期刊文献+
共找到3篇文章
< 1 >
每页显示 20 50 100
Nonlinear Dynamic Study on Geomagnetic Polarity Reversal and Cretaceous Normal Superchron
1
作者 SHEN Wei 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2007年第6期1097-1102,共6页
It is generally acknowledged that geomagnetic polarity has reversed many times in geological history and an abnormal geologic phenomenon is the Cretaceous normal superchron. However, the causes have been unknown up to... It is generally acknowledged that geomagnetic polarity has reversed many times in geological history and an abnormal geologic phenomenon is the Cretaceous normal superchron. However, the causes have been unknown up to now. The nonlinear theory has been applied to analyze the phenomenon in geomagnetic polarity reversal and the Cretaceous normal superchron. The Cretaceous normal superchron implies that interaction of the Earth's core-mantle and liquid movement in the outer core may be the lowest energy state and the system of Earth magnetic field maintains a sort of temporal or spatial order structure by exchanging substance and energy in the outside continuously. During 121-83 Ma, there was no impact of a celestial body that would result in a geomagnetic polarity reversal, which may be a cause for occurrence of the Cretaceous normal superchron.The randomness of geomagnetic polarity reversal has the self-reversion characteristic of chaos and the chaos theory gives a simple and clear explanation for the dynamic cause of the geomagnetic polarity reversal. 展开更多
关键词 NONLINEARITY geomagnetic polarity reversal Cretaceous normal superchron (CNS)
下载PDF
A Middle Pleistocene Glaciation Record from Lacustrine Sediments in the Western Tibetan Plateau and Discussion on Climate Change
2
作者 ZHAO Zhenming JI Wenhua FU Chaofeng 《Acta Geologica Sinica(English Edition)》 SCIE CAS CSCD 2023年第2期623-635,共13页
The Tibetan Plateau is an important area for studying global climate change,but the answers to many scientific problems remain unknown.Here,we present new information from the lacustrine sedimentary record in the west... The Tibetan Plateau is an important area for studying global climate change,but the answers to many scientific problems remain unknown.Here,we present new information from the lacustrine sedimentary record in the western Tibetan Plateau,related to the third most-recent glaciations.Continuous sediment data,including sporopollen,particle size,total organic carbon,mass susceptibility,CaCO_(3),CaSO_(4),BaSO_(4)contents and chronological data,were reconstructed and revealed that climate and environmental conditions obviously and distinctly changed between 600 and 700 thousand years ago.In comparison,the data obtained from the Guliya ice core in this area also corresponds to the global glacial climatic characteristics recorded in basin sediments in the eastern and southeastern regions of the plateau and to the information obtained from ice cores in the Antarctic and Arctic regions.In this study,we conclude that the main reason for the glaciations and new tectonic movement must be a geomagnetic polarity reversal 774 thousand years ago(from Matuyama to Brunhes).Indeed,the results of this study suggest that the described reversal event might have influenced the current global climate pattern and will continue to impact climatic changes in the future. 展开更多
关键词 glacial record global climate change geomagnetic polarity reversal middle Pleistocene western Tibetan Plateau
下载PDF
Geomagnetic polarity transitions recorded in the Miocene lavas of the Wuyu basin,Tibet
3
作者 TONG YaBo YANG ZhenYu +4 位作者 PAN YongXin ZHENG LianDi SUN ZhiMing PEI JunLing ZHUANG ZhongHai 《Science China Earth Sciences》 SCIE EI CAS 2011年第4期561-570,共10页
Geomagnetic polarity transitions were the most important phenomena in the study of the geomagnetic field evolution and the earth's deep interior dynamics. The Miocene postcollisional ultrapotassic-potassic rocks are ... Geomagnetic polarity transitions were the most important phenomena in the study of the geomagnetic field evolution and the earth's deep interior dynamics. The Miocene postcollisional ultrapotassic-potassic rocks are widely distributed in the Lhasa Block of southern Tibet. Paleomagnetic studies on the Wuyu Formation indicated that these volcanic rocks recorded the C5Bn.2n-C5Bn.lr and C5ACr-C5ACn geomagnetic polarity transitions. The virtual geomagnetic poles (VGPs) of these two polarity transitions were located in the Atlantic and the central Pacific, respectively. Due to data scarcity, it remains unclear whether VGP paths of Miocene geomagnetic polarity transitions were longitudinal preference and/or 90° away from the sampiing sites. 展开更多
关键词 Tibetan Plateau MIOCENE VOLCANICS PALEOMAGNETIC geomagnetic polarity transition
原文传递
上一页 1 下一页 到第
使用帮助 返回顶部