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Pregled bibliografske jedinice broj: 960185

Shock deformation of calcite, a possible tool for reconstruction of the size of deeply eroded impact structure. Agoudal impact structure (Morocco) case study


Čalogović, Marina; Marjanac, Tihomir; El Kerni, Houda; Chennaoui Aoudjehane, Hasnaa
Shock deformation of calcite, a possible tool for reconstruction of the size of deeply eroded impact structure. Agoudal impact structure (Morocco) case study // 81st Annual Meeting of The Meteoritical Society, program
Moskva, 2018. 6267, 1 (predavanje, međunarodna recenzija, sažetak, znanstveni)


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Naslov
Shock deformation of calcite, a possible tool for reconstruction of the size of deeply eroded impact structure. Agoudal impact structure (Morocco) case study

Autori
Čalogović, Marina ; Marjanac, Tihomir ; El Kerni, Houda ; Chennaoui Aoudjehane, Hasnaa

Vrsta, podvrsta i kategorija rada
Sažeci sa skupova, sažetak, znanstveni

Izvornik
81st Annual Meeting of The Meteoritical Society, program / - Moskva, 2018

Skup
81st Annual Meeting of The Meteoritical Society

Mjesto i datum
Moskva, Rusija, 22-27.07.2018

Vrsta sudjelovanja
Predavanje

Vrsta recenzije
Međunarodna recenzija

Ključne riječi
X-ray diffraction, calcite, peak broadening, microstrain

Sažetak
Study from Ries crater in Germany showed that peaks in X-ray diffraction patterns of shocked carbonates are broadened due to increased domain size and microstrain and the deformation is correlated with peak pressure. It is expected that shock-induced deformations of calcite unit-cell decreases with increasing distance from the impact structure centre, which would allow for estimation of the structure size by analysis of diffractograms of a number of samples from a deeply eroded structure. We have tested this hypothesis by analyzing target limestone samples from various locations within the Agoudal impact structure in Morocco. The XRD powder analysis revealed peak broadening in X-ray diffraction pattern, as well as peak shift that indicates shock induced effects in calcite. The observed peak broadening was determined by calculation of Full Width at Half Maximum (FWHM). The domain size and strain are determined after Williamson-Hall method by calculations in XPowderX software. Also, unit-cell parameters were refined from peak positions. Comparison of X-ray diffraction patterns from different locations in the Agoudal impact structure revealed that shock-induced effects decrease with distance from the presumed impact centre.

Izvorni jezik
Engleski

Znanstvena područja
Geologija, Kemija



POVEZANOST RADA


Ustanove
Prirodoslovno-matematički fakultet, Zagreb

Profili:

Avatar Url Tihomir Marjanac (autor)

Citiraj ovu publikaciju

Čalogović, Marina; Marjanac, Tihomir; El Kerni, Houda; Chennaoui Aoudjehane, Hasnaa
Shock deformation of calcite, a possible tool for reconstruction of the size of deeply eroded impact structure. Agoudal impact structure (Morocco) case study // 81st Annual Meeting of The Meteoritical Society, program
Moskva, 2018. 6267, 1 (predavanje, međunarodna recenzija, sažetak, znanstveni)
Čalogović, M., Marjanac, T., El Kerni, H. & Chennaoui Aoudjehane, H. (2018) Shock deformation of calcite, a possible tool for reconstruction of the size of deeply eroded impact structure. Agoudal impact structure (Morocco) case study. U: 81st Annual Meeting of The Meteoritical Society, program.
@article{article, year = {2018}, pages = {1}, chapter = {6267}, keywords = {X-ray diffraction, calcite, peak broadening, microstrain}, title = {Shock deformation of calcite, a possible tool for reconstruction of the size of deeply eroded impact structure. Agoudal impact structure (Morocco) case study}, keyword = {X-ray diffraction, calcite, peak broadening, microstrain}, publisherplace = {Moskva, Rusija}, chapternumber = {6267} }