典型文献
Resolving impact volatilization and condensation from target rock mixing and hydrothermal overprinting within the Chicxulub impact structure
文献摘要:
This work presents isotopic data for the non-traditional isotope systems Fe,Cu,and Zn on a set of Chicxulub impactites and target lithologies with the aim of better documenting the dynamic processes taking place during hypervelocity impact events,as well as those affecting impact structures during the post-impact phase.The focus lies on material from the recent IODP-ICDP Expedition 364 Hole M0077A drill core obtained from the offshore Chicxulub peak ring.Two ejecta blanket samples from the UNAM 5 and 7 cores were used to compare the crater lithologies with those outside of the impact structure.The datasets of bulk Fe,Cu,and Zn isotope ratios are coupled with petrographic observations and bulk major and trace element compositions to disentangle equilibrium isotope fractionation effects from kinetic processes.The observed Fe and Cu isotopic signatures,with δ56/54Fe ranging from-0.95‰ to 0.58‰ and δ65/63Cu from-0.73‰ to 0.14%,mostly reflect felsic,mafic,and carbonate target lithology mixing and secondary sulfide mineral formation,the latter associated to the extensive and long-lived(>105 years)hydrothermal system within Chicxulub structure.On the other hand,the stable Zn isotope ratios provide evidence for volatility-governed isotopic fractionation.The heavier Zn isotopic composi-tions observed for the uppermost part of the impactite sequence and a metamorphic clast(δ66/64Zn of up to 0.80‰ and 0.87‰,respectively)relative to most basement lithologies and impact melt rock units indicate partial vaporization of Zn,comparable to what has been observed for Cretaceous-Paleogene boundary layer sediments around the world,as well as for tektites from various strewn fields.In contrast to previous work,our data indicate that an isotopically light Zn reservoir(δ66/64Zn down to-0.49‰),of which the existence has previously been suggested based on mass balance considerations,may reside within the upper impact melt rock(UIM)unit.This observation is restricted to a few UIM samples only and cannot be extended to other target or impact melt rock units.Light isotopic signatures of moderately volatile elements in tektites and microtektites have previously been linked to(back-)condensation under distinct kinetic regimes.Although some of the signatures observed may have been partially overprinted during post-impact processes,our bulk data confirm impact volatilization and condensation of Zn,which may be even more pronounced at the microscale,with variable degrees of mixing between isotopically distinct reservoirs,not only at proximal to distal ejecta sites,but also within the lithologies associated with the Chicxulub impact crater.
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作者姓名:
Thomas Déhais;Stepan M.Chernonozhkin;Pim Kaskes;Sietze J.de Graaff;Vinciane Debaille;Frank Vanhaecke;Philippe Claeys;Steven Goderis
作者机构:
Analytical,Environmental and Geo-Chemistry,Vrije Universiteit Brussel,Brussels,Belgium;Laboratoire G-Time,Université Libre de Bruxelles,Brussels,Belgium;Department of Chemistry,Atomic&Mass Spectrometry,Ghent University,Ghent,Belgium
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引用格式:
[1]Thomas Déhais;Stepan M.Chernonozhkin;Pim Kaskes;Sietze J.de Graaff;Vinciane Debaille;Frank Vanhaecke;Philippe Claeys;Steven Goderis-.Resolving impact volatilization and condensation from target rock mixing and hydrothermal overprinting within the Chicxulub impact structure)[J].地学前缘(英文版),2022(05):16-31
A类:
Chicxulub,impactites,M0077A,UNAM,54Fe,impactite,clast,64Zn,tektites,microtektites
B类:
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AB值:
0.481328
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