用户名: 密码: 验证码:
Mantle transition-zone structure beneath the South Pacific Superswell and evidence for a mantle plume underlying the Society hotspot
详细信息查看全文 | 推荐本文 |
摘要
Underside reflections of shear waves from the discontinuities at 410 and 660 km depth are used to map lateral variations in the thickness of the mantle transition zone beneath the South Pacific Superswell and surrounding regions. Differential travel times of reflected waves indicate that the transition zone is about 25 km thinner than normal, and thus hotter than normal, over an area 500 km or less in diameter beneath the Society hotspot. There is no general difference, however, in transition-zone thickness between the Superswell area and its surroundings. Our observations support the inference that the thermal flux from lower to upper mantle beneath the South Pacific Superswell occur on the lateral scale of a mantle plume (several hundred kilometers) rather than that of a superplume (several thousand kilometers).

© 2004-2018 中国地质图书馆版权所有 京ICP备05064691号 京公网安备11010802017129号

地址:北京市海淀区学院路29号 邮编:100083

电话:办公室:(+86 10)66554848;文献借阅、咨询服务、科技查新:66554700