1997年 | 9篇 |
1996年 | 4篇 |
1994年 | 2篇 |
1993年 | 1篇 |
1992年 | 2篇 |
1989年 | 1篇 |
1988年 | 1篇 |
1987年 | 2篇 |
1982年 | 1篇 |
排序方式: 共有547条查询结果,搜索用时 15 毫秒
471.
Leticia Chiglino Claudio Gaucher Alcides N. Sial Jorge Bossi Valderez P. Ferreira Márcio M. Pimentel 《Precambrian Research》2010
Increasing evidence shows that Mesoproterozoic rocks are widespread in the Río de la Plata Craton. Carbon and strontium isotope analyses were carried out for three different, carbonate-bearing successions in the southern Nico Pérez Terrane. The Parque UTE Group is erected, comprising (from base to top) the mainly volcanogenic Cañada Espinillo Formation, the dolomitic Mina Valencia Formation and the mixed carbonate-siliciclastic Cerro del Mástil Formation. A δ13C curve was obtained for carbonates of the Parque UTE Group, which is characterized by a plateau at +1 to +1.6‰ V-PDB, bracketed between two negative excursions (−1.8‰ V-PDB at the base and −3.3‰ V-PDB at the top). These values are consistent with a Mesoproterozoic depositional age for the unit, as indicated by U–Pb ages of synsedimentary volcanics and gabbros of 1429 ± 21 and 1492 ± 4 Ma, respectively. 相似文献
472.
Neoproterozoic Mafic Dykes and Basalts in the Southern Margin of Tarim, Northwest China: Age, Geochemistry and Geodynamic Implications 总被引:4,自引:0,他引:4
<正>Neoproterozoic rifting-related mafic igneous rocks are widely distributed both in the northern and southern margins of the Tarim Block,NW China.Here we report the geochronology and systematic whole-rock geochemistry of the Neoproterozoic mafic dykes and basalts along the southern margin of Tarim.Our zircon U-Pb age,in combination with stratigraphic constraint on their emplacement ages,indicates that the mafic dykes were crystallized at ca.802 Ma,and the basalt, possibly coeval with the ca.740 Ma volcanic rocks in Quruqtagh in the northern margin of Tarim. Elemental and Nd isotope geochemistry of the mafic dykes and basalts suggest that their primitive magma was derived from asthenospheric mantle(OIB-like) and lithospheric mantle respectively,with variable assimilation of crustal materials.Integrating the data supplied in the present study and that reported previously in the northern margin of Tarim,we recognize two types of mantle sources of the Neoproterozoic mafic igneous rocks in Tarim,namely the matasomatized subcontinental lithospheric mantle(SCLM) in the northern margin and the long-term enriched lithospheric mantle and asthenospheric mantle in the southern margin.A comprehensive synthesis of the Neoproterozoic igneous rocks throughout the Tarim Block led to the recognition of two major episodes of Neoproterozoic igneous activities at ca.820-800 Ma and ca.780-740 Ma,respectively.These two episodes of igneous activities were concurrent with those in many other Rodinian continents and were most likely related to mantle plume activities during the break-up of the Rodinia. 相似文献
473.
474.
大气分层扰动位能控制方程及其应用——南海夏季风活动的能量收支 总被引:1,自引:1,他引:0
针对局地环流能量转换问题,本文推导了分层扰动位能一阶矩 (LPPE1) 和动能 (KE) 的控制方程,分析了方程中各能量项的空间分布和季节变化特征,并以南海夏季风为例,诊断了夏季风活动各相位的能量收支特征.结果表明,850 hPa高度上在赤道辐合带、大部分季风区、风暴轴地区是LPPE1的源区,副热带的大洋东部和高纬度地区是LPPE1的汇区,强源、汇的中心与LPPE1的纬向偏差场的脊、槽分布对应较好.LPPE1向KE的转化项 (CK)取决于垂直速度和大气稳定度,是连接KE和LPPE1的纽带,在暖 (冷) 空气上升 (下沉) 时,转化项为正,LPPE1向KE转化能量,反之KE转化为LPPE1.在850 hPa 高度上CK的分布特征是在赤道辐合带以及大部分季风区有大值分布,北半球风暴轴和南半球西风带有连续分布的正值区.将这应用到南海夏季风活动的能量收支,在南海夏季风恢复相位,CK增大,在南海夏季风活跃相位,CK达到最大,且为边界输入能量的2~3倍,CK是南海夏季风恢复、活跃的最重要因素.探讨了南海夏季风活跃的条件,当LPPE1等于南海季风区的夏季气候平均值时,上升速度大于临界速度的情形,有利于南海夏季风由中断相位向活跃相位的转变. 相似文献
475.
深水环境多级地貌坡折控制下的重力流动力学的演变 总被引:4,自引:0,他引:4
台湾浅滩陆坡具有活跃的重力流机制,发育了壮观的重力流沉积体系,是研究重力流动力学作用过程的理想场所。自陆架前缘直至深海的马尼拉海沟,发育了三个地貌坡折(包括一个陆架坡折和两个陆坡坡折)。这些地貌坡折控制了重力(流)的启动和整个演化过程,控制了各种重力流沉积体系的空间分布格局。其中陆架坡折控制了重力滑塌的产生,第一和第二陆坡坡折则分别控制了重力滑塌体、碎屑流、浊流的转换。论文利用重力流沉积物波的波形参数恢复了重力流流体有关参数,实证了研究区的确存在有非常活跃的重力流机制。而多级地貌坡折代表着陆坡地貌的不均衡和向均衡的演化,重力流的侵蚀-沉积效应只是陆坡体系调整过程的表现。 相似文献
476.
We present hornblende, white mica, biotite and alkali feldspar 40Ar/39Ar data from Paleo-Mesoproterozoic rocks of the Mt. Isa Inlier, Australia, which reveal a previously unrecognised post-orogenic, non-linear cooling history of part of the Northern Australian Craton. Plateau and total fusion 40Ar/39Ar ages range between 1500 and 767 Ma and record increases in regional cooling rates of up to 4 °C/Ma during 1440–1390 and 1260–1000 Ma. Forward modelling of the alkali feldspar 40Ar/39Ar Arrhenius parameters reveals subsequent increases in cooling rates during 600–400 Ma. The cooling episodes were driven by both erosional exhumation at average rates of 0.25 km/Ma and thermal relaxation following crustal heating and magmatic events. Early Mesoproterozoic cooling is synchronous with exhumation and shearing in the Arunta Block and Gawler Craton. Late Mesoproterozoic cooling could have either been driven by increased rates of exhumation, or a result of thermal relaxation following a heat pulse that was synchronous with dyke emplacement in the Arunta, Musgrave and Mt. Isa province, as well as Grenville-aged orogenesis in the Albany–Fraser Belt. Latest Neoproterozoic–Cambrian cooling and exhumation was probably driven by the convergence of part of the East Antarctic Shield with the Musgrave Block and Western Australia (Petermann Ranges Orogeny), as well as collisional tectonics that produced the Delamerian–Ross Orogen. Major changes in the stress field and geothermal gradients of the Australian plate that are synchronous with the assembly and break-up of parts of Rodinia and Gondwana resulted in shearing and repeated brittle reactivation of the Mt. Isa Inlier, probably via the displacement of long-lived basement faults within the Northern Australian Craton. 相似文献
477.
478.
479.
480.