期刊文献+
共找到3篇文章
< 1 >
每页显示 20 50 100
Palaeoclimatic Cycles, Global Environmental Changes and New Glacial Periods Induced by the Impact of Extraterrestrial Bodies
1
作者 王世杰 欧阳自远 肖志峰 《Chinese Journal Of Geochemistry》 EI CAS 1999年第4期298-304,共7页
In terms of Earth\|Sun geometry, the Milankovitch theory has successfully explained most of the cyclic palaeoclimatic variations during the history of the Earth, especially in the Quaternary. In this paper, the author... In terms of Earth\|Sun geometry, the Milankovitch theory has successfully explained most of the cyclic palaeoclimatic variations during the history of the Earth, especially in the Quaternary. In this paper, the authors suggest that the impact of extraterrestrial bodies on the Earth may be another mechanism to cause palaeoclimatic cycles, global environmental changes and new glacial periods. Based on geological and geochemical records in the boundary layers produced by six huge Cenozoic bolide\|impact events (65, 34, 15, 2.4, 1.1, 0.73 Ma B.P.), including those at 34, 15, 1.1 and 0.73 Ma B.P. which are represented by four famous tektite\|strewn fields, the process and mechanics of palaeoclimatic cycles and global environmental catastrophes induced by extraterrestrial impact are discussed in detail. Impact\|generated dust, soot and aerosol floating in the stratosphere could result in short\|term (<1 year), rapid drop in temperature immediately after impact. Through self\|regulation of the Earth’s climate system, the temperature at the surface slowly went up within 100a and maintained stable for a long time at 250K. If there were no other factors leading to the break\|down of the newly\|established equilibrium, a new glacial period would be initiated. Estimating from the thickness of \{δ\{\}\+\{13\}C\} and \{δ\{\}\+\{18\}O\} anomalies in sediments across the impact boundary layer and deposition rate, the duration of two stages of the palaeoclimate cycle in the form of cold weather—greenhouse effect—normal weather was 10\+4-10\+5a, respectively. The conclusion deduced from the above model is supported by palaeotemperature change recorded by oxygen isotope in sediments across the impact boundary layer. 展开更多
关键词 古气候 地球环境 流星事件 新生代 新冰河时期
下载PDF
Palaeoclimatic cycles and new glacial periods induced by the impact of extraterrestrial bodies
2
作者 WANG Shijie, OUYANG Ziyuan, XIAO Zhifeng and LI Chunlai State Key Laboratory of Environmental Geochemistry, Institute of Geochemistry, Chinese Academy of Sciences, Guiyang 550002, China. 《Chinese Science Bulletin》 SCIE EI CAS 1999年第S2期128-130,共3页
THE consequence of "nuclear winter" induced by nuclear war and climatic catastrophe induced by extraterrestrial impact were widely studied for fear of the potential danger of the basic nuclear war (the total... THE consequence of "nuclear winter" induced by nuclear war and climatic catastrophe induced by extraterrestrial impact were widely studied for fear of the potential danger of the basic nuclear war (the totalexplosive equivalent 5 000Mt TNT). Using zero-dimensional energy balance model authors reportedthe short-term climatic effect induced by six huge Cenozoic bolide-impact events (65, 34, 15, 2.4,1.1, 0.73 MaBP). However, only the direct climatic effect of dusts yielded by the impact was considered in the previous study. In this note, based on the previous simulation results the effect of variance ofglobal reflectance with temperature on the long-term climatic change was further taken into consideration.Combined with the strata records of palaeoclimatic change the relationship of impact energy with its in- 展开更多
关键词 bolide impact events palaeoclimatic cycle formation of new glacial period simulating calculation cenozoic.
原文传递
地外撞击诱发的气候循环和新冰期的形成 被引量:2
3
作者 王世杰 欧阳自远 +1 位作者 肖志峰 李春来 《地球科学(中国地质大学学报)》 EI CAS CSCD 北大核心 1999年第6期568-572,共5页
考虑全球反照率随温度的变化 ,利用零维能量平衡模式 ,对撞击能量与其诱发的气候循环和新冰期形成之间的关系进行了计算模拟研究 .当撞击坑的直径大于 1 5~ 2 0km ,全球气温在 1a的时间里会产生快速的降温 ,降温幅度取决于撞击能量的大... 考虑全球反照率随温度的变化 ,利用零维能量平衡模式 ,对撞击能量与其诱发的气候循环和新冰期形成之间的关系进行了计算模拟研究 .当撞击坑的直径大于 1 5~ 2 0km ,全球气温在 1a的时间里会产生快速的降温 ,降温幅度取决于撞击能量的大小 .大约不到 1 0 0a的时间 ,下降趋势逐渐减缓 ,全球气温缓慢上升 ,并稳定在 2 5 0K .如果没有别的因素影响 ,这一平衡温度将会稳定地存在较长一段时间 ,有可能导致地球上冰期气候的形成 .结合新生代以来 6次撞击事件 ,包括 6 5Ma的白垩纪 /第三纪 (K/R)和 2 .4Ma的第三纪 /第四纪 (R/Q)界线事件以及距今 34Ma ,1 5Ma ,1 .1Ma和 0 .73Ma前的北美玻璃陨石、捷克斯洛伐克玻璃陨石、象牙海岸玻璃陨石和澳 -亚玻璃陨石事件的古气候变化记录 ,估算巨大地外撞击作用诱发的冷期—回升—正常的古气候循环 ,每一阶段所需的时间为 1 0 4 ~ 1 0 5a.多期次的 2 .4Ma撞击事件可能是诱发第四纪特有的、频繁激烈的周期性冰期 展开更多
关键词 地外撞击作用 古气候循环 古气候记录 新生代
下载PDF
上一页 1 下一页 到第
使用帮助 返回顶部