Late Eocene Ni-rich Spinel from LL44-GPC3 (Central Pacific), ODP Site 689B (Maud Rise, Antarctic), DSDP Sites 94 (Gulf of Mexico) and 612 (US East Coast)

Details Late Eocene Ni-rich Spinel from LL44-GPC3 (Central Pacific), ODP Site 689B (Maud Rise, Antarctic), DSDP Sites 94 (Gulf of Mexico) and 612 (US East Coast) Late Eocene Ni-rich Spinel from LL44-GPC3 (Central Pacific), ODP Site 689B (Maud Rise, Antarctic), DSDP Sites 94 (Gulf of Mexico) and 612 (US East Coast)

Mar 1999

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1999lpi....30.1674p&link_type=abstract

30th Annual Lunar and Planetary Science Conference, March 15-29, 1999, Houston, TX, abstract no. 1674

Physics

Scientific paper

The Ni-rich spinel anomaly, previously reported in the E/O Stratotype at
Massignano in Italy, is recorded worldwide in upper Eocene sediments. We
show that this anomaly derives from the same event as the one that
produced microkrystites, probably a comet impact.

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