Geomagnetic polarity transitions recorded in the Miocene lavas of the Wuyu basin, Tibet
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 th...
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| Veröffentlicht in: | Science China. Earth sciences 2011-04, Vol.54 (4), p.561-570 |
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| container_title | Science China. Earth sciences |
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| creator | Tong, YaBo Yang, ZhenYu Pan, YongXin Zheng, LianDi Sun, ZhiMing Pei, JunLing Zhuang, ZhongHai |
| description | 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. |
| doi_str_mv | 10.1007/s11430-010-4123-8 |
| format | Article |
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Earth sciences</jtitle></facets><delivery><delcategory>Remote Search Resource</delcategory><fulltext>fulltext</fulltext></delivery><addata><au>Tong, YaBo</au><au>Yang, ZhenYu</au><au>Pan, YongXin</au><au>Zheng, LianDi</au><au>Sun, ZhiMing</au><au>Pei, JunLing</au><au>Zhuang, ZhongHai</au><format>journal</format><genre>article</genre><ristype>JOUR</ristype><atitle>Geomagnetic polarity transitions recorded in the Miocene lavas of the Wuyu basin, Tibet</atitle><jtitle>Science China. Earth sciences</jtitle><stitle>Sci. China Earth Sci</stitle><addtitle>SCIENCE CHINA Earth Sciences</addtitle><date>2011-04-01</date><risdate>2011</risdate><volume>54</volume><issue>4</issue><spage>561</spage><epage>570</epage><pages>561-570</pages><issn>1674-7313</issn><eissn>1869-1897</eissn><abstract>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.</abstract><cop>Heidelberg</cop><pub>SP Science China Press</pub><doi>10.1007/s11430-010-4123-8</doi><tpages>10</tpages></addata></record> |
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| ispartof | Science China. Earth sciences, 2011-04, Vol.54 (4), p.561-570 |
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| subjects | Earth and Environmental Science Earth Sciences Geological time Geomagnetic field Geophysics Magnetic fields Miocene Paleomagnetism Polarity Research Paper Volcanic rocks 中新世 地球深部动力学 地磁极性转换 太平洋中部 火山岩 磁场演化 西藏南部 |
| title | Geomagnetic polarity transitions recorded in the Miocene lavas of the Wuyu basin, Tibet |
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