CHLORINE-36 EVIDENCE FOR THE MONO LAKE EVENT IN THE SUMMIT GRIP ICE CORE
| dc.contributor.author | Wagner G. | |
| dc.contributor.author | Beer J. | |
| dc.contributor.author | Laj C. | |
| dc.contributor.author | Kissel C. | |
| dc.contributor.author | Masarik J. | |
| dc.contributor.author | Muscheler R. | |
| dc.contributor.author | Synal H.A. | |
| dc.date.accessioned | 2021-01-24T05:12:18Z | |
| dc.date.available | 2021-01-24T05:12:18Z | |
| dc.date.issued | 2000 | |
| dc.description.abstract | A distinct peak has been discovered in the 36Cl data from the GRIP ice core between the Dansgaard Oeschger (D-O) events 6 and 7 at approximately 32 kyr BP. This peak can be attributed to a minimum of the geomagnetic dipole field associated with the Mono Lake event. Since the 36Cl peak reflects a higher production rate of all cosmogenic radionuclides, it has an impact on the 14C dating of the last ice age. Furthermore, it provides an additional time marker similar to a peak found earlier corresponding to the Laschamp event at approximately 39 kyr BP. | |
| dc.identifier | https://www.elibrary.ru/item.asp?id=367735 | |
| dc.identifier.citation | Earth and Planetary Science Letters, 2000, 181, 1-2, 1-6 | |
| dc.identifier.issn | 0012-821X | |
| dc.identifier.uri | https://repository.geologyscience.ru/handle/123456789/23642 | |
| dc.subject | CL-36 | |
| dc.subject | MAGNETIC FIELD | |
| dc.subject | PALEOMAGNETISM | |
| dc.subject | COSMOGENIC ELEMENTS | |
| dc.subject | RADIOACTIVE ELEMENTS | |
| dc.title | CHLORINE-36 EVIDENCE FOR THE MONO LAKE EVENT IN THE SUMMIT GRIP ICE CORE | |
| dc.type | Статья |