EconPapers    
Economics at your fingertips  
 

Origin of Columbia River flood basalt controlled by propagating rupture of the Farallon slab

Lijun Liu and Dave R. Stegman
Additional contact information
Lijun Liu: IGPP, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California 92093, USA
Dave R. Stegman: IGPP, Scripps Institution of Oceanography, University of California, San Diego, La Jolla, California 92093, USA

Nature, 2012, vol. 482, issue 7385, 386-389

Abstract: A model of subduction that reveals a long tear under Oregon and Nevada provides a new mechanism for the origin of Columbia River flood basalt, resolving previous hypotheses.

Date: 2012
References: Add references at CitEc
Citations:

Downloads: (external link)
https://www.nature.com/articles/nature10749 Abstract (text/html)
Access to the full text of the articles in this series is restricted.

Related works:
This item may be available elsewhere in EconPapers: Search for items with the same title.

Export reference: BibTeX RIS (EndNote, ProCite, RefMan) HTML/Text

Persistent link: https://EconPapers.repec.org/RePEc:nat:nature:v:482:y:2012:i:7385:d:10.1038_nature10749

Ordering information: This journal article can be ordered from
https://www.nature.com/

DOI: 10.1038/nature10749

Access Statistics for this article

Nature is currently edited by Magdalena Skipper

More articles in Nature from Nature
Bibliographic data for series maintained by Sonal Shukla () and Springer Nature Abstracting and Indexing ().

 
Page updated 2025-03-19
Handle: RePEc:nat:nature:v:482:y:2012:i:7385:d:10.1038_nature10749