3篇
您的检索式：作者名="N.J.Shackleton"
|
|
|
题名
|
作者
|
年代
|
出处
|
被引量
|
| 1 | 最近130ka洛川黄土堆积序列与格陵兰冰芯记录显示文摘现今中国大陆冬季气候与冷空气活动有关,的巴伦支海、西北方的喀拉海和西方的大西洋.形成西伯利亚-蒙古高压的冷空气来自北方现代尘暴和降尘事件主要发生于冬半年,并与西伯利亚-蒙古高压冷空气活动决定的偏北风有关. | 安芷生 孙东怀 张小曳 周卫建 S.C.Porter J.Chappell N.J.Shackleton 张代洲 | 1994 | 科学通报1994，39，24： | 58 |
| 2 | 欧亚黄土中古地磁极性界线的地层学解释显示文摘本文以欧亚黄土中记录的布容一松山极性倒转界线为例,简要回顾近年来对黄土中 古地磁极性界线地层学解释的讨论。研究表明,由于在记录古地磁极性转换时存在不同程度 的“错位”,黄土中所测的极性界线的年代地层意义存在很大的不确定性。就中国黄土而言,第 8层黄土(L_8)中下部或第8层古土壤(S_8)顶部测得的布容-松山界线系“错位”的产物,该层位 的年龄应老于 0.79MaB.P。对黄土中测得的Cobb Mountain极性事件界线进行地层学解释, 推论蓝田猿人化石层位的年龄1.2MaB.P。 | 周力平 N.J.Shackleton A.E.Dodonov | 2000 | 第四纪研究2000，20，2： | 13 |
| 3 | NEW TECHNIQUE FOR STUDY ON ISOTOPIC FRACTIONATION BETWEEN SEA WATER AND FORAMINIFERAL GROWING PROCESSES显示文摘The stable isotopic δ18O and δ13C composition of foraminiferal shell calcite varies as a function of many factors including temperature and salinity. In order to understand and interpret the variations in the isotopic composition of foraminiferal shell calcite, research has been recently focused on the role of the 'vital effects’. Our examination of the lamella structure of several recent planktonic foraminifera indicates that the secretion of sequential lamellae results in multiple lamillae on earlier chambers and a single lamella on the final chamber. We used a very simple procedure to separate the individual whole test of foraminifera into several chambers and measured the isotopic composition of each growth stage chamber. The results indicate that the stable isotopic composition (carbon and oxy -gen), particukrly that of the last two chambers, of the foraminiferal test varies as a function of the individual growing process. | 苍树溪 N.J.Shackleton | 1990 | Chinese Journal of Oceanology and Limnology1990，8，4： | 0 |
您所在的机构暂未开通此部分的功能，请联系管理员