日期:
2020 年 — 2026 年
2020
2021
2022
2023
2024
2025
2026
影响因子:

Fluid flow behaviour in vesicular basalt samples from the Skoll High, Vøring Margin

来自斯科尔高地和沃林海沟的泡状玄武岩样品中的流体流动行为

Betlem, Peter; Rosenqvist, Marija Plahter; Millett, John; Griffiths, Luke; Filina, Irina; Park, Joonsang; Planke, Sverre; Senger, Kim; Skurtveit, Elin

Meltwater sediment transport as the dominating process in mid-latitude trough mouth fan formation

融水沉积物输送是中纬度海槽口扇形成的主要过程

Bellwald, Benjamin; Planke, Sverre; Becker, Lukas W M; Myklebust, Reidun

A Cyber-Physical-Human System for One-to-Many UAS Operations: Cognitive Load Analysis

面向一对多无人机系统操作的赛博物理人系统:认知负荷分析

Planke, Lars J; Lim, Yixiang; Gardi, Alessandro; Sabatini, Roberto; Kistan, Trevor; Ezer, Neta

The main pulse of the Siberian Traps expanded in size and composition

西伯利亚地盾的主要脉动在规模和成分上都发生了扩张。

Augland, L E; Ryabov, V V; Vernikovsky, V A; Planke, S; Polozov, A G; Callegaro, S; Jerram, D A; Svensen, H H

Sensor Networks for Aerospace Human-Machine Systems

航空航天人机系统的传感器网络

Pongsakornsathien, Nichakorn; Lim, Yixiang; Gardi, Alessandro; Hilton, Samuel; Planke, Lars; Sabatini, Roberto; Kistan, Trevor; Ezer, Neta

Author Correction: Glacigenic sedimentation pulses triggered post-glacial gas hydrate dissociation

作者更正:冰川沉积脉冲引发了冰后期天然气水合物的分解

Karstens, Jens; Haflidason, Haflidi; Becker, Lukas W M; Berndt, Christian; Rüpke, Lars; Planke, Sverre; Liebetrau, Volker; Schmidt, Mark; Mienert, Jürgen

Sills and gas generation in the Siberian Traps

西伯利亚地盾的岩床和天然气生成

Svensen, Henrik H; Frolov, Sergei; Akhmanov, Grigorii G; Polozov, Alexander G; Jerram, Dougal A; Shiganova, Olga V; Melnikov, Nikolay V; Iyer, Karthik; Planke, Sverre

Constraining shifts in North Atlantic plate motions during the Palaeocene by U-Pb dating of Svalbard tephra layers

利用斯瓦尔巴群岛火山灰层的U-Pb定年法来约束古新世期间北大西洋板块运动的变化

Jones, Morgan T; Augland, Lars E; Shephard, Grace E; Burgess, Seth D; Eliassen, Gauti T; Jochmann, Malte M; Friis, Bjarki; Jerram, Dougal A; Planke, Sverre; Svensen, Henrik H

Thermogenic methane release as a cause for the long duration of the PETM

热生成甲烷的释放是导致古新世-始新世极热事件(PETM)持续时间较长的原因之一。

Frieling, Joost; Svensen, Henrik H; Planke, Sverre; Cramwinckel, Marlow J; Selnes, Haavard; Sluijs, Appy