Extensive 200-Million-Year-Old Continental Flood Basalts of the Central Atlantic Magmatic Province
The Central Atlantic Magmatic Province (CAMP) is defined by tholeiitic basalts that crop out in once-contiguous parts of North America, Europe, Africa, and South America and is associated with the breakup of Pangea. $^{40}$Ar/$^{39}$Ar and paleomagnetic data indicate that CAMP magmatism extended ove...
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| Published in | Science (American Association for the Advancement of Science) Vol. 284; no. 5414; pp. 616 - 618 |
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| Main Authors | , , , , , |
| Format | Journal Article |
| Language | English |
| Published |
Washington, DC
American Society for the Advancement of Science
23.04.1999
American Association for the Advancement of Science The American Association for the Advancement of Science |
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| Online Access | Get full text |
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| Abstract | The Central Atlantic Magmatic Province (CAMP) is defined by tholeiitic basalts that crop out in once-contiguous parts of North America, Europe, Africa, and South America and is associated with the breakup of Pangea. $^{40}$Ar/$^{39}$Ar and paleomagnetic data indicate that CAMP magmatism extended over an area of 2.5 million square kilometers in north and central Brazil, and the total aerial extent of the magmatism exceeded 7 million square kilometers in a few million years, with peak activity at 200 million years ago. The magmatism coincided closely in time with a major mass extinction at the Triassic-Jurassic boundary. |
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| AbstractList | The Central Atlantic Magmatic Province (CAMP) is defined by tholeiitic basalts that crop out in once-contiguous parts of North America, Europe, Africa, and South America and is associated with the breakup of Pangea. 40Ar/39Ar and paleomagnetic data indicate that CAMP magmatism extended over an area of 2.5 million square kilometers in north and central Brazil, and the total aerial extent of the magmatism exceeded 7 million square kilometers in a few million years, with peak activity at 200 million years ago. The magmatism coincided closely in time with a major mass extinction at the Triassic-Jurassic boundary. The Central Atlantic Magmatic Province (CAMP) is defined by tholeiitic basalts that crop out in once-contiguous parts of North America, Europe, Africa, and South America and is associated with the breakup of Pangea. $^{40}$Ar/$^{39}$Ar and paleomagnetic data indicate that CAMP magmatism extended over an area of 2.5 million square kilometers in north and central Brazil, and the total aerial extent of the magmatism exceeded 7 million square kilometers in a few million years, with peak activity at 200 million years ago. The magmatism coincided closely in time with a major mass extinction at the Triassic-Jurassic boundary. The Central Atlantic Magmatic Province (CAMP) is defined by tholeiitic basalts that crop out in once-contiguous parts of North America, Europe, Africa, and South America and is associated with the breakup of Pangea. [sup.40]Ar/[sup.39]Ar and paleomagnetic data indicate that CAMP magrnatism extended over an area of 2.5 million square kilometers in north and central Brazil, and the total aerial extent of the magmatism exceeded 7 million square kilometers in a few million years, with peak activity at 200 million years ago. The magmatism coincided closely in time with a major mass extinction at the Triassic-Jurassic boundary. The Central Atlantic Magmatic Province (CAMP) is defined by tholeiitic basalts that crop out in once-contiguous parts of North America, Europe, Africa and South America and is associated with the breakup of Pangea. The Central Atlantic Magmatic Province (CAMP) is defined by tholeiitic basalts that crop out in once-contiguous parts of North America, Europe, Africa, and South America and is associated with the breakup of Pangea. super(40)Ar/ super(39)Ar and paleomagnetic data indicate that CAMP magmatism extended over an area of 2.5 million square kilometers in north and central Brazil, and the total aerial extent of the magmatism exceeded 7 million square kilometers in a few million years, with peak activity at 200 million years ago. The magmatism coincided closely in time with a major mass extinction at the Triassic-Jurassic boundary. The Central Atlantic Magmatic Province (CAMP) is defined by tholeiitic basalts that crop out in once-contiguous parts of North America, Europe, Africa, and South America and is associated with the breakup of Pangea. 40 Ar/ 39 Ar and paleomagnetic data indicate that CAMP magmatism extended over an area of 2.5 million square kilometers in north and central Brazil, and the total aerial extent of the magmatism exceeded 7 million square kilometers in a few million years, with peak activity at 200 million years ago. The magmatism coincided closely in time with a major mass extinction at the Triassic-Jurassic boundary. |
| Audience | Academic |
| Author | Bellieni, Giuliano de Min, Angelo Renne, Paul R. Ernesto, Marcia Piccirillo, Enzo M. Marzoli, Andrea |
| Author_xml | – sequence: 1 givenname: Andrea surname: Marzoli fullname: Marzoli, Andrea – sequence: 2 givenname: Paul R. surname: Renne fullname: Renne, Paul R. – sequence: 3 givenname: Enzo M. surname: Piccirillo fullname: Piccirillo, Enzo M. – sequence: 4 givenname: Marcia surname: Ernesto fullname: Ernesto, Marcia – sequence: 5 givenname: Giuliano surname: Bellieni fullname: Bellieni, Giuliano – sequence: 6 givenname: Angelo surname: de Min fullname: de Min, Angelo |
| BackLink | http://pascal-francis.inist.fr/vibad/index.php?action=getRecordDetail&idt=1795259$$DView record in Pascal Francis https://www.ncbi.nlm.nih.gov/pubmed/10213679$$D View this record in MEDLINE/PubMed |
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| CODEN | SCIEAS |
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| Keywords | South America Mesozoic stratigraphic boundary Pangaea volcanic rocks Atlantic Ocean mass extinction igneous rocks volcanism volume Jurassic Triassic basalts paleomagnetism Ar-40/Ar-39 dating rifting Phanerozoic tholeiitic basalt |
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E. – ident: e_1_3_1_23_2 doi: 10.1126/science.253.5016.176 – volume: 161 start-page: 161 year: 1998 ident: e_1_3_1_26_2 publication-title: ibid. contributor: fullname: Leitch A. M. – volume: 237 start-page: 1025 year: 1987 ident: e_1_3_1_27_3 publication-title: ibid. contributor: fullname: Olsen P. E. |
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| Snippet | The Central Atlantic Magmatic Province (CAMP) is defined by tholeiitic basalts that crop out in once-contiguous parts of North America, Europe, Africa, and... The Central Atlantic Magmatic Province (CAMP) is defined by tholeiitic basalts that crop out in once-contiguous parts of North America, Europe, Africa and... |
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| SubjectTerms | Analysis Argon Basalt Crystalline rocks Data sampling Earth Earth sciences Earth, ocean, space Error rates Exact sciences and technology Geochronology Geology Heat Igneous and metamorphic rocks petrology, volcanic processes, magmas Individualized Instruction Lava flows Magmatism Marine Plumes Scientific Concepts |
| Title | Extensive 200-Million-Year-Old Continental Flood Basalts of the Central Atlantic Magmatic Province |
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