Dîne des Puys, France) : résultats préliminaires
详细信息    查看全文
文摘
Preliminary soil-temperature measurements over 16 months indicate an important geothermal flux of at least 0.4 Wm−2 on the summit of a scoria cone in the Chaîne des Puys (France). This anomaly can be explained by a residual hydrothermal flux that has begun when the maar and the overlying cone were formed around 30000 years ago. To cite this article: M. Aubert, C. R. Geoscience 336 (2004).

© 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