机译:南南极洲阿蒙松海扶盟的地热表面热流升高
Alfred Wegener Inst Helmholtz Ctr Polar &
Marine Res Alten Hafen 26 D-27568 Bremerhaven Germany;
Alfred Wegener Inst Helmholtz Ctr Polar &
Marine Res Alten Hafen 26 D-27568 Bremerhaven Germany;
Univ Bremen Dept Geosci Klagenfurter Str 2-4 D-28359 Bremen Germany;
AWI Bremerhaven Germany;
AWI Bremerhaven Germany;
AWI Bremerhaven Germany;
AWI Bremerhaven Germany;
AWI Bremerhaven Germany;
AWI Bremerhaven Germany;
AWI Bremerhaven Germany;
AWI Bremerhaven Germany;
AWI Bremerhaven Germany;
AWI Bremerhaven Germany;
BAS Cambridge England;
BAS Cambridge England;
BAS Cambridge England;
MARUM Bremen Germany;
MARUM Bremen Germany;
MARUM Bremen Germany;
MARUM Bremen Germany;
Univ Bremen Bremen Germany;
Univ Bremen Bremen Germany;
Univ Leipzig Leipzig Germany;
NOCS UK Southampton Hants England;
Imperial UK London England;
Imperial BAS London England;
Univ Lancaster Lancaster England;
Tech Univ Dresden Dresden Germany;
Tech Univ Dresden Dresden Germany;
VNIlOkean Moscow Russia;
skin depth for geothermal gradients; spatial variation of geothermal heat flow on small scales; in situ temperature measurements; geotherm transition;
机译:南南极洲阿蒙松海扶盟的地热表面热流升高
机译:西南极阿蒙松海部扇区的地热热通量:从温度测量,磁源估计底部的深度和热建模的新见解
机译:西南极阿蒙松海部扇区的地热热通量:从温度测量,磁源估计底部的深度和热建模的新见解
机译:南极阿蒙森海的海冰性质
机译:南极洲Weddell海上掌握的冰川历史
机译:方丈冰架阿蒙森海大陆边缘的结构和西南极洲贝灵斯豪森板块向南的边界
机译:南极西部阿蒙森海湾的极地深水入流和出口冰川减薄的热带强迫