首页 | 本学科首页   官方微博 | 高级检索  
文章检索
  按 检索   检索词:      
出版年份:   被引次数:   他引次数: 提示:输入*表示无穷大
  收费全文   4篇
  免费   0篇
地球物理   1篇
地质学   2篇
综合类   1篇
  2015年   1篇
  2013年   1篇
  2000年   1篇
  1998年   1篇
排序方式: 共有4条查询结果,搜索用时 15 毫秒
1
1.
This study presents cross-sectional vector maps of the magnetic field derived from IMP 8 magnetometer in the magnetosheath at 30 Re behind the Earth. In addition the vector patterns of the magnetosheath field for northward, southward, and east-west interplanetary magnetic field (IMF) directions are qualitatively compared with those obtained from the Spreiter-Stahara gas dynamic (GD) and Fedder-Lyon magnetohydrodynamic models (MHD). The main purpose is to display the cross-sectional differences in relation to the dayside merging with different IMF directions, allowing the reader to make direct visual comparisons of the vector patterns. It is seen that for east-west IMF directions, the data-based and MHD-based patterns differ noticeably in a similar way from the GD model, presumably reflecting the influence of dayside magnetic merging of the Earths magnetic field with the y-component of the interplanetary magnetic field. All three northward IMF cross sections show comparable field draping patterns as expected for a closed magnetosphere. For southward IMF case, on the other hand, differences between the three cross-sectional patterns are greater as seen in the field vector sizes and directions, especially closer to the magnetopause where more disturbed magneto-spheric conditions are known to be exist. The data comparisons with the MHD and GD models show that the differences result from the magnetic field-flow coupling and that the effects of dayside reconnection are present in IMP 8 magnetic field measurements.  相似文献   
2.
韩吉龙  王清海 《世界地质》2015,34(4):886-902
华北克拉通辽东半岛地区广泛发育侵位于青白口系不同层位中的辉绿岩(脉)岩墙,对其锆石CL图像、U--Pb定年和岩石地球化学特征研究得出以下结论。锆石类型有三组:前两组锆石具有早期岩浆作用的锆石属性或结晶基底的变质锆石属性,反映该区辉绿岩岩浆上升过程受到了陆壳的混染;第三组锆石多呈自形--半自形短柱状,发育岩浆振荡生长环带结构或条带结构,具原生岩浆成因锆石属性,锆石SHRIMP U--Pb定年显示其加权平均年龄为832.3±8.1 Ma(n=14,MSWD=1.3),可以代表辉绿岩的结晶年龄。岩石地球化学组成,其具有低Si O_2、Al_2O_3,高TFe_2O_3、MgO、Ti O_2的特征,这与拉斑玄武岩特征相似;其稀土元素总量相对较低(ΣREE=71.88×10~-6~129.64×10~-6),且具弱的正Eu异常和铌亏损;略富集轻稀土元素(LREE)、富集大离子亲石元素(LILE:Rb、Pb、Ba)和高场强元素(HFSE:Th、U、Zr、Ti、Hf),而亏损高场强元素(HFSE:Nb、Sm、Gd、P)等;以上特征指示岩浆源区为富集型地幔,且上侵位就位过程中受陆壳不同程度的同化混染。本文对辉绿岩的研究显示华北克拉通辽东半岛地区在新元古代早期存在基性岩浆活动,结合前人对华北克拉通中元古代晚期—新元古代早期构造--岩浆事件的研究成果,进一步证明了华北克拉通东北部在新元古代早期经历了挤压汇聚后的伸展裂解演化过程,这与Rodinia超大陆聚合和裂解事件一致。  相似文献   
3.
AMP deaminase catalyzes the conversion of AMP into IMP and ammonia. In the present study, a full-length cDNA of AMPD1 from skeletal muscle of Japanese flounder Paralichthys olivaceus was cloned and characterized. The 2 526 bp cDNA contains a 5’-UTR of 78 bp, a 3’-UTR of 237 bp and an open reading frame (ORF) of 2 211 bp, which encodes a protein of 736 amino acids. The predicted protein contains a highly conserved AMP deaminase motif (SLSTDDP) and an ATP-binding site sequence (EPLMEEYAIAAQVFK). Phylogenetic analysis showed that the AMPD1 and AMPD3 genes originate from the same branch, but are evolutionarily distant from the AMPD2 gene. RT-PCR showed that the flounder AMPD1 gene was expressed only in skeletal muscle. QRT-PCR analysis revealed a statistically significant 2.54 fold higher level of AMPD1 mRNA in adult muscle (750±40 g) compared with juvenile muscle (7.5±2 g) (P<0.05). HPLC analysis showed that the IMP content in adult muscle (3.35±0.21 mg/g) was also statistically significantly higher than in juvenile muscle (1.08±0.04 mg/g) (P<0.05). There is a direct relationship between the AMPD1 gene expression level and IMP content in the skeletal muscle of juvenile and adult flounders. These results may provide useful information for quality improvement and molecular breeding of aquatic animals.  相似文献   
4.
A RIFTING STORY OF SOUTH CHINA, WITH PARTICULAR REFERENCE TO RODINIA BREAKUP  相似文献   
1
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号