FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2528221477> ?p ?o ?g. }

• W2528221477 endingPage "221" @default.
• W2528221477 startingPage "214" @default.
• W2528221477 abstract "The possible presence of the high-density carbon polymorph with hexagonal symmetry known as “lonsdaleite” provides an important marker for shock impact events. It is typically considered to form as a metastable phase produced from graphite or other carbonaceous precursors. However, its existence has recently been called into question. Here we collected high-resolution synchrotron X-ray diffraction data for laboratory-shocked and natural impact diamonds that both show evidence for deviations from cubic symmetry, that would be consistent with the appearance of hexagonal stacking sequences. These results show that hexagonality can be achieved by shocking diamond as well as from graphite precursors. The diffraction results are analyzed in terms of a general model that describes intermediate stacking sequences between pure diamond (fully cubic) and “lonsdaleite” (fully hexagonal) phases, with provision made for ordered vs disordered stacking arrangements. This approach provides a “hexagonality index” that can be used to characterize and distinguish among samples that have experienced different degrees of shock or static high pressure-high temperature treatments. We have also examined the relative energetics of diamond and “lonsdaleite” structures using density functional theoretical (DFT) methods. The results set limits on the conditions under which a transformation between diamond and “lonsdaleite” structures can be achieved. Calculated Raman spectra provide an indicator for the presence of extended hexagonal stacking sequences within natural and laboratory-prepared samples. Our results show that comparable crystallographic structures may be developed by impact-generated shockwaves starting from ambient conditions using either of the two different allotropes of carbon (diamond, graphite). This broadens the scope for its occurrence in terrestrial and planetary systems." @default.
• W2528221477 created "2016-10-14" @default.
• W2528221477 creator A5011594268 @default.
• W2528221477 creator A5018680494 @default.
• W2528221477 creator A5023698297 @default.
• W2528221477 creator A5027451469 @default.
• W2528221477 creator A5038290524 @default.
• W2528221477 creator A5044875056 @default.
• W2528221477 creator A5055607365 @default.
• W2528221477 creator A5057537207 @default.
• W2528221477 creator A5082649235 @default.
• W2528221477 date "2016-11-01" @default.
• W2528221477 modified "2023-10-16" @default.
• W2528221477 title "Structural characterization of natural diamond shocked to 60 GPa; implications for Earth and planetary systems" @default.
• W2528221477 cites W1490481542 @default.
• W2528221477 cites W1527174217 @default.
• W2528221477 cites W1650202143 @default.
• W2528221477 cites W1964070428 @default.
• W2528221477 cites W1964581458 @default.
• W2528221477 cites W1964884186 @default.
• W2528221477 cites W1969625381 @default.
• W2528221477 cites W1972972958 @default.
• W2528221477 cites W1982650110 @default.
• W2528221477 cites W1987074928 @default.
• W2528221477 cites W1997084181 @default.
• W2528221477 cites W2014593285 @default.
• W2528221477 cites W2018526410 @default.
• W2528221477 cites W2023271753 @default.
• W2528221477 cites W2023789912 @default.
• W2528221477 cites W2026331501 @default.
• W2528221477 cites W2028777514 @default.
• W2528221477 cites W2030725132 @default.
• W2528221477 cites W2032556527 @default.
• W2528221477 cites W2041784109 @default.
• W2528221477 cites W2043570127 @default.
• W2528221477 cites W2044662712 @default.
• W2528221477 cites W2048835561 @default.
• W2528221477 cites W2049959724 @default.
• W2528221477 cites W2054864475 @default.
• W2528221477 cites W2059040772 @default.
• W2528221477 cites W2069356849 @default.
• W2528221477 cites W2070498342 @default.
• W2528221477 cites W2072700653 @default.
• W2528221477 cites W2074906637 @default.
• W2528221477 cites W2079006841 @default.
• W2528221477 cites W2080808829 @default.
• W2528221477 cites W2102727317 @default.
• W2528221477 cites W2116617856 @default.
• W2528221477 cites W2126974341 @default.
• W2528221477 cites W2129722247 @default.
• W2528221477 cites W2133437740 @default.
• W2528221477 cites W2149420261 @default.
• W2528221477 cites W2168690982 @default.
• W2528221477 cites W2210655415 @default.
• W2528221477 cites W2328383347 @default.
• W2528221477 doi "https://doi.org/10.1016/j.lithos.2016.09.023" @default.
• W2528221477 hasPublicationYear "2016" @default.
• W2528221477 type Work @default.
• W2528221477 sameAs 2528221477 @default.
• W2528221477 citedByCount "27" @default.
• W2528221477 countsByYear W25282214772016 @default.
• W2528221477 countsByYear W25282214772017 @default.
• W2528221477 countsByYear W25282214772018 @default.
• W2528221477 countsByYear W25282214772019 @default.
• W2528221477 countsByYear W25282214772020 @default.
• W2528221477 countsByYear W25282214772021 @default.
• W2528221477 countsByYear W25282214772022 @default.
• W2528221477 countsByYear W25282214772023 @default.
• W2528221477 crossrefType "journal-article" @default.
• W2528221477 hasAuthorship W2528221477A5011594268 @default.
• W2528221477 hasAuthorship W2528221477A5018680494 @default.
• W2528221477 hasAuthorship W2528221477A5023698297 @default.
• W2528221477 hasAuthorship W2528221477A5027451469 @default.
• W2528221477 hasAuthorship W2528221477A5038290524 @default.
• W2528221477 hasAuthorship W2528221477A5044875056 @default.
• W2528221477 hasAuthorship W2528221477A5055607365 @default.
• W2528221477 hasAuthorship W2528221477A5057537207 @default.
• W2528221477 hasAuthorship W2528221477A5082649235 @default.
• W2528221477 hasBestOaLocation W25282214772 @default.
• W2528221477 hasConcept C104779481 @default.
• W2528221477 hasConcept C120665830 @default.
• W2528221477 hasConcept C121332964 @default.
• W2528221477 hasConcept C140205800 @default.
• W2528221477 hasConcept C159985019 @default.
• W2528221477 hasConcept C162882748 @default.
• W2528221477 hasConcept C185592680 @default.
• W2528221477 hasConcept C192562407 @default.
• W2528221477 hasConcept C207114421 @default.
• W2528221477 hasConcept C21368211 @default.
• W2528221477 hasConcept C2776921476 @default.
• W2528221477 hasConcept C2779698641 @default.
• W2528221477 hasConcept C33347731 @default.
• W2528221477 hasConcept C39173455 @default.
• W2528221477 hasConcept C40003534 @default.
• W2528221477 hasConcept C46141821 @default.
• W2528221477 hasConcept C8010536 @default.
• W2528221477 hasConceptScore W2528221477C104779481 @default.
• W2528221477 hasConceptScore W2528221477C120665830 @default.

• next