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Updated: Jul 13, 2026

Measuring Carbon-based Contaminant Mineralization Using Combined CO2 Flux and Radiocarbon Analyses
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哥伦比亚河洪水玄武岩和沃洛瓦山脉在俄勒冈州东北部升起的石质层不稳定的起源

T C Hales1, D L Abt, E D Humphreys

  • 1Department of Geological Sciences, 1272 University of Oregon, Eugene, Oregon 97403, USA. thales@uoregon.edu

Nature
|December 13, 2005
PubMed
概括

哥伦比亚河基岩 (CRB) 起源于沃洛瓦山脉附近,而不是黄石热点轨道. 地幔下垂和脱离的浮动根解释了CRB的岩和升起.

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