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pubmed-article:17796676rdf:typepubmed:Citationlld:pubmed
pubmed-article:17796676lifeskim:mentionsumls-concept:C0079853lld:lifeskim
pubmed-article:17796676lifeskim:mentionsumls-concept:C1707807lld:lifeskim
pubmed-article:17796676pubmed:issue4336lld:pubmed
pubmed-article:17796676pubmed:dateCreated2010-6-7lld:pubmed
pubmed-article:17796676pubmed:abstractTextThe Gruithuisen and Mairan domes on the moon represent morphologically and spectrally distinct nonmare extrusive volcanic features of Imbrian age. The composition, morphology, and age relationships of the domes indicate that nonmare extrusive volcanism in the northern Procellarum region of the moon continued until about 3.3 x 10(9) to 3.6 x 10(9) years ago and was partially contemporaneous with the emplacement of the main sequence of mare deposits.lld:pubmed
pubmed-article:17796676pubmed:languageenglld:pubmed
pubmed-article:17796676pubmed:journalhttp://linkedlifedata.com/r...lld:pubmed
pubmed-article:17796676pubmed:statusPubMed-not-MEDLINElld:pubmed
pubmed-article:17796676pubmed:monthMarlld:pubmed
pubmed-article:17796676pubmed:issn0036-8075lld:pubmed
pubmed-article:17796676pubmed:authorpubmed-author:HeadJ WJW3rdlld:pubmed
pubmed-article:17796676pubmed:authorpubmed-author:McCordT BTBlld:pubmed
pubmed-article:17796676pubmed:issnTypePrintlld:pubmed
pubmed-article:17796676pubmed:day31lld:pubmed
pubmed-article:17796676pubmed:volume199lld:pubmed
pubmed-article:17796676pubmed:ownerNLMlld:pubmed
pubmed-article:17796676pubmed:authorsCompleteYlld:pubmed
pubmed-article:17796676pubmed:pagination1433-6lld:pubmed
pubmed-article:17796676pubmed:year1978lld:pubmed
pubmed-article:17796676pubmed:articleTitleImbrian-age highland volcanism on the moon: the gruithuisen and mairan domes.lld:pubmed
pubmed-article:17796676pubmed:publicationTypeJournal Articlelld:pubmed