Comparison of the osmium and chromium isotopic methods for the detection of meteoritic components in impactites: Examples from the Morokweng and Vredefort impact structures, South Africa

نویسندگان

  • Christian Koeberl
  • C. Koeberl
چکیده

Breccias and melt rocks found at possible meteorite impact structures on Earth may contain a minor extraterrestrial component. In the absence of evidence of shockmetamorphic effects in such rocks, the unambiguous detection of an extraterrestrial component can be of diagnostic value regarding the impact origin of a geologic structure. Previously the concentrations of siderophile elements, mainly the platinumgroup elements (PGEs), or osmium isotopic studies have been used to detect such a meteoritic component. The Cr isotopic method has shown great potential for identifying the type of impactor. Here we use a combination of trace element (PGE) and Os and Cr isotopic data for rocks from the two large impact structures, Vredefort and Morokweng, both in South Africa, to compare the two isotopic methods directly for the first time. The percentage of a meteoritic component in Vredefort granophyre was too low to yield a Cr isotopic signal, but there was a distinct Os isotope effect. For Morokweng, both methods yielded positive results, the Cr isotope data suggesting that the projectile had the composition of an ordinary chondrite, probably an L chondrite. Comparison of the two methods thus confirms that the Os isotopic method is a Koeberl, C., Peucker-Ehrenbrink, B., Reimold, W.U., Shukolyukov, A., and Lugmair, G.W., 2002, Comparison of the osmium and chromium isotopic methods for the detection of meteoritic components in impactites: Examples from the Morokweng and Vredefort impact structures, South Africa, in Koeberl, C., and MacLeod, K.G., eds., Catastrophic Events and Mass Extinctions: Impacts and Beyond: Boulder, Colorado, Geological Society of America Special Paper 356, p. 607–617. *E-mails: Koeberl, [email protected]; Peucker-Ehrenbrink, [email protected]; Reimold, [email protected]; Shukolyukov, [email protected]; Lugmair, [email protected] C. Koeberl et al. 608 more sensitive tool for detecting an extraterrestrial component, whereas the Cr isotopic method, where applicable, can provide additional information regarding the nature of the impactor.

برای دانلود رایگان متن کامل این مقاله و بیش از 32 میلیون مقاله دیگر ابتدا ثبت نام کنید

ثبت نام

اگر عضو سایت هستید لطفا وارد حساب کاربری خود شوید

منابع مشابه

Osmium Isotope Constraints on the Proportion of Bolide Component in Chicxulub

Introduction: There have been numerous previous attempts to identify the projectile that produced the Chicxulub impact crater. Kyte [1] reported a fragment of rock in K/T boundary sediments that had been deposited in the Pacific Ocean. The textures and chemistry of the fragment suggested it was an altered fragment of carbonaceous chondrite material. Kyte interpreted it to be from the Chicxulub ...

متن کامل

Re-Os isotope and geochemical study of the Vredefort Granophyre: Clues to the origin of the Vredefort structure, South Africa

The origin of granophyric rock dikes (the Vredefort Granophyre) at the 2 Ga Vredefort structure in South Africa has been controversial. They have been interpreted as either impact melt or igneous intrusions. Most Vredefort Granophyre samples have considerably higher Os contents than the country rocks and Re/Os and Os/Os ratios that scatter about a 2 Ga isochron. Their initial Os/Os ratios (at 2...

متن کامل

Bosumtwi impact structure, Ghana: Geochemistry of impactites and target rocks, and search for a meteoritic component

available online at http://meteoritics.org 1493 © The Meteoritical Society, 2005. Printed in USA. Bosumtwi impact structure, Ghana: Geochemistry of impactites and target rocks, and search for a meteoritic component Xiongxin DAI1, 4, Daniel BOAMAH1, Christian KOEBERL1*, Wolf Uwe REIMOLD2, Gordon IRVINE3, and Iain MCDONALD3 1Department of Geological Sciences, University of Vienna, Althanstrasse 1...

متن کامل

Metamorphism on the Moon: A terrestrial analogue in the Vredefort dome, South Africa?

A new model is proposed to explain the origin of enigmatic fine-grained granulite facies rocks sampled from the Moon, based on observations from the Vredefort dome, South Africa. The dome is the deeply eroded central uplift of the ;300-km-diameter Vredefort impact structure. In the dome, fine-grained granulites displaying poikilitic or granoblastic microstructures were formed by relatively slow...

متن کامل

Geochemistry and petrography of impact breccias and target rocks from the 145 Ma Morokweng impact structure, South Africa

Morokweng is a large, 145 Ma impact structure in the Northwest Province of South Africa. The impact origin of this structure and its melt rock has been confirmed by ample evidence of shock metamorphism in clasts within the melt rock and samples from granitoid basement below the melt body. The age of this structure is indistinguishable from the biostratigraphic age of the Jurassic-Cretaceous (J-...

متن کامل

ذخیره در منابع من


  با ذخیره ی این منبع در منابع من، دسترسی به آن را برای استفاده های بعدی آسان تر کنید

عنوان ژورنال:

دوره   شماره 

صفحات  -

تاریخ انتشار 2002