This article examined the use of the <sup>40</sup>Ar/<sup>39</sup>Ar incremental heating and K/Ar analyses to date dolerites located in the extreme north region in Brazil. The material used for...This article examined the use of the <sup>40</sup>Ar/<sup>39</sup>Ar incremental heating and K/Ar analyses to date dolerites located in the extreme north region in Brazil. The material used for dating was whole rock and separated minerals(plagioclases,pyroxene or/and amphibole)in 6 samples of dykes and sills from Roraima.The dolerites yield plateau ages ranging from 1955±17 Ma to 1179±10 Ma.The reason展开更多
<sup>40</sup>Ar/<sup>39</sup>Ar dating of plagioclases,pyroxene or/and amphibole of separated grains from Avanavero Dolerite located in the Guiana Shield,in Roraima State,Brazil yield plateau a...<sup>40</sup>Ar/<sup>39</sup>Ar dating of plagioclases,pyroxene or/and amphibole of separated grains from Avanavero Dolerite located in the Guiana Shield,in Roraima State,Brazil yield plateau ages ranging from 1840±50 Ma to 1179±10 Ma.The highest ages are interpreted to represent the emplacement of dolerites within the sandstones ofRoraima Supergroup,while the younger results reveal partial argon loss during the cooling history of the samples related to a large展开更多
文摘This article examined the use of the <sup>40</sup>Ar/<sup>39</sup>Ar incremental heating and K/Ar analyses to date dolerites located in the extreme north region in Brazil. The material used for dating was whole rock and separated minerals(plagioclases,pyroxene or/and amphibole)in 6 samples of dykes and sills from Roraima.The dolerites yield plateau ages ranging from 1955±17 Ma to 1179±10 Ma.The reason
文摘<sup>40</sup>Ar/<sup>39</sup>Ar dating of plagioclases,pyroxene or/and amphibole of separated grains from Avanavero Dolerite located in the Guiana Shield,in Roraima State,Brazil yield plateau ages ranging from 1840±50 Ma to 1179±10 Ma.The highest ages are interpreted to represent the emplacement of dolerites within the sandstones ofRoraima Supergroup,while the younger results reveal partial argon loss during the cooling history of the samples related to a large