Platinum-group element abundances in background samples and the K-T boundary interval from DSDP Hole 91-596 (Table 2)
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| Natura: | Dataset Open Access |
| Lingua: | en |
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PANGAEA
1995
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| _version_ | 1867169956655792128 |
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| author | Evans, Noreen J Ahrens, Thomas J Gregoire, D C |
| author_facet | Evans, Noreen J Ahrens, Thomas J Gregoire, D C |
| collection | Datos científicos de ciencias marinas y ambientales |
| contents | New data on Ru/Ir abundance ratios are presented for nonmarine (Hell Creek, Montana; Frenchman River, Saskatchewan) and marine Cretaceous-Tertiary boundary sites (Brazos River, Texas; Beloc, Haiti; DSDP 577 and DSDP 596). The Ru/Ir ratio varies from 0.5 to 1 within 4000 km of Chicxulub and increases to 2-3 at paleodistances (65 Ma) of up to 12,000 km from the impact site. For CI chondrites, Ru/Ir = 1.5. A ballistic model of ejecta cloud cooling and expansion, which employs the available vapor-pressure versus temperature data for Ru and It, predicts qualitatively similar global variation in the Ru/Ir ratio but by only a factor of 1.5. We infer that several other factors, such as remobilization of PGE during diagenesis, preferential oxidation of Ru, condensation kinetics and atmospheric chemical and circulation processes, may account for the observed larger Ru/Ir variation. |
| format | Dataset Open Access |
| id | pangaea_https___doi_org_10_1594_PANGAEA_712117 |
| institution | PANGAEA |
| language | en |
| publishDate | 1995 |
| publisher | PANGAEA |
| record_format | pangaea |
| spellingShingle | Platinum-group element abundances in background samples and the K-T boundary interval from DSDP Hole 91-596 (Table 2) Evans, Noreen J Ahrens, Thomas J Gregoire, D C 91-596; Calculated; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Inductively coupled plasma - mass spectrometry (ICP-MS); Iridium; Leg91; Palladium; Platinum; Rubidium; Rubidium/Iridium ratio; Sample code/label; South Pacific Ocean New data on Ru/Ir abundance ratios are presented for nonmarine (Hell Creek, Montana; Frenchman River, Saskatchewan) and marine Cretaceous-Tertiary boundary sites (Brazos River, Texas; Beloc, Haiti; DSDP 577 and DSDP 596). The Ru/Ir ratio varies from 0.5 to 1 within 4000 km of Chicxulub and increases to 2-3 at paleodistances (65 Ma) of up to 12,000 km from the impact site. For CI chondrites, Ru/Ir = 1.5. A ballistic model of ejecta cloud cooling and expansion, which employs the available vapor-pressure versus temperature data for Ru and It, predicts qualitatively similar global variation in the Ru/Ir ratio but by only a factor of 1.5. We infer that several other factors, such as remobilization of PGE during diagenesis, preferential oxidation of Ru, condensation kinetics and atmospheric chemical and circulation processes, may account for the observed larger Ru/Ir variation. |
| title | Platinum-group element abundances in background samples and the K-T boundary interval from DSDP Hole 91-596 (Table 2) |
| topic | 91-596; Calculated; Deep Sea Drilling Project; DRILL; Drilling/drill rig; DSDP; DSDP/ODP/IODP sample designation; Glomar Challenger; Inductively coupled plasma - mass spectrometry (ICP-MS); Iridium; Leg91; Palladium; Platinum; Rubidium; Rubidium/Iridium ratio; Sample code/label; South Pacific Ocean |
| url | https://doi.org/10.1594/PANGAEA.712117 |