| pubmed-article:11875202 | rdf:type | pubmed:Citation | lld:pubmed |
| pubmed-article:11875202 | lifeskim:mentions | umls-concept:C0025260 | lld:lifeskim |
| pubmed-article:11875202 | lifeskim:mentions | umls-concept:C1446409 | lld:lifeskim |
| pubmed-article:11875202 | lifeskim:mentions | umls-concept:C0013463 | lld:lifeskim |
| pubmed-article:11875202 | lifeskim:mentions | umls-concept:C0015744 | lld:lifeskim |
| pubmed-article:11875202 | lifeskim:mentions | umls-concept:C2911691 | lld:lifeskim |
| pubmed-article:11875202 | pubmed:dateCreated | 2002-3-4 | lld:pubmed |
| pubmed-article:11875202 | pubmed:abstractText | We review the "critical point" concept for large earthquakes and enlarge it in the framework of so-called "finite-time singularities." The singular behavior associated with accelerated seismic release is shown to result from a positive feedback of the seismic activity on its release rate. The most important mechanisms for such positive feedback are presented. We solve analytically a simple model of geometrical positive feedback in which the stress shadow cast by the last large earthquake is progressively fragmented by the increasing tectonic stress. | lld:pubmed |
| pubmed-article:11875202 | pubmed:commentsCorrections | http://linkedlifedata.com/r... | lld:pubmed |
| pubmed-article:11875202 | pubmed:commentsCorrections | http://linkedlifedata.com/r... | lld:pubmed |
| pubmed-article:11875202 | pubmed:language | eng | lld:pubmed |
| pubmed-article:11875202 | pubmed:journal | http://linkedlifedata.com/r... | lld:pubmed |
| pubmed-article:11875202 | pubmed:citationSubset | IM | lld:pubmed |
| pubmed-article:11875202 | pubmed:status | MEDLINE | lld:pubmed |
| pubmed-article:11875202 | pubmed:month | Feb | lld:pubmed |
| pubmed-article:11875202 | pubmed:issn | 0027-8424 | lld:pubmed |
| pubmed-article:11875202 | pubmed:author | pubmed-author:SandraAA | lld:pubmed |
| pubmed-article:11875202 | pubmed:author | pubmed-author:SornetteDD | lld:pubmed |
| pubmed-article:11875202 | pubmed:issnType | Print | lld:pubmed |
| pubmed-article:11875202 | pubmed:day | 19 | lld:pubmed |
| pubmed-article:11875202 | pubmed:volume | 99 Suppl 1 | lld:pubmed |
| pubmed-article:11875202 | pubmed:owner | NLM | lld:pubmed |
| pubmed-article:11875202 | pubmed:authorsComplete | Y | lld:pubmed |
| pubmed-article:11875202 | pubmed:pagination | 2501-8 | lld:pubmed |
| pubmed-article:11875202 | pubmed:dateRevised | 2010-9-14 | lld:pubmed |
| pubmed-article:11875202 | pubmed:meshHeading | pubmed-meshheading:11875202... | lld:pubmed |
| pubmed-article:11875202 | pubmed:meshHeading | pubmed-meshheading:11875202... | lld:pubmed |
| pubmed-article:11875202 | pubmed:meshHeading | pubmed-meshheading:11875202... | lld:pubmed |
| pubmed-article:11875202 | pubmed:meshHeading | pubmed-meshheading:11875202... | lld:pubmed |
| pubmed-article:11875202 | pubmed:meshHeading | pubmed-meshheading:11875202... | lld:pubmed |
| pubmed-article:11875202 | pubmed:year | 2002 | lld:pubmed |
| pubmed-article:11875202 | pubmed:articleTitle | Positive feedback, memory, and the predictability of earthquakes. | lld:pubmed |
| pubmed-article:11875202 | pubmed:affiliation | Department of Earth Sciences, University of Southern California, Los Angeles, CA 90089-0740, USA. sammis@usc.edu | lld:pubmed |
| pubmed-article:11875202 | pubmed:publicationType | Journal Article | lld:pubmed |
| pubmed-article:11875202 | pubmed:publicationType | Research Support, U.S. Gov't, Non-P.H.S. | lld:pubmed |
| pubmed-article:11875202 | pubmed:publicationType | Research Support, Non-U.S. Gov't | lld:pubmed |
| http://linkedlifedata.com/r... | pubmed:referesTo | pubmed-article:11875202 | lld:pubmed |
