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101.
Jihua?LiuEmail author Xuefa?Shi Lirong?Chen Yongyang?Huang Yinxi?Wang Yingchun?Cui Wenrui?Bu 《中国科学D辑(英文版)》2005,48(5):701-712
Clay fractions in the non-calcareous surface sediments from the eastern Pacific were analyzed for clay minerals, REE and 143Nd/144Nd. Montmorillonite/illite ratio (M/I ratio), total REE contents (ΣREE), LREE/HREE ratio and cerium anomaly (δCe) may effectively
indicate the genesis of clay minerals. Clay fractions with M/I ratio <1, δCe >0.85, ΣREE <400 μg/g, LREE/HREE ratio ≈4, and
REE patterns similar to those of pelagic sediments are terrigenous and autogenetic mixed clay fractions and contain more autogenetic
montmorillonite. Clay fractions with M/I ratio >1, δCe=0.86 to 1.5, ΣREE=200 to 350 μg/g, LREE/HREE ratio ≈6 and REE distribution
patterns similar to that of China loess are identified as terrigenous clay fraction. The 143Nd/144Nd ratios or ɛNd values of clay fractions inherit the features of terrigenous sources of clay minerals. Clay fractions are divided into 4
types according to ɛNd values. Terrigenous clay minerals of type I with the ɛNd values of ™8 to ™6 originate mainly from North American fluvial deposits. Those of type II with the ε Nd values of ™9 to
™7 are mainly from the East Asia and North American fluvial deposits. Those of type III with ε Nd values of ™6 to ™3 could
come from the central and eastern Pacific volcanic islands. Those of type IV with ε Nd values of ™13 to ™12 may be from East
Asia eolian. The terrigenous and autogenetic mixed clay fractions show patchy distributions, indicating that there are volcanic
or hot-spot activities in the eastern Pacific plate, while the terrigenous clay fractions cover a large part of the study
area, proving that the terrigenous clay minerals are dominant in the eastern Pacific. 相似文献
102.
1.地裂缝的基本特征1977年8月—9月西安辛家庙铁炉庙一带相继发现地裂缝。铁炉庙地裂缝位于市东南郊渭河三级阶地内黄土塬前缘洼地的北侧,东起铁炉庙,经后村、小寨、西到吉样村,断续延伸约6.5公里,尤以铁炉庙地段最为发育。其总体走向为北70°东,倾角70—90°(一般为76°)。由数十条地裂缝组成裂缝带,宽度为8—20米,一般在10米左右。地裂所经之处,建筑物多被裂开。 相似文献
103.
104.
New Nd and Sr isotope data are presented in this paper for sediments from the Yellow and Yangtze River drainage basins. The
average 143Nd/144Nd isotope compositions of fine-grained sediments from two drainage basins seem similar. The T
DMNd ages of sediments from the two drainage basins are relatively uniform but exhibit subtle differences. This reflects the different
underlying bedrocks, in association with the unique tectonic terranes that comprise central and southeastern China, including
the North China Block, the Yangtze Block, the South China Block, the Tibet Plateau and the Qinling-Dabie Orogenic Belt. In
contrast, there is an obvious difference in the 87Sr/86Sr ratios between fine-grained sediments of the Yellow and Yangtze Rivers, which actually reflects an increase in chemical
weathering intensity from northwestern to southeastern China. 相似文献
105.
大洋钻探与中国边缘海沉积地质学 总被引:3,自引:0,他引:3
边缘海沉积地质学研究在大洋钻探计划中占据着重要地位,也是我国的优势所在,应该成为我国ODP近期工作的主要内容。本文讨论了与ODP有关的几个中国边缘海沉积地质学问题:古黑潮的演变与陆海相互作用,长江、黄河入海时间及其对海洋沉积作用的影响,冲绳海槽的沉积相和沉积体系,古季风与海平面变化,这些问题的深入研究与解决将会为实现ODP的学术目标,为全球变化研究做出重要贡献。 相似文献
106.
107.
海峡是不同于三角洲、陆架的一类独特沉积环境,具有特殊的沉积作用组合。海峡的形态多样,长度为几千米至数百千米,深度为几十米至上千米; 海峡由狭窄区域向两端逐渐过渡为相对开阔海区,开阔海区大多深度相比海峡更深; 海峡的狭窄区域横截面积小、流体流速最大,通常以侵蚀地貌为特征; 流体流经狭窄区域后,由于海峡横截面积增加,导致流速向两端开阔海区域锐减,并表现为沉积地貌。浅水海峡通常以潮流为最主要的沉积作用,其他的沉积物搬运方式包括单向的海流和重力流; 深水海峡则以海流和重力流为主。海峡高能区沉积以砾石滞留和发育交错层理为特征,低能区表现为泥质沉积并发育流水砂纹; 在低海平面时期,暴露的浅水海峡以河流沉积作用为主; 海平面上升过程中,河流逐渐演化为三角洲/河口湾、海湾和贯通的海峡。 相似文献
108.
基于AMS 14C年龄和底栖有孔虫氧同位素建立的地层年代框架,重点探讨了冲绳海槽中北部CSHC-15孔MIS6期以来(约200 ka)底栖有孔虫δ13C特征及其古海洋指示意义。结果显示,冰期-间冰期表层初级生产力和有机质通量的变化是导致底栖有孔虫δ13C值在MIS4和MIS6期负偏而在MIS1、MIS3和MIS5期正偏的主要原因。MIS2期的底栖有孔虫δ13C正偏,指示了NPIW侵入冲绳海槽,导致通风性加强,底层水呈弱氧化状态。甲烷渗漏引发的甲烷厌氧氧化作用(AOM)是导致CSHC-15孔底栖有孔虫在MIS4期碳同位素大幅负偏的原因。 相似文献
109.
陆地生态系统研究通常未考虑影响整个岩石风化层--土壤剖面的生物地球化学过程,而关键带科学则强调从冠层到基岩重新认识整个生态系统的结构和功能,在流域尺度上应该强调大气和植物之间、植物和土壤之间、小流域土壤和溪流之间物质和元素循环的相互联系等。植物碳固定及分配、从地表到基岩的土壤碳库分解和转化以及小流域碳迁移与平衡是碳生物地球化学循环的起始、周转和迁移过程的关键环节,应该加强流域尺度上从冠层到基岩的生态系统碳循环过程、机制及其生态功能研究。同位素技术具有指示、示踪和整合功能,通过δ13C自然示踪和人工标记技术,可以辅助解析碳生物地球化学过程与机制。 相似文献
110.
Xin Shan Xuefa Shi Peter D. Clift Shuqing Qiao Lina Jin Jianxing Liu Xisheng Fang Taoyu Xu Shunli Li Selvaraj Kandasamy Mengwei Zhao Ying Zhu Hui Zhang Dan Zhang Huawei Wang Yalong Li Zhengquan Yao Sai Wang Jun Xu 《Sedimentology》2019,66(5):1861-1895
The East China Sea Shelf has an unusually wide and low gradient shelf, supplied from sediment‐charged rivers and large river delta systems, with bottom currents sweeping the sea floor and located in the path of strong typhoons. Sediment gravity flow deposits, including four hybrid event beds and a high density turbidite, are identified in a core from the mid‐shelf of the East China Sea. The hybrid event beds typically comprise three or two internal divisions from the base to the top: (i) H1, H3 and H5; or (ii) H3 and H5. Radiocarbon ages of the hybrid event beds were in the range of 3821 to 8526 yr bp . Based on correlation with surrounding cores, the hybrid events may have happened at any time between 1930 yr bp and 3890 yr bp . The δ13C values in hybrid event beds together with bathymetry data suggest local erosion on the shelf. The average δ13C value for the H1 division is similar to the H3 division in the hybrid event beds, implying that the organic matter in the H1 and H3 divisions may come from the same source area. Cross‐plots of upper continental crust normalized rare earth elements in the five units reveal that the sediment source of the four hybrid event beds and the turbidite was ultimately primarily from Korean rivers. Partial transformation from a moderate‐strength debris flow with the additional role of erosional bulking can explain occurrences of hybrid event beds on the East China Sea Shelf. The data indicate that hybrid sediment gravity flow deposits were sourced from intra‐shelf failures and subsequently transformed and deposited as hybrid event beds. The study shows that hybrid sediment gravity flows and turbidity currents may not necessarily indicate proximity to a major fluvial or deltaic system and that intra‐shelf sedimentation can be a sediment source. It is unlikely that the debris flows and turbidity currents were triggered by a hyperpycnal flow or tsunami, because both can carry continental and/or coastal signals which have not been recognized in the core. Typhoons are the probable triggering mechanism. 相似文献